際際滷shows by User: mnsurvase / http://www.slideshare.net/images/logo.gif 際際滷shows by User: mnsurvase / Tue, 21 Apr 2020 11:08:30 GMT 際際滷Share feed for 際際滷shows by User: mnsurvase India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane) /slideshow/india-minerals-and-energy-resources-marathibhartatil-khanij-ani-urja-sadhane-232359993/232359993 india-mineralsandenergyresourcesmarathi-bhartatilkhanijaniurjasadhane-200421110830
Geography of India India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane) ]]>

Geography of India India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane) ]]>
Tue, 21 Apr 2020 11:08:30 GMT /slideshow/india-minerals-and-energy-resources-marathibhartatil-khanij-ani-urja-sadhane-232359993/232359993 mnsurvase@slideshare.net(mnsurvase) India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane) mnsurvase Geography of India India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane) <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/india-mineralsandenergyresourcesmarathi-bhartatilkhanijaniurjasadhane-200421110830-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Geography of India India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane)
India- Minerals and energy resources (marathi-bhartatil khanij ani urja sadhane) from Malhari Survase
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Soil management (mruda vyvasthapan marathi) /mnsurvase/soil-management-mruda-vyvasthapan-marathi soilmanagementmrudavyvasthapan-marathi-190324072511
爐爛爐萎ぞ爐伍爐むぞ爐朽た爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐伍爐爐迦爐爐爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐朽ざ爛爐爐爐むぞ 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐爐爛爐爛爐むい爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐爐爛爐оい爛]]>

爐爛爐萎ぞ爐伍爐むぞ爐朽た爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐伍爐爐迦爐爐爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐朽ざ爛爐爐爐むぞ 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐爐爛爐爛爐むい爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐爐爛爐оい爛]]>
Sun, 24 Mar 2019 07:25:11 GMT /mnsurvase/soil-management-mruda-vyvasthapan-marathi mnsurvase@slideshare.net(mnsurvase) Soil management (mruda vyvasthapan marathi) mnsurvase 爐爛爐萎ぞ爐伍爐むぞ爐朽た爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐伍爐爐迦爐爐爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐朽ざ爛爐爐爐むぞ 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐爐爛爐爛爐むい爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐爐爛爐оい爛 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/soilmanagementmrudavyvasthapan-marathi-190324072511-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爛爐萎ぞ爐伍爐むぞ爐朽た爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐伍爐爐迦爐爐爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐朽ざ爛爐爐爐むぞ 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐爐鉦爛 爐爐爐爛爐爛爐むい爐 爐爛爐爐 爐朽爐爐朽じ爛爐ムぞ爐爐 爐爐爛爐оい爛
Soil management (mruda vyvasthapan marathi) from Malhari Survase
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Introduction to soil geography (mruda bhugolachi olakh marathi) /slideshow/introduction-to-soil-geography-mruda-bhugolachi-olakh-marathi/137924016 introductiontosoilgeographymrudabhugolachiolakh-marathi-190324072043
爐爛爐萎じ爛爐むぞ爐朽え爐 爐爛爐爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐 爐謹ぞ爐伍爐む爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爛爐爐 爐爛爐爛爐迦ぞ爐爐 爐爛爐爐 爐謹ぞ爐伍爐む爐萎ぞ爐謹 爐伍爐爐爐 ]]>

爐爛爐萎じ爛爐むぞ爐朽え爐 爐爛爐爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐 爐謹ぞ爐伍爐む爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爛爐爐 爐爛爐爛爐迦ぞ爐爐 爐爛爐爐 爐謹ぞ爐伍爐む爐萎ぞ爐謹 爐伍爐爐爐 ]]>
Sun, 24 Mar 2019 07:20:43 GMT /slideshow/introduction-to-soil-geography-mruda-bhugolachi-olakh-marathi/137924016 mnsurvase@slideshare.net(mnsurvase) Introduction to soil geography (mruda bhugolachi olakh marathi) mnsurvase 爐爛爐萎じ爛爐むぞ爐朽え爐 爐爛爐爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐 爐謹ぞ爐伍爐む爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爛爐爐 爐爛爐爛爐迦ぞ爐爐 爐爛爐爐 爐謹ぞ爐伍爐む爐萎ぞ爐謹 爐伍爐爐爐 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/introductiontosoilgeographymrudabhugolachiolakh-marathi-190324072043-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爛爐萎じ爛爐むぞ爐朽え爐 爐爛爐爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐 爐謹ぞ爐伍爐む爐: 爐朽爐爐鉦爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爛爐爐 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爛爐爐 爐爛爐爛爐迦ぞ爐爐 爐爛爐爐 爐謹ぞ爐伍爐む爐萎ぞ爐謹 爐伍爐爐爐
Introduction to soil geography (mruda bhugolachi olakh marathi) from Malhari Survase
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Introduction to human geography (manavi bhugolachi olakh marathi) /slideshow/introduction-to-human-geography-manavi-bhugolachi-olakh-marathi/137923891 introductiontohumangeographymanavibhugolachiolakh-marathi-190324071623
爐爐爛爐о爐 爐爛爐爛爐迦ぞ爐爛爐爐 爐爛爐萎ぎ爛爐 爐謹ぞ爐爐 爐爛爐萎じ爛爐むぞ爐朽え爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛爐爐 爐朽爐爐鉦爛爐爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爐鉦え爐朽 爐爛爐爛爐 爐爐爛爐爐鉦じ爐鉦爛 爐爛爐劇爐爛爐爛爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐爐項い爛爐 ]]>

爐爐爛爐о爐 爐爛爐爛爐迦ぞ爐爛爐爐 爐爛爐萎ぎ爛爐 爐謹ぞ爐爐 爐爛爐萎じ爛爐むぞ爐朽え爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛爐爐 爐朽爐爐鉦爛爐爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爐鉦え爐朽 爐爛爐爛爐 爐爐爛爐爐鉦じ爐鉦爛 爐爛爐劇爐爛爐爛爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐爐項い爛爐 ]]>
Sun, 24 Mar 2019 07:16:23 GMT /slideshow/introduction-to-human-geography-manavi-bhugolachi-olakh-marathi/137923891 mnsurvase@slideshare.net(mnsurvase) Introduction to human geography (manavi bhugolachi olakh marathi) mnsurvase 爐爐爛爐о爐 爐爛爐爛爐迦ぞ爐爛爐爐 爐爛爐萎ぎ爛爐 爐謹ぞ爐爐 爐爛爐萎じ爛爐むぞ爐朽え爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛爐爐 爐朽爐爐鉦爛爐爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爐鉦え爐朽 爐爛爐爛爐 爐爐爛爐爐鉦じ爐鉦爛 爐爛爐劇爐爛爐爛爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐爐項い爛爐 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/introductiontohumangeographymanavibhugolachiolakh-marathi-190324071623-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爐爛爐о爐 爐爛爐爛爐迦ぞ爐爛爐爐 爐爛爐萎ぎ爛爐 爐謹ぞ爐爐 爐爛爐萎じ爛爐むぞ爐朽え爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛爐爐 爐朽爐爐鉦爛爐爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐伍爐朽ぐ爛爐 爐爐鉦え爐朽 爐爛爐爛爐 爐爐爛爐爐鉦じ爐鉦爛 爐爛爐劇爐爛爐爛爐 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐朽爐爐鉦お爛爐む 爐爐鉦え爐朽 爐爛爐爛爐迦ぞ爐爛 爐爐項い爛爐
Introduction to human geography (manavi bhugolachi olakh marathi) from Malhari Survase
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Population (loksankhya marathi) /slideshow/population-loksankhya-marathi/137923647 populationloksankhya-marathi-190324070853
爐迦爐爐伍爐爛爐爛爐爐 爐朽た爐むぐ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐 爐爐鉦げ爛爐ムじ爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐∇爐爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐爛爐萎ぎ爐爐鉦爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐ムげ爐鉦爐むぐ ]]>

爐迦爐爐伍爐爛爐爛爐爐 爐朽た爐むぐ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐 爐爐鉦げ爛爐ムじ爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐∇爐爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐爛爐萎ぎ爐爐鉦爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐ムげ爐鉦爐むぐ ]]>
Sun, 24 Mar 2019 07:08:53 GMT /slideshow/population-loksankhya-marathi/137923647 mnsurvase@slideshare.net(mnsurvase) Population (loksankhya marathi) mnsurvase 爐迦爐爐伍爐爛爐爛爐爐 爐朽た爐むぐ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐 爐爐鉦げ爛爐ムじ爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐∇爐爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐爛爐萎ぎ爐爐鉦爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐ムげ爐鉦爐むぐ <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/populationloksankhya-marathi-190324070853-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐迦爐爐伍爐爛爐爛爐爐 爐朽た爐むぐ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐 爐爐鉦げ爛爐ムじ爐爐 爐迦爐爐伍爐爛爐爐 爐朽ぞ爐∇爐爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐爛爐萎ぎ爐爐鉦爐 爐伍た爐爛爐оぞ爐爐 爐迦爐爐伍爐爛爐爐 爐伍爐ムげ爐鉦爐むぐ
Population (loksankhya marathi) from Malhari Survase
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Settelments (vasahati) marathi /slideshow/settelments-vasahati-marathi/136264740 settelmentsvasahati-marathi-190314041219
爐爛爐萎じ爛爐むぞ爐朽え爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む (Rural Settelment) 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛爐爐 爐伍爐ムぞ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐朽じ爐鉦す爐む爐爛 爐爛爐萎ぞ爐萎爐爐鉦え爛爐伍ぞ爐 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爐爛 爐朽爐謹た爐劇爐爛 爐爐鉦爐萎 爐朽じ爛爐む/ 爐朽じ爐鉦す爐む 爐爐鉦爐萎爐爐萎ぃ 爐爐鉦ぐ爐むぞ爐む爐 爐爐鉦爐萎爐爐萎ぃ 爐伍爐ムた爐む 爐爐爐萎爐爐萎ぃ爐鉦爛 爐爐萎た爐爐鉦ぎ 爐謹す爐萎 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 ]]>

爐爛爐萎じ爛爐むぞ爐朽え爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む (Rural Settelment) 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛爐爐 爐伍爐ムぞ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐朽じ爐鉦す爐む爐爛 爐爛爐萎ぞ爐萎爐爐鉦え爛爐伍ぞ爐 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爐爛 爐朽爐謹た爐劇爐爛 爐爐鉦爐萎 爐朽じ爛爐む/ 爐朽じ爐鉦す爐む 爐爐鉦爐萎爐爐萎ぃ 爐爐鉦ぐ爐むぞ爐む爐 爐爐鉦爐萎爐爐萎ぃ 爐伍爐ムた爐む 爐爐爐萎爐爐萎ぃ爐鉦爛 爐爐萎た爐爐鉦ぎ 爐謹す爐萎 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 ]]>
Thu, 14 Mar 2019 04:12:19 GMT /slideshow/settelments-vasahati-marathi/136264740 mnsurvase@slideshare.net(mnsurvase) Settelments (vasahati) marathi mnsurvase 爐爛爐萎じ爛爐むぞ爐朽え爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む (Rural Settelment) 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛爐爐 爐伍爐ムぞ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐朽じ爐鉦す爐む爐爛 爐爛爐萎ぞ爐萎爐爐鉦え爛爐伍ぞ爐 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爐爛 爐朽爐謹た爐劇爐爛 爐爐鉦爐萎 爐朽じ爛爐む/ 爐朽じ爐鉦す爐む 爐爐鉦爐萎爐爐萎ぃ 爐爐鉦ぐ爐むぞ爐む爐 爐爐鉦爐萎爐爐萎ぃ 爐伍爐ムた爐む 爐爐爐萎爐爐萎ぃ爐鉦爛 爐爐萎た爐爐鉦ぎ 爐謹す爐萎 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/settelmentsvasahati-marathi-190314041219-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爛爐萎じ爛爐むぞ爐朽え爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む (Rural Settelment) 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛爐爐 爐伍爐ムぞ爐爐鉦さ爐 爐爐萎た爐爐鉦ぎ 爐爐萎ぃ爐鉦ぐ爛 爐爐爐 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爛爐萎爐鉦ぐ 爐朽じ爐鉦す爐む爐爛 爐爛爐萎ぞ爐萎爐爐鉦え爛爐伍ぞ爐 爐爛爐萎爐鉦ぐ 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛 爐爛爐萎ぞ爐爛爐 爐朽じ爐鉦す爐む爐爐爛 爐朽爐謹た爐劇爐爛 爐爐鉦爐萎 爐朽じ爛爐む/ 爐朽じ爐鉦す爐む 爐爐鉦爐萎爐爐萎ぃ 爐爐鉦ぐ爐むぞ爐む爐 爐爐鉦爐萎爐爐萎ぃ 爐伍爐ムた爐む 爐爐爐萎爐爐萎ぃ爐鉦爛 爐爐萎た爐爐鉦ぎ 爐謹す爐萎 爐朽じ爐鉦す爐む爐爛 爐爐鉦ぐ爛爐爛
Settelments (vasahati) marathi from Malhari Survase
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Factors affecting tourism development (Paryatanavar Parinam Karnare Ghatak) /slideshow/factors-affecting-tourism-development-paryatanavar-parinam-karnare-ghatak/136261924 factorsaffectingtourismdevelopment-190314035923
爐爛爐爛爐迦た爐 爐爐爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐 爐爐萎爐ムた爐 爐爐爐]]>

爐爛爐爛爐迦た爐 爐爐爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐 爐爐萎爐ムた爐 爐爐爐]]>
Thu, 14 Mar 2019 03:59:23 GMT /slideshow/factors-affecting-tourism-development-paryatanavar-parinam-karnare-ghatak/136261924 mnsurvase@slideshare.net(mnsurvase) Factors affecting tourism development (Paryatanavar Parinam Karnare Ghatak) mnsurvase 爐爛爐爛爐迦た爐 爐爐爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐 爐爐萎爐ムた爐 爐爐爐 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/factorsaffectingtourismdevelopment-190314035923-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爛爐爛爐迦た爐 爐爐爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐 爐爐萎爐ムた爐 爐爐爐
Factors affecting tourism development (Paryatanavar Parinam Karnare Ghatak) from Malhari Survase
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Impact of tourism (paryatanache parinam- marathi) /slideshow/impact-of-tourism-paryatanache-parinam-marathi/136261038 impactoftourismparyatanacheparinam-marathi-190314035416
爐爐萎爐爐爐爐鉦爐 爐朽た爐朽た爐 爐爛爐劇爐む爐萎ぞ爐朽ぐ 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐爐萎爐ムた爐 爐爐爐爐鉦爐朽ぐ 爐項爐爐鉦ぐ爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐爐 爐朽ぐ爛爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爛 爐爐萎爐爐鉦さ爐萎ぃ爐鉦さ爐萎爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐謹ぞ爐謹爐朽い 爐朽た爐爐鉦じ]]>

爐爐萎爐爐爐爐鉦爐 爐朽た爐朽た爐 爐爛爐劇爐む爐萎ぞ爐朽ぐ 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐爐萎爐ムた爐 爐爐爐爐鉦爐朽ぐ 爐項爐爐鉦ぐ爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐爐 爐朽ぐ爛爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爛 爐爐萎爐爐鉦さ爐萎ぃ爐鉦さ爐萎爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐謹ぞ爐謹爐朽い 爐朽た爐爐鉦じ]]>
Thu, 14 Mar 2019 03:54:16 GMT /slideshow/impact-of-tourism-paryatanache-parinam-marathi/136261038 mnsurvase@slideshare.net(mnsurvase) Impact of tourism (paryatanache parinam- marathi) mnsurvase 爐爐萎爐爐爐爐鉦爐 爐朽た爐朽た爐 爐爛爐劇爐む爐萎ぞ爐朽ぐ 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐爐萎爐ムた爐 爐爐爐爐鉦爐朽ぐ 爐項爐爐鉦ぐ爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐爐 爐朽ぐ爛爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爛 爐爐萎爐爐鉦さ爐萎ぃ爐鉦さ爐萎爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐謹ぞ爐謹爐朽い 爐朽た爐爐鉦じ <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/impactoftourismparyatanacheparinam-marathi-190314035416-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爐萎爐爐爐爐鉦爐 爐朽た爐朽た爐 爐爛爐劇爐む爐萎ぞ爐朽ぐ 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐爐萎爐ムた爐 爐爐爐爐鉦爐朽ぐ 爐項爐爐鉦ぐ爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐伍ぞ爐爐鉦爐逗 爐 爐伍ぞ爐爐伍爐爛爐むた爐 爐爐爐爐 爐朽ぐ爛爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爛 爐爐萎爐爐鉦さ爐萎ぃ爐鉦さ爐萎爐 爐爐萎た爐爐鉦ぎ 爐爐萎爐爐爐爐鉦爐 爐謹ぞ爐謹爐朽い 爐朽た爐爐鉦じ
Impact of tourism (paryatanache parinam- marathi) from Malhari Survase
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Introduction to tourism geography- Marathi /slideshow/introduction-to-tourism-geography-marathi/135839758 introductiontotourismgeography-190312101515
爐爐萎爐爐爐 爐爛爐項ぃ爐爛 爐爐鉦く? 爐爐萎爐爐爐爐鉦い爛爐 爐爐項い爛爐朽ぞ爐爛爐爐 爐む爐 爐爛爐劇爐爛 爐爐萎爐爐爐 爐爐萎う爛爐謹 爐 爐伍爐朽う爛爐謹 爐爐萎爐爐爐 爐爐萎爐爐爐爐鉦爛 爐朽爐謹た爐劇爐爛 爐爐萎爐爐爐爐鉦爛 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛 爐朽爐爐鉦お爛爐む 爐爐萎爐爐爐爐鉦爛 爐爐項い爛爐 爐爐萎爐爐爐爐鉦爛 爐爐爐むぐ爐朽た爐爛爐爐鉦ざ爐鉦爛爐 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛爐爐 爐伍ぎ爐伍爐爐 爐伍う爛爐爐伍爐ムた爐む爐む爐 爐爐萎爐爐爐 爐伍ぞ爐萎ぞ爐爐 ]]>

爐爐萎爐爐爐 爐爛爐項ぃ爐爛 爐爐鉦く? 爐爐萎爐爐爐爐鉦い爛爐 爐爐項い爛爐朽ぞ爐爛爐爐 爐む爐 爐爛爐劇爐爛 爐爐萎爐爐爐 爐爐萎う爛爐謹 爐 爐伍爐朽う爛爐謹 爐爐萎爐爐爐 爐爐萎爐爐爐爐鉦爛 爐朽爐謹た爐劇爐爛 爐爐萎爐爐爐爐鉦爛 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛 爐朽爐爐鉦お爛爐む 爐爐萎爐爐爐爐鉦爛 爐爐項い爛爐 爐爐萎爐爐爐爐鉦爛 爐爐爐むぐ爐朽た爐爛爐爐鉦ざ爐鉦爛爐 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛爐爐 爐伍ぎ爐伍爐爐 爐伍う爛爐爐伍爐ムた爐む爐む爐 爐爐萎爐爐爐 爐伍ぞ爐萎ぞ爐爐 ]]>
Tue, 12 Mar 2019 10:15:15 GMT /slideshow/introduction-to-tourism-geography-marathi/135839758 mnsurvase@slideshare.net(mnsurvase) Introduction to tourism geography- Marathi mnsurvase 爐爐萎爐爐爐 爐爛爐項ぃ爐爛 爐爐鉦く? 爐爐萎爐爐爐爐鉦い爛爐 爐爐項い爛爐朽ぞ爐爛爐爐 爐む爐 爐爛爐劇爐爛 爐爐萎爐爐爐 爐爐萎う爛爐謹 爐 爐伍爐朽う爛爐謹 爐爐萎爐爐爐 爐爐萎爐爐爐爐鉦爛 爐朽爐謹た爐劇爐爛 爐爐萎爐爐爐爐鉦爛 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛 爐朽爐爐鉦お爛爐む 爐爐萎爐爐爐爐鉦爛 爐爐項い爛爐 爐爐萎爐爐爐爐鉦爛 爐爐爐むぐ爐朽た爐爛爐爐鉦ざ爐鉦爛爐 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛爐爐 爐伍ぎ爐伍爐爐 爐伍う爛爐爐伍爐ムた爐む爐む爐 爐爐萎爐爐爐 爐伍ぞ爐萎ぞ爐爐 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/introductiontotourismgeography-190312101515-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> 爐爐萎爐爐爐 爐爛爐項ぃ爐爛 爐爐鉦く? 爐爐萎爐爐爐爐鉦い爛爐 爐爐項い爛爐朽ぞ爐爛爐爐 爐む爐 爐爛爐劇爐爛 爐爐萎爐爐爐 爐爐萎う爛爐謹 爐 爐伍爐朽う爛爐謹 爐爐萎爐爐爐 爐爐萎爐爐爐爐鉦爛 爐朽爐謹た爐劇爐爛 爐爐萎爐爐爐爐鉦爛 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛 爐朽爐爐鉦お爛爐む 爐爐萎爐爐爐爐鉦爛 爐爐項い爛爐 爐爐萎爐爐爐爐鉦爛 爐爐爐むぐ爐朽た爐爛爐爐鉦ざ爐鉦爛爐 爐伍爐朽ぐ爛爐 爐爐萎爐爐爐爐鉦爛爐爐 爐伍ぎ爐伍爐爐 爐伍う爛爐爐伍爐ムた爐む爐む爐 爐爐萎爐爐爐 爐伍ぞ爐萎ぞ爐爐
Introduction to tourism geography- Marathi from Malhari Survase
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Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 鐃準お爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 ) /slideshow/classification-and-recent-trend-in-tourism/117020042 classificationandrecenttrendintourism-180928041034
Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 爐爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 )]]>

Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 爐爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 )]]>
Fri, 28 Sep 2018 04:10:34 GMT /slideshow/classification-and-recent-trend-in-tourism/117020042 mnsurvase@slideshare.net(mnsurvase) Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 鐃準お爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 ) mnsurvase Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 爐爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 ) <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/classificationandrecenttrendintourism-180928041034-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 爐爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 )
Classification and recent trend in tourism (爐爐萎爐爐爐 爐朽ぐ爛爐爛爐爐萎ぃ 爐 爐爐萎爐爐爐爐鉦い爛爐 爐爐朽爐 爐伍爐爐迦爐爐爐 ) from Malhari Survase
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Procedure to Obtain Patents in India /slideshow/procedure-to-obtain-patents-in-india/90768368 proceduretoprotectintellectualitybyobtainingpatentsin-180315102325
The IPR protects your innovations and ideas related rights and from infringement by others and restricts its uses, making and selling without your permissions. This presentation aims to explore the significance of intellectual property rights and to know the procedure to obtain patents in India. For that, the data and information is collected from news papers, articles, magazines, internet websites, and expert interviews. Protecting intellectual property with patents provides the exclusive rights by law to the assignees or originator to make use of and exploit their inventions. The invention which meets the novelty, non-obviousness, usefulness in the industry, enabled etc criterias as per Indian patent act and fulfilling patentable criterias with proper application and details justifications with fallow up and clearing the objections are eligible to grants the patents. ]]>

The IPR protects your innovations and ideas related rights and from infringement by others and restricts its uses, making and selling without your permissions. This presentation aims to explore the significance of intellectual property rights and to know the procedure to obtain patents in India. For that, the data and information is collected from news papers, articles, magazines, internet websites, and expert interviews. Protecting intellectual property with patents provides the exclusive rights by law to the assignees or originator to make use of and exploit their inventions. The invention which meets the novelty, non-obviousness, usefulness in the industry, enabled etc criterias as per Indian patent act and fulfilling patentable criterias with proper application and details justifications with fallow up and clearing the objections are eligible to grants the patents. ]]>
Thu, 15 Mar 2018 10:23:25 GMT /slideshow/procedure-to-obtain-patents-in-india/90768368 mnsurvase@slideshare.net(mnsurvase) Procedure to Obtain Patents in India mnsurvase The IPR protects your innovations and ideas related rights and from infringement by others and restricts its uses, making and selling without your permissions. This presentation aims to explore the significance of intellectual property rights and to know the procedure to obtain patents in India. For that, the data and information is collected from news papers, articles, magazines, internet websites, and expert interviews. Protecting intellectual property with patents provides the exclusive rights by law to the assignees or originator to make use of and exploit their inventions. The invention which meets the novelty, non-obviousness, usefulness in the industry, enabled etc criterias as per Indian patent act and fulfilling patentable criterias with proper application and details justifications with fallow up and clearing the objections are eligible to grants the patents. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/proceduretoprotectintellectualitybyobtainingpatentsin-180315102325-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The IPR protects your innovations and ideas related rights and from infringement by others and restricts its uses, making and selling without your permissions. This presentation aims to explore the significance of intellectual property rights and to know the procedure to obtain patents in India. For that, the data and information is collected from news papers, articles, magazines, internet websites, and expert interviews. Protecting intellectual property with patents provides the exclusive rights by law to the assignees or originator to make use of and exploit their inventions. The invention which meets the novelty, non-obviousness, usefulness in the industry, enabled etc criterias as per Indian patent act and fulfilling patentable criterias with proper application and details justifications with fallow up and clearing the objections are eligible to grants the patents.
Procedure to Obtain Patents in India from Malhari Survase
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POTENTIALITY OF RAINWATER HARVESTING IN DANGE COLLEGE CAMPUS OF HATKANANGALE FOR SHRINKING THE WATER SCARCITY /slideshow/potentiality-of-rainwater-harvesting-in-dange-college-campus-of-hatkanangale-for-shrinking-the-water-scarcity-85954800/85954800 survaseeconomics-180110060631
Harvesting the rainwater for the water conservation and fulfilment of water requirements in the micro level areas with the optimistic method is essential in for better future. Thus the present research aims to identify the potentiality of rainwater harvesting in Dange college campus of Hatkanangale for shrinking the water scarcity.The campus located in rain shadow zone of Western Ghats receives 820.4mm annual average rainfall. It has 4.5 acres of campus with 6090 sq.m. built up area and 2547 sq. m. area of the roof surface. College has 6070 sq.m. area of fruit garden and 7100 sq. m. Play ground. For the present investigation, data regarding various aspects are collected through the college administration office, and skymet website. Runoff Coefficient and Annual rainwater harvesting potential (ARHP) of the campus is estimated by using formula (ARHP = R x AC x RC) given by Pecey, et.al; 1989. The analysis revels that approximate of 75 Lakh Litre water will be collected from the whole campus. Out of that 18.80 Lakh litre water will be collected purely on rooftop of the building and it is directly usable for the drinking and sanitization. It will be fulfil 90 % demand of the fresh water. Out of 74.52 Lakh litre water 55.71 L. Litre water will be useful for the gardening in the dry season. ]]>

Harvesting the rainwater for the water conservation and fulfilment of water requirements in the micro level areas with the optimistic method is essential in for better future. Thus the present research aims to identify the potentiality of rainwater harvesting in Dange college campus of Hatkanangale for shrinking the water scarcity.The campus located in rain shadow zone of Western Ghats receives 820.4mm annual average rainfall. It has 4.5 acres of campus with 6090 sq.m. built up area and 2547 sq. m. area of the roof surface. College has 6070 sq.m. area of fruit garden and 7100 sq. m. Play ground. For the present investigation, data regarding various aspects are collected through the college administration office, and skymet website. Runoff Coefficient and Annual rainwater harvesting potential (ARHP) of the campus is estimated by using formula (ARHP = R x AC x RC) given by Pecey, et.al; 1989. The analysis revels that approximate of 75 Lakh Litre water will be collected from the whole campus. Out of that 18.80 Lakh litre water will be collected purely on rooftop of the building and it is directly usable for the drinking and sanitization. It will be fulfil 90 % demand of the fresh water. Out of 74.52 Lakh litre water 55.71 L. Litre water will be useful for the gardening in the dry season. ]]>
Wed, 10 Jan 2018 06:06:31 GMT /slideshow/potentiality-of-rainwater-harvesting-in-dange-college-campus-of-hatkanangale-for-shrinking-the-water-scarcity-85954800/85954800 mnsurvase@slideshare.net(mnsurvase) POTENTIALITY OF RAINWATER HARVESTING IN DANGE COLLEGE CAMPUS OF HATKANANGALE FOR SHRINKING THE WATER SCARCITY mnsurvase Harvesting the rainwater for the water conservation and fulfilment of water requirements in the micro level areas with the optimistic method is essential in for better future. Thus the present research aims to identify the potentiality of rainwater harvesting in Dange college campus of Hatkanangale for shrinking the water scarcity.The campus located in rain shadow zone of Western Ghats receives 820.4mm annual average rainfall. It has 4.5 acres of campus with 6090 sq.m. built up area and 2547 sq. m. area of the roof surface. College has 6070 sq.m. area of fruit garden and 7100 sq. m. Play ground. For the present investigation, data regarding various aspects are collected through the college administration office, and skymet website. Runoff Coefficient and Annual rainwater harvesting potential (ARHP) of the campus is estimated by using formula (ARHP = R x AC x RC) given by Pecey, et.al; 1989. The analysis revels that approximate of 75 Lakh Litre water will be collected from the whole campus. Out of that 18.80 Lakh litre water will be collected purely on rooftop of the building and it is directly usable for the drinking and sanitization. It will be fulfil 90 % demand of the fresh water. Out of 74.52 Lakh litre water 55.71 L. Litre water will be useful for the gardening in the dry season. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/survaseeconomics-180110060631-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Harvesting the rainwater for the water conservation and fulfilment of water requirements in the micro level areas with the optimistic method is essential in for better future. Thus the present research aims to identify the potentiality of rainwater harvesting in Dange college campus of Hatkanangale for shrinking the water scarcity.The campus located in rain shadow zone of Western Ghats receives 820.4mm annual average rainfall. It has 4.5 acres of campus with 6090 sq.m. built up area and 2547 sq. m. area of the roof surface. College has 6070 sq.m. area of fruit garden and 7100 sq. m. Play ground. For the present investigation, data regarding various aspects are collected through the college administration office, and skymet website. Runoff Coefficient and Annual rainwater harvesting potential (ARHP) of the campus is estimated by using formula (ARHP = R x AC x RC) given by Pecey, et.al; 1989. The analysis revels that approximate of 75 Lakh Litre water will be collected from the whole campus. Out of that 18.80 Lakh litre water will be collected purely on rooftop of the building and it is directly usable for the drinking and sanitization. It will be fulfil 90 % demand of the fresh water. Out of 74.52 Lakh litre water 55.71 L. Litre water will be useful for the gardening in the dry season.
POTENTIALITY OF RAINWATER HARVESTING IN DANGE COLLEGE CAMPUS OF HATKANANGALE FOR SHRINKING THE WATER SCARCITY from Malhari Survase
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CREATING AWARENESS FOR THE CASHLESS ECONOMY OF INDIA /slideshow/creating-awareness-for-the-cashless-economy-of-india/85953947 awarenessforcashlessindia-180110054402
The dream of the cashless economy becomes unreal due to the lack of awareness of cashless economy and demerits of cash transitions. This paper aims to focus on the significance of awareness among the society for the cashless transitions and reduce the cash transitions. For the same paper, the data and information is collected from newspapers, articles, magazines, internet websites, and expert interviews. The results of demonetization leads to the cashless economy but its effectiveness decreased due to the lack of awareness among the society and created the need of awareness the betterment of Indian economy.]]>

The dream of the cashless economy becomes unreal due to the lack of awareness of cashless economy and demerits of cash transitions. This paper aims to focus on the significance of awareness among the society for the cashless transitions and reduce the cash transitions. For the same paper, the data and information is collected from newspapers, articles, magazines, internet websites, and expert interviews. The results of demonetization leads to the cashless economy but its effectiveness decreased due to the lack of awareness among the society and created the need of awareness the betterment of Indian economy.]]>
Wed, 10 Jan 2018 05:44:02 GMT /slideshow/creating-awareness-for-the-cashless-economy-of-india/85953947 mnsurvase@slideshare.net(mnsurvase) CREATING AWARENESS FOR THE CASHLESS ECONOMY OF INDIA mnsurvase The dream of the cashless economy becomes unreal due to the lack of awareness of cashless economy and demerits of cash transitions. This paper aims to focus on the significance of awareness among the society for the cashless transitions and reduce the cash transitions. For the same paper, the data and information is collected from newspapers, articles, magazines, internet websites, and expert interviews. The results of demonetization leads to the cashless economy but its effectiveness decreased due to the lack of awareness among the society and created the need of awareness the betterment of Indian economy. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/awarenessforcashlessindia-180110054402-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The dream of the cashless economy becomes unreal due to the lack of awareness of cashless economy and demerits of cash transitions. This paper aims to focus on the significance of awareness among the society for the cashless transitions and reduce the cash transitions. For the same paper, the data and information is collected from newspapers, articles, magazines, internet websites, and expert interviews. The results of demonetization leads to the cashless economy but its effectiveness decreased due to the lack of awareness among the society and created the need of awareness the betterment of Indian economy.
CREATING AWARENESS FOR THE CASHLESS ECONOMY OF INDIA from Malhari Survase
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Diagnosis of Soil Texture for Soil Erosion Risk Assessment in Panchaganga Basin /slideshow/diagnosis-of-soil-texture-for-soil-erosion-risk-assessment-in-panchaganga-basin/84971760 balwantcollegevitadepartmentofgeography-171226090157
Soil physical properties plays significant role in the erosion process in the specified region. Thus the present research aims to assess the soil texture as a physical characteristics affecting on the erosion severity in the Panchaganga Basin. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding various aspects of soil obtained from Government Soil Testing Laboratory, Kolhapur. The slope, stream frequency and drainage density along with the soil texture of the region is considered as a responsible factor of erosion response of the soil. The high erosion prone areas of the region mostly have coarse sand and fine sand in soil. The silt and clay soil is relatively low erosion affected.]]>

Soil physical properties plays significant role in the erosion process in the specified region. Thus the present research aims to assess the soil texture as a physical characteristics affecting on the erosion severity in the Panchaganga Basin. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding various aspects of soil obtained from Government Soil Testing Laboratory, Kolhapur. The slope, stream frequency and drainage density along with the soil texture of the region is considered as a responsible factor of erosion response of the soil. The high erosion prone areas of the region mostly have coarse sand and fine sand in soil. The silt and clay soil is relatively low erosion affected.]]>
Tue, 26 Dec 2017 09:01:57 GMT /slideshow/diagnosis-of-soil-texture-for-soil-erosion-risk-assessment-in-panchaganga-basin/84971760 mnsurvase@slideshare.net(mnsurvase) Diagnosis of Soil Texture for Soil Erosion Risk Assessment in Panchaganga Basin mnsurvase Soil physical properties plays significant role in the erosion process in the specified region. Thus the present research aims to assess the soil texture as a physical characteristics affecting on the erosion severity in the Panchaganga Basin. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding various aspects of soil obtained from Government Soil Testing Laboratory, Kolhapur. The slope, stream frequency and drainage density along with the soil texture of the region is considered as a responsible factor of erosion response of the soil. The high erosion prone areas of the region mostly have coarse sand and fine sand in soil. The silt and clay soil is relatively low erosion affected. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/balwantcollegevitadepartmentofgeography-171226090157-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Soil physical properties plays significant role in the erosion process in the specified region. Thus the present research aims to assess the soil texture as a physical characteristics affecting on the erosion severity in the Panchaganga Basin. The selected region for the present investigation is the &#39;Panchaganga Basin&#39; of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding various aspects of soil obtained from Government Soil Testing Laboratory, Kolhapur. The slope, stream frequency and drainage density along with the soil texture of the region is considered as a responsible factor of erosion response of the soil. The high erosion prone areas of the region mostly have coarse sand and fine sand in soil. The silt and clay soil is relatively low erosion affected.
Diagnosis of Soil Texture for Soil Erosion Risk Assessment in Panchaganga Basin from Malhari Survase
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Alkaline Soils and its Improvement in Panchganga Basin (Maharashtra): A Geographical Analysis /slideshow/alkaline-soils-and-its-improvement-in-panchganga-basin-maharashtra-a-geographical-analysis/84971072 alkalinesoilsanditsimprovementinpanchgangabasin-171226084848
The use of land without consideration its limits will result in disturbing soil from its natural or ideal state. Both the physical and chemical properties of soil can be totally or partly altered due to human interference. The economic man always tries to achieve maximum economic gain without consideration of potential problems. These results gradually in deteriorating soil quality. The aims of this paper are to understand distribution, severity and estimating extent of chemically degraded alkaline soils which affect directly on the capacity of soil and environment in the region and suggest suitable conservation measures. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation,both primary and secondary sources are used for this paper. Data regarding different properties of soil and water is collected from Government Soil Survey and Soil Testing Laboratory, Kolhapur and other through field work. Soil analysis has been done and chemical properties of soils are represented by choropleth methods. For this purpose special soil sample data is used. Area of alkali soil is identified with the help of soil chemical and physical properties. Simultaneously field observation and village wise obtained data has been supported. In the study region 46.72% area has covered by alkaline soil. Out of that 31.96% are slightly alkaline and 14.76% are strongly alkaline. Most of the eastern tahsils such as Shirol (94.59%), Hatkanangle (83.33%), Panhala (52.94%) and eastern part of Karveer (45.28%) tahsils have above 40% areas under alkaline soils. As per the risk of alkalinity, the physical, chemical and agronomic measures suggested for the improvement of alkaline soils. ]]>

The use of land without consideration its limits will result in disturbing soil from its natural or ideal state. Both the physical and chemical properties of soil can be totally or partly altered due to human interference. The economic man always tries to achieve maximum economic gain without consideration of potential problems. These results gradually in deteriorating soil quality. The aims of this paper are to understand distribution, severity and estimating extent of chemically degraded alkaline soils which affect directly on the capacity of soil and environment in the region and suggest suitable conservation measures. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation,both primary and secondary sources are used for this paper. Data regarding different properties of soil and water is collected from Government Soil Survey and Soil Testing Laboratory, Kolhapur and other through field work. Soil analysis has been done and chemical properties of soils are represented by choropleth methods. For this purpose special soil sample data is used. Area of alkali soil is identified with the help of soil chemical and physical properties. Simultaneously field observation and village wise obtained data has been supported. In the study region 46.72% area has covered by alkaline soil. Out of that 31.96% are slightly alkaline and 14.76% are strongly alkaline. Most of the eastern tahsils such as Shirol (94.59%), Hatkanangle (83.33%), Panhala (52.94%) and eastern part of Karveer (45.28%) tahsils have above 40% areas under alkaline soils. As per the risk of alkalinity, the physical, chemical and agronomic measures suggested for the improvement of alkaline soils. ]]>
Tue, 26 Dec 2017 08:48:48 GMT /slideshow/alkaline-soils-and-its-improvement-in-panchganga-basin-maharashtra-a-geographical-analysis/84971072 mnsurvase@slideshare.net(mnsurvase) Alkaline Soils and its Improvement in Panchganga Basin (Maharashtra): A Geographical Analysis mnsurvase The use of land without consideration its limits will result in disturbing soil from its natural or ideal state. Both the physical and chemical properties of soil can be totally or partly altered due to human interference. The economic man always tries to achieve maximum economic gain without consideration of potential problems. These results gradually in deteriorating soil quality. The aims of this paper are to understand distribution, severity and estimating extent of chemically degraded alkaline soils which affect directly on the capacity of soil and environment in the region and suggest suitable conservation measures. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation,both primary and secondary sources are used for this paper. Data regarding different properties of soil and water is collected from Government Soil Survey and Soil Testing Laboratory, Kolhapur and other through field work. Soil analysis has been done and chemical properties of soils are represented by choropleth methods. For this purpose special soil sample data is used. Area of alkali soil is identified with the help of soil chemical and physical properties. Simultaneously field observation and village wise obtained data has been supported. In the study region 46.72% area has covered by alkaline soil. Out of that 31.96% are slightly alkaline and 14.76% are strongly alkaline. Most of the eastern tahsils such as Shirol (94.59%), Hatkanangle (83.33%), Panhala (52.94%) and eastern part of Karveer (45.28%) tahsils have above 40% areas under alkaline soils. As per the risk of alkalinity, the physical, chemical and agronomic measures suggested for the improvement of alkaline soils. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/alkalinesoilsanditsimprovementinpanchgangabasin-171226084848-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The use of land without consideration its limits will result in disturbing soil from its natural or ideal state. Both the physical and chemical properties of soil can be totally or partly altered due to human interference. The economic man always tries to achieve maximum economic gain without consideration of potential problems. These results gradually in deteriorating soil quality. The aims of this paper are to understand distribution, severity and estimating extent of chemically degraded alkaline soils which affect directly on the capacity of soil and environment in the region and suggest suitable conservation measures. The selected region for the present investigation is the &#39;Panchaganga Basin&#39; of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation,both primary and secondary sources are used for this paper. Data regarding different properties of soil and water is collected from Government Soil Survey and Soil Testing Laboratory, Kolhapur and other through field work. Soil analysis has been done and chemical properties of soils are represented by choropleth methods. For this purpose special soil sample data is used. Area of alkali soil is identified with the help of soil chemical and physical properties. Simultaneously field observation and village wise obtained data has been supported. In the study region 46.72% area has covered by alkaline soil. Out of that 31.96% are slightly alkaline and 14.76% are strongly alkaline. Most of the eastern tahsils such as Shirol (94.59%), Hatkanangle (83.33%), Panhala (52.94%) and eastern part of Karveer (45.28%) tahsils have above 40% areas under alkaline soils. As per the risk of alkalinity, the physical, chemical and agronomic measures suggested for the improvement of alkaline soils.
Alkaline Soils and its Improvement in Panchganga Basin (Maharashtra): A Geographical Analysis from Malhari Survase
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Geographic Analysis of Erosion Prone Areas and Soil Erosion in Panchaganga Basin /slideshow/geographic-analysis-of-erosion-prone-areas-and-soil-erosion-in-panchaganga-basin/84970923 erosionpaper-171226084559
The main aim of this study is to identify erosion prone areas and nature of soil erosion in Panchaganga Basin of South Maharashtra. The region lies between 160 13N. to 170 11N latitude and 730 41E. to 740 42E longitude, comprise seven tahsils of Kolhapur District i.e. Karveer, Panhala, Shahuwadi, Hatkanagle, Shirol, Gaganbawada and Radhanagari. It covers about 45752.2sq.km area and supports 26, 11,547 populations. For the identification of erosion prone area in the Panchaganga Basin three important components i.e. slope, stream frequency and drainage density has been considered. The SOI toposheets of 1:2,50,000 scale has been divided into 2 cm grids. The slope analysis has been calculated by employing Wentworth method. By marking the values derived from three components of each grid, the erosion proneness has computed and categorized into five distinct spatial units. Such areas ware further checked empirically through field trips. Topsoil loss due to raindrop erosion, rill erosion, formation of gullies, stream channel erosion, etc. is the nature of erosion. Deforestation, overgrazing, monsoonal rainfall of high intensity, hilly landforms, and smooth texture of soil is the major causes of erosion. The area of upper Panchaganga Basin including Radhanagari, Gaganbawada, Panhala, Shahuwadi and some part of Karveer tahsil has been facing acute problem of soil erosion. The reciprocal relationship has been found between slope and eroded areas. It needs to take due care immediately ]]>

The main aim of this study is to identify erosion prone areas and nature of soil erosion in Panchaganga Basin of South Maharashtra. The region lies between 160 13N. to 170 11N latitude and 730 41E. to 740 42E longitude, comprise seven tahsils of Kolhapur District i.e. Karveer, Panhala, Shahuwadi, Hatkanagle, Shirol, Gaganbawada and Radhanagari. It covers about 45752.2sq.km area and supports 26, 11,547 populations. For the identification of erosion prone area in the Panchaganga Basin three important components i.e. slope, stream frequency and drainage density has been considered. The SOI toposheets of 1:2,50,000 scale has been divided into 2 cm grids. The slope analysis has been calculated by employing Wentworth method. By marking the values derived from three components of each grid, the erosion proneness has computed and categorized into five distinct spatial units. Such areas ware further checked empirically through field trips. Topsoil loss due to raindrop erosion, rill erosion, formation of gullies, stream channel erosion, etc. is the nature of erosion. Deforestation, overgrazing, monsoonal rainfall of high intensity, hilly landforms, and smooth texture of soil is the major causes of erosion. The area of upper Panchaganga Basin including Radhanagari, Gaganbawada, Panhala, Shahuwadi and some part of Karveer tahsil has been facing acute problem of soil erosion. The reciprocal relationship has been found between slope and eroded areas. It needs to take due care immediately ]]>
Tue, 26 Dec 2017 08:45:58 GMT /slideshow/geographic-analysis-of-erosion-prone-areas-and-soil-erosion-in-panchaganga-basin/84970923 mnsurvase@slideshare.net(mnsurvase) Geographic Analysis of Erosion Prone Areas and Soil Erosion in Panchaganga Basin mnsurvase The main aim of this study is to identify erosion prone areas and nature of soil erosion in Panchaganga Basin of South Maharashtra. The region lies between 160 13N. to 170 11N latitude and 730 41E. to 740 42E longitude, comprise seven tahsils of Kolhapur District i.e. Karveer, Panhala, Shahuwadi, Hatkanagle, Shirol, Gaganbawada and Radhanagari. It covers about 45752.2sq.km area and supports 26, 11,547 populations. For the identification of erosion prone area in the Panchaganga Basin three important components i.e. slope, stream frequency and drainage density has been considered. The SOI toposheets of 1:2,50,000 scale has been divided into 2 cm grids. The slope analysis has been calculated by employing Wentworth method. By marking the values derived from three components of each grid, the erosion proneness has computed and categorized into five distinct spatial units. Such areas ware further checked empirically through field trips. Topsoil loss due to raindrop erosion, rill erosion, formation of gullies, stream channel erosion, etc. is the nature of erosion. Deforestation, overgrazing, monsoonal rainfall of high intensity, hilly landforms, and smooth texture of soil is the major causes of erosion. The area of upper Panchaganga Basin including Radhanagari, Gaganbawada, Panhala, Shahuwadi and some part of Karveer tahsil has been facing acute problem of soil erosion. The reciprocal relationship has been found between slope and eroded areas. It needs to take due care immediately <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/erosionpaper-171226084559-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The main aim of this study is to identify erosion prone areas and nature of soil erosion in Panchaganga Basin of South Maharashtra. The region lies between 160 13N. to 170 11N latitude and 730 41E. to 740 42E longitude, comprise seven tahsils of Kolhapur District i.e. Karveer, Panhala, Shahuwadi, Hatkanagle, Shirol, Gaganbawada and Radhanagari. It covers about 45752.2sq.km area and supports 26, 11,547 populations. For the identification of erosion prone area in the Panchaganga Basin three important components i.e. slope, stream frequency and drainage density has been considered. The SOI toposheets of 1:2,50,000 scale has been divided into 2 cm grids. The slope analysis has been calculated by employing Wentworth method. By marking the values derived from three components of each grid, the erosion proneness has computed and categorized into five distinct spatial units. Such areas ware further checked empirically through field trips. Topsoil loss due to raindrop erosion, rill erosion, formation of gullies, stream channel erosion, etc. is the nature of erosion. Deforestation, overgrazing, monsoonal rainfall of high intensity, hilly landforms, and smooth texture of soil is the major causes of erosion. The area of upper Panchaganga Basin including Radhanagari, Gaganbawada, Panhala, Shahuwadi and some part of Karveer tahsil has been facing acute problem of soil erosion. The reciprocal relationship has been found between slope and eroded areas. It needs to take due care immediately
Geographic Analysis of Erosion Prone Areas and Soil Erosion in Panchaganga Basin from Malhari Survase
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CHANGING CROPPING PATTERN IN PANCHAGANGA BASIN, MAHARASHTRA: A GEOGRAPHICAL INVESTIGATION /slideshow/changing-cropping-pattern-in-panchaganga-basin-maharashtra-a-geographical-investigation-84970605/84970605 changingcroppingpatterninpanchagangabasin-171226083959
Cropping pattern simply means the proportion of area under different crops at a point of time, whereas changes in cropping pattern refer to change in proportion of area under different crops at two different times. Present paper aims to study cropping pattern and changes therein for individual crops in general and irrigated crops in particular in the region. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under different crops has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1973- 78 and 2003-08. When we include sugarcane, fruits and vegetables, condiments and spices, the total food crops has occupy about 77.43 per cent during the period 2001- 05. Among the non-food crops groundnut shares (9.22%) major area. The share of sugarcane has increased by 10.03 percent on the contrary the share of sereals has decreased by 12.34 percent.]]>

Cropping pattern simply means the proportion of area under different crops at a point of time, whereas changes in cropping pattern refer to change in proportion of area under different crops at two different times. Present paper aims to study cropping pattern and changes therein for individual crops in general and irrigated crops in particular in the region. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under different crops has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1973- 78 and 2003-08. When we include sugarcane, fruits and vegetables, condiments and spices, the total food crops has occupy about 77.43 per cent during the period 2001- 05. Among the non-food crops groundnut shares (9.22%) major area. The share of sugarcane has increased by 10.03 percent on the contrary the share of sereals has decreased by 12.34 percent.]]>
Tue, 26 Dec 2017 08:39:58 GMT /slideshow/changing-cropping-pattern-in-panchaganga-basin-maharashtra-a-geographical-investigation-84970605/84970605 mnsurvase@slideshare.net(mnsurvase) CHANGING CROPPING PATTERN IN PANCHAGANGA BASIN, MAHARASHTRA: A GEOGRAPHICAL INVESTIGATION mnsurvase Cropping pattern simply means the proportion of area under different crops at a point of time, whereas changes in cropping pattern refer to change in proportion of area under different crops at two different times. Present paper aims to study cropping pattern and changes therein for individual crops in general and irrigated crops in particular in the region. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under different crops has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1973- 78 and 2003-08. When we include sugarcane, fruits and vegetables, condiments and spices, the total food crops has occupy about 77.43 per cent during the period 2001- 05. Among the non-food crops groundnut shares (9.22%) major area. The share of sugarcane has increased by 10.03 percent on the contrary the share of sereals has decreased by 12.34 percent. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/changingcroppingpatterninpanchagangabasin-171226083959-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Cropping pattern simply means the proportion of area under different crops at a point of time, whereas changes in cropping pattern refer to change in proportion of area under different crops at two different times. Present paper aims to study cropping pattern and changes therein for individual crops in general and irrigated crops in particular in the region. The selected region for the present investigation is the &#39;Panchaganga Basin&#39; of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under different crops has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1973- 78 and 2003-08. When we include sugarcane, fruits and vegetables, condiments and spices, the total food crops has occupy about 77.43 per cent during the period 2001- 05. Among the non-food crops groundnut shares (9.22%) major area. The share of sugarcane has increased by 10.03 percent on the contrary the share of sereals has decreased by 12.34 percent.
CHANGING CROPPING PATTERN IN PANCHAGANGA BASIN, MAHARASHTRA: A GEOGRAPHICAL INVESTIGATION from Malhari Survase
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A STUDY OF FERTILITY STATUS OF SOIL AND NUTRIENTS RECOMMENDATIONS IN PANCHGANGA BASIN (MAHARASHTRA): A MICRO LEVEL ANALYSIS /mnsurvase/a-study-of-fertility-status-of-soil-and-nutrients-recommendations-in-panchganga-basin-maharashtra-a-micro-level-analysis fertilitystatusandnutrientsrecommendationspresentation-171226083012
The existence of nutrients in soils and its balance determine the growth of plants. Fertility of soils is determined by various macro and micro nutrients available in the soil.In view of this the present study aims to analyse the fertility level of the soil with the help of N. P. & K. and to recommend essential nutrients wherever necessary in Panchganga Basin of south Maharashtra. The Panchganga Basin, a well watered and agriculturally developed region covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. The index values of N, P & K are collected from government soil survey and soil testing Laboratory, Kolhapur at village level. These index values of N. P. & K. are grouped into six categories and tahsil wise areas in percentage in concern category are computed and shown in tabular form. To recognised the fertility level of the soils composite index is computed with the help of NPK values and is grouped into five categories. Simultaneously village level fertility is shown with the help of choropleth maps prepared by using ARC-GIS software. Deficiency and sufficiency of soil nutrients are identified and specific nutrients are recommended wherever necessary. The analysis reveals that there is large variation in the distribution of macronutrients of the soil. It is observed that most of the areas of the study region are fertile in nature. Low and very low fertility of soil is noted in some pockets only. The physiography, climate and agricultural activities have greatly influenced the nutrients status of soil. Specific fertilizers and addition of organic matters are recommended for nutrients deficient areas which will help to keep the balance of nutrients and to restore the fertility of soils. Moreover, it is observed during the fieldwork that the anthropogenic influences are degrading the soils in the region which needs further investigations. ]]>

The existence of nutrients in soils and its balance determine the growth of plants. Fertility of soils is determined by various macro and micro nutrients available in the soil.In view of this the present study aims to analyse the fertility level of the soil with the help of N. P. & K. and to recommend essential nutrients wherever necessary in Panchganga Basin of south Maharashtra. The Panchganga Basin, a well watered and agriculturally developed region covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. The index values of N, P & K are collected from government soil survey and soil testing Laboratory, Kolhapur at village level. These index values of N. P. & K. are grouped into six categories and tahsil wise areas in percentage in concern category are computed and shown in tabular form. To recognised the fertility level of the soils composite index is computed with the help of NPK values and is grouped into five categories. Simultaneously village level fertility is shown with the help of choropleth maps prepared by using ARC-GIS software. Deficiency and sufficiency of soil nutrients are identified and specific nutrients are recommended wherever necessary. The analysis reveals that there is large variation in the distribution of macronutrients of the soil. It is observed that most of the areas of the study region are fertile in nature. Low and very low fertility of soil is noted in some pockets only. The physiography, climate and agricultural activities have greatly influenced the nutrients status of soil. Specific fertilizers and addition of organic matters are recommended for nutrients deficient areas which will help to keep the balance of nutrients and to restore the fertility of soils. Moreover, it is observed during the fieldwork that the anthropogenic influences are degrading the soils in the region which needs further investigations. ]]>
Tue, 26 Dec 2017 08:30:12 GMT /mnsurvase/a-study-of-fertility-status-of-soil-and-nutrients-recommendations-in-panchganga-basin-maharashtra-a-micro-level-analysis mnsurvase@slideshare.net(mnsurvase) A STUDY OF FERTILITY STATUS OF SOIL AND NUTRIENTS RECOMMENDATIONS IN PANCHGANGA BASIN (MAHARASHTRA): A MICRO LEVEL ANALYSIS mnsurvase The existence of nutrients in soils and its balance determine the growth of plants. Fertility of soils is determined by various macro and micro nutrients available in the soil.In view of this the present study aims to analyse the fertility level of the soil with the help of N. P. & K. and to recommend essential nutrients wherever necessary in Panchganga Basin of south Maharashtra. The Panchganga Basin, a well watered and agriculturally developed region covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. The index values of N, P & K are collected from government soil survey and soil testing Laboratory, Kolhapur at village level. These index values of N. P. & K. are grouped into six categories and tahsil wise areas in percentage in concern category are computed and shown in tabular form. To recognised the fertility level of the soils composite index is computed with the help of NPK values and is grouped into five categories. Simultaneously village level fertility is shown with the help of choropleth maps prepared by using ARC-GIS software. Deficiency and sufficiency of soil nutrients are identified and specific nutrients are recommended wherever necessary. The analysis reveals that there is large variation in the distribution of macronutrients of the soil. It is observed that most of the areas of the study region are fertile in nature. Low and very low fertility of soil is noted in some pockets only. The physiography, climate and agricultural activities have greatly influenced the nutrients status of soil. Specific fertilizers and addition of organic matters are recommended for nutrients deficient areas which will help to keep the balance of nutrients and to restore the fertility of soils. Moreover, it is observed during the fieldwork that the anthropogenic influences are degrading the soils in the region which needs further investigations. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/fertilitystatusandnutrientsrecommendationspresentation-171226083012-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The existence of nutrients in soils and its balance determine the growth of plants. Fertility of soils is determined by various macro and micro nutrients available in the soil.In view of this the present study aims to analyse the fertility level of the soil with the help of N. P. &amp; K. and to recommend essential nutrients wherever necessary in Panchganga Basin of south Maharashtra. The Panchganga Basin, a well watered and agriculturally developed region covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. The index values of N, P &amp; K are collected from government soil survey and soil testing Laboratory, Kolhapur at village level. These index values of N. P. &amp; K. are grouped into six categories and tahsil wise areas in percentage in concern category are computed and shown in tabular form. To recognised the fertility level of the soils composite index is computed with the help of NPK values and is grouped into five categories. Simultaneously village level fertility is shown with the help of choropleth maps prepared by using ARC-GIS software. Deficiency and sufficiency of soil nutrients are identified and specific nutrients are recommended wherever necessary. The analysis reveals that there is large variation in the distribution of macronutrients of the soil. It is observed that most of the areas of the study region are fertile in nature. Low and very low fertility of soil is noted in some pockets only. The physiography, climate and agricultural activities have greatly influenced the nutrients status of soil. Specific fertilizers and addition of organic matters are recommended for nutrients deficient areas which will help to keep the balance of nutrients and to restore the fertility of soils. Moreover, it is observed during the fieldwork that the anthropogenic influences are degrading the soils in the region which needs further investigations.
A STUDY OF FERTILITY STATUS OF SOIL AND NUTRIENTS RECOMMENDATIONS IN PANCHGANGA BASIN (MAHARASHTRA): A MICRO LEVEL ANALYSIS from Malhari Survase
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Diagnosis & Improvement of Degraded Soils in Panchaganga Basin (Maharashtra): 鐃A Micro Level Analysis /slideshow/diagnosis-improvement-of-degraded-soils-in-panchaganga-basin-maharashtra-a-micro-level-analysis/84969785 survasem-171226082445
The chemical properties of soil perform significant functions in crop growth. The chemical processes and reactions transform the soil properties from ideal to worst in the chemical degradation of soil. The use of soil without considering its limits, make it difficult to supply essential elements for crops resulting into declining the agricultural productivity. Hence the present investigation aims to analyse the nature, extent and gravity of chemically degraded soils and recommend suitable reclamation measures in Panchganga basin. It is well watered and agriculturally developed part of the state which covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. For the present investigation required village level data has been collected from Govt. Soil Survey and Soil Testing Laboratory, Kolhapur and supported by intensive field trips and interviews of the farmers. The extent and gravity of acidic, alkaline, saline, sodic and saline sodic soils are identified with the help of soil chemical analysis. The results obtained are represented through tables and choropleth map. The analyses reveal that the soils in the western hilly and high rainfall parts are mostly acidic in nature. By contrast the soils in the eastern plain areas are mostly alkaline, saline and saline sodic. This can be well attributed to the plain topography, low natural drainage, monoculture of sugarcane, unscientific practices of cultivation, excessive use of chemical fertilizers and irrigation etc. As a result the soil fertility has declined and hundreds of hectares of fertile soils have gone out of cultivation. To reclaims such soils site specific recommendations such as physical, chemical, agronomic and biological measures need be implemented immediately to reverse soil degradation process and to restore the valuable soil resource of the region.]]>

The chemical properties of soil perform significant functions in crop growth. The chemical processes and reactions transform the soil properties from ideal to worst in the chemical degradation of soil. The use of soil without considering its limits, make it difficult to supply essential elements for crops resulting into declining the agricultural productivity. Hence the present investigation aims to analyse the nature, extent and gravity of chemically degraded soils and recommend suitable reclamation measures in Panchganga basin. It is well watered and agriculturally developed part of the state which covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. For the present investigation required village level data has been collected from Govt. Soil Survey and Soil Testing Laboratory, Kolhapur and supported by intensive field trips and interviews of the farmers. The extent and gravity of acidic, alkaline, saline, sodic and saline sodic soils are identified with the help of soil chemical analysis. The results obtained are represented through tables and choropleth map. The analyses reveal that the soils in the western hilly and high rainfall parts are mostly acidic in nature. By contrast the soils in the eastern plain areas are mostly alkaline, saline and saline sodic. This can be well attributed to the plain topography, low natural drainage, monoculture of sugarcane, unscientific practices of cultivation, excessive use of chemical fertilizers and irrigation etc. As a result the soil fertility has declined and hundreds of hectares of fertile soils have gone out of cultivation. To reclaims such soils site specific recommendations such as physical, chemical, agronomic and biological measures need be implemented immediately to reverse soil degradation process and to restore the valuable soil resource of the region.]]>
Tue, 26 Dec 2017 08:24:45 GMT /slideshow/diagnosis-improvement-of-degraded-soils-in-panchaganga-basin-maharashtra-a-micro-level-analysis/84969785 mnsurvase@slideshare.net(mnsurvase) Diagnosis & Improvement of Degraded Soils in Panchaganga Basin (Maharashtra): 鐃A Micro Level Analysis mnsurvase The chemical properties of soil perform significant functions in crop growth. The chemical processes and reactions transform the soil properties from ideal to worst in the chemical degradation of soil. The use of soil without considering its limits, make it difficult to supply essential elements for crops resulting into declining the agricultural productivity. Hence the present investigation aims to analyse the nature, extent and gravity of chemically degraded soils and recommend suitable reclamation measures in Panchganga basin. It is well watered and agriculturally developed part of the state which covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. For the present investigation required village level data has been collected from Govt. Soil Survey and Soil Testing Laboratory, Kolhapur and supported by intensive field trips and interviews of the farmers. The extent and gravity of acidic, alkaline, saline, sodic and saline sodic soils are identified with the help of soil chemical analysis. The results obtained are represented through tables and choropleth map. The analyses reveal that the soils in the western hilly and high rainfall parts are mostly acidic in nature. By contrast the soils in the eastern plain areas are mostly alkaline, saline and saline sodic. This can be well attributed to the plain topography, low natural drainage, monoculture of sugarcane, unscientific practices of cultivation, excessive use of chemical fertilizers and irrigation etc. As a result the soil fertility has declined and hundreds of hectares of fertile soils have gone out of cultivation. To reclaims such soils site specific recommendations such as physical, chemical, agronomic and biological measures need be implemented immediately to reverse soil degradation process and to restore the valuable soil resource of the region. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/survasem-171226082445-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The chemical properties of soil perform significant functions in crop growth. The chemical processes and reactions transform the soil properties from ideal to worst in the chemical degradation of soil. The use of soil without considering its limits, make it difficult to supply essential elements for crops resulting into declining the agricultural productivity. Hence the present investigation aims to analyse the nature, extent and gravity of chemically degraded soils and recommend suitable reclamation measures in Panchganga basin. It is well watered and agriculturally developed part of the state which covers 45752.2 sq.km area and supports 26, 11,547 (2.6 percent of state) population. For the present investigation required village level data has been collected from Govt. Soil Survey and Soil Testing Laboratory, Kolhapur and supported by intensive field trips and interviews of the farmers. The extent and gravity of acidic, alkaline, saline, sodic and saline sodic soils are identified with the help of soil chemical analysis. The results obtained are represented through tables and choropleth map. The analyses reveal that the soils in the western hilly and high rainfall parts are mostly acidic in nature. By contrast the soils in the eastern plain areas are mostly alkaline, saline and saline sodic. This can be well attributed to the plain topography, low natural drainage, monoculture of sugarcane, unscientific practices of cultivation, excessive use of chemical fertilizers and irrigation etc. As a result the soil fertility has declined and hundreds of hectares of fertile soils have gone out of cultivation. To reclaims such soils site specific recommendations such as physical, chemical, agronomic and biological measures need be implemented immediately to reverse soil degradation process and to restore the valuable soil resource of the region.
Diagnosis & Improvement of Degraded Soils in Panchaganga Basin (Maharashtra): A Micro Level Analysis from Malhari Survase
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Irrigation development in panchaganga basin /slideshow/irrigation-development-in-panchaganga-basin/84969610 irrigationdevelopmentinpanchagangabasin-171226082131
Irrigation plays significant role in transforming the agricultural activity and the rural livelihood. Thus the present research aims to assess the growth of irrigated area under different sources of irrigation, along with the consideration of methods of 測irrigation applied changes in source of irrigation and intensity of irrigation in the Panchaganga Basin. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under irrigation with different sources has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1971- 75 and 2001-05 and supported by intensive field trips. It is noteworthy increased the area under the irrigation in the study region throughout the period under review. The area under well irrigation has increased by 46158 hectors and lift by 6950 hectors. The intensity of irrigation is about 25.1%. During the period under review it increased by 9.2%. The various sources of irrigation bring changes in attitude of the farmers and adopted the new and scientific techniques for the agricultural development. ]]>

Irrigation plays significant role in transforming the agricultural activity and the rural livelihood. Thus the present research aims to assess the growth of irrigated area under different sources of irrigation, along with the consideration of methods of 測irrigation applied changes in source of irrigation and intensity of irrigation in the Panchaganga Basin. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under irrigation with different sources has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1971- 75 and 2001-05 and supported by intensive field trips. It is noteworthy increased the area under the irrigation in the study region throughout the period under review. The area under well irrigation has increased by 46158 hectors and lift by 6950 hectors. The intensity of irrigation is about 25.1%. During the period under review it increased by 9.2%. The various sources of irrigation bring changes in attitude of the farmers and adopted the new and scientific techniques for the agricultural development. ]]>
Tue, 26 Dec 2017 08:21:31 GMT /slideshow/irrigation-development-in-panchaganga-basin/84969610 mnsurvase@slideshare.net(mnsurvase) Irrigation development in panchaganga basin mnsurvase Irrigation plays significant role in transforming the agricultural activity and the rural livelihood. Thus the present research aims to assess the growth of irrigated area under different sources of irrigation, along with the consideration of methods of 測irrigation applied changes in source of irrigation and intensity of irrigation in the Panchaganga Basin. The selected region for the present investigation is the 'Panchaganga Basin' of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under irrigation with different sources has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1971- 75 and 2001-05 and supported by intensive field trips. It is noteworthy increased the area under the irrigation in the study region throughout the period under review. The area under well irrigation has increased by 46158 hectors and lift by 6950 hectors. The intensity of irrigation is about 25.1%. During the period under review it increased by 9.2%. The various sources of irrigation bring changes in attitude of the farmers and adopted the new and scientific techniques for the agricultural development. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/irrigationdevelopmentinpanchagangabasin-171226082131-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Irrigation plays significant role in transforming the agricultural activity and the rural livelihood. Thus the present research aims to assess the growth of irrigated area under different sources of irrigation, along with the consideration of methods of 測irrigation applied changes in source of irrigation and intensity of irrigation in the Panchaganga Basin. The selected region for the present investigation is the &#39;Panchaganga Basin&#39; of south Maharashtra state comprising 7 tahsils of Kolhapur district, Maharashtra. For the present investigation, data regarding area under irrigation with different sources has been compiled from Socio-Economic Review and District Statistical Abstracts of Kolhapur District, 1971- 75 and 2001-05 and supported by intensive field trips. It is noteworthy increased the area under the irrigation in the study region throughout the period under review. The area under well irrigation has increased by 46158 hectors and lift by 6950 hectors. The intensity of irrigation is about 25.1%. During the period under review it increased by 9.2%. The various sources of irrigation bring changes in attitude of the farmers and adopted the new and scientific techniques for the agricultural development.
Irrigation development in panchaganga basin from Malhari Survase
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