ºÝºÝߣshows by User: afmfreire62 / http://www.slideshare.net/images/logo.gif ºÝºÝߣshows by User: afmfreire62 / Sat, 31 Oct 2020 20:38:22 GMT ºÝºÝߣShare feed for ºÝºÝߣshows by User: afmfreire62 Egg10086 aula 07-densidade e pe_2020-1 https://pt.slideshare.net/slideshow/egg10086-aula-07densidade-e-pe20201/239036671 egg10086aula-07densidadeepe2020-1-201031203822
Perfis de Densidade e Fator Fotoelétrico]]>
Perfis de Densidade e Fator Fotoelétrico]]> Sat, 31 Oct 2020 20:38:22 GMT https://pt.slideshare.net/slideshow/egg10086-aula-07densidade-e-pe20201/239036671 afmfreire62@slideshare.net(afmfreire62) Egg10086 aula 07-densidade e pe_2020-1 afmfreire62 Perfis de Densidade e Fator Fotoelétrico <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-07densidadeepe2020-1-201031203822-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Perfis de Densidade e Fator Fotoelétrico
from Fernando Freire
]]> 242 0 https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-07densidadeepe2020-1-201031203822-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Egg10086 aula 06-dipmeter_2020-1 https://pt.slideshare.net/slideshow/egg10086-aula-06dipmeter20201/239036667 egg10086aula-06dipmeter2020-1-201031203720
Perfil Dipmeter]]>
Perfil Dipmeter]]> Sat, 31 Oct 2020 20:37:20 GMT https://pt.slideshare.net/slideshow/egg10086-aula-06dipmeter20201/239036667 afmfreire62@slideshare.net(afmfreire62) Egg10086 aula 06-dipmeter_2020-1 afmfreire62 Perfil Dipmeter <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-06dipmeter2020-1-201031203720-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Perfil Dipmeter
from Fernando Freire
]]> 97 1 https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-06dipmeter2020-1-201031203720-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Egg10086 aula 05-resistividade_2020-1 https://pt.slideshare.net/slideshow/egg10086-aula-05resistividade20201/239036662 egg10086aula-05resistividade2020-1-201031203618
Perfis de Resistividade]]>
Perfis de Resistividade]]> Sat, 31 Oct 2020 20:36:18 GMT https://pt.slideshare.net/slideshow/egg10086-aula-05resistividade20201/239036662 afmfreire62@slideshare.net(afmfreire62) Egg10086 aula 05-resistividade_2020-1 afmfreire62 Perfis de Resistividade <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-05resistividade2020-1-201031203618-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Perfis de Resistividade
from Fernando Freire
]]> 312 0 https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-05resistividade2020-1-201031203618-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Egg10086 aula 04-gr e gr espectral_2020-1 https://pt.slideshare.net/slideshow/egg10086-aula-04gr-e-gr-espectral20201/239036654 egg10086aula-04gregrespectral2020-1-201031203454
Gamma Ray and Spectral Gamma Ray]]>
Gamma Ray and Spectral Gamma Ray]]> Sat, 31 Oct 2020 20:34:54 GMT https://pt.slideshare.net/slideshow/egg10086-aula-04gr-e-gr-espectral20201/239036654 afmfreire62@slideshare.net(afmfreire62) Egg10086 aula 04-gr e gr espectral_2020-1 afmfreire62 Gamma Ray and Spectral Gamma Ray <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-04gregrespectral2020-1-201031203454-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Gamma Ray and Spectral Gamma Ray
from Fernando Freire
]]> 92 0 https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-04gregrespectral2020-1-201031203454-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Egg10086 aula 02-caliper_2020-1 https://pt.slideshare.net/slideshow/egg10086-aula-02caliper20201/239024838 egg10086aula-02caliper2020-1-201030223615
Perfil Caliper]]>
Perfil Caliper]]> Fri, 30 Oct 2020 22:36:15 GMT https://pt.slideshare.net/slideshow/egg10086-aula-02caliper20201/239024838 afmfreire62@slideshare.net(afmfreire62) Egg10086 aula 02-caliper_2020-1 afmfreire62 Perfil Caliper <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-02caliper2020-1-201030223615-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Perfil Caliper
from Fernando Freire
]]> 69 1 https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-02caliper2020-1-201030223615-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Freire ALAGO 2017-06-21 /slideshow/freire-alago-20170621/77414208 freirealago2017-06-21-170701013803
Natural gas hydrates are solids formed by the combination of water and gases, which may be hydrocarbons or not. It has the appearance of snow or dry ice and crystallizes in the form of nodules, layers or within faults and in the porous space of marine sediments. They are distributed along the continental margins around the world or in permafrost zones, located in the polar circles. Hydrates originate through the movement of gaseous molecules during migration within the sedimentary column or in the water, through an exothermic reaction that freezes the water immediately surrounding each gas molecule. This molecule, usually methane, is then trapped within a crystalline structure composed of a trap of water molecules. For this reason, hydrates are also known as methane clathrates. However, other natural components such as ethane, propane and carbon dioxide can be observed in this form. The maximum temperature for this structure to be stable depends on the combination of temperature and pressure in the gas hydrate stability zone and, secondarily, on the composition of the gas and the salinity of the water contained in the pores of marine sediment. Methane, trapped as a hydrate, may be biogenic or thermogenic. Experimental studies indicate that 1 m3 of methane hydrate, dissociated under pressure and atmospheric temperature, releases 164 m3 of natural methane, in addition to 0.8 m3 of fresh water. For this reason, estimates of the amount of natural gas contained in hydrates far exceed the known reserves of natural gas in the world, ranging from 105 trillion cubic feet (TCF) to more than 3x109 TCF. The volume of carbon contained in this form is estimated to be twice the total amount of all the earth's fossil organic carbon, including oil, gas, and coal. Gas hydrates have been attracting interest as a potential energy resource, in addition to being considered as a possible cause of greenhouse effect and of instability of marine slopes. However, little is known about the factors controlling the formation and stability of hydrates on the marine seafloor, although significant advances have been achieved thanks to the continued study of the subject by academies and research institutions. The interaction between gas hydrates dissociation and methane plumes at the seawater column is a natural phenomenon that modifies seafloor scenario, transforming the landscape by the precipitation of carbonates and pyrite on the shallow sedimentary pores, resulting in nucleous of hardgrounds for living benthic organisms, known as chemosynthetic communities. For this reason, methane seeps related with gas hydrates dissociation creates a micro environment for living species, important for the marine ecosystem. This is an open and exciting study field for geologists, geochemical researchers and biologists.]]>
Natural gas hydrates are solids formed by the combination of water and gases, which may be hydrocarbons or not. It has the appearance of snow or dry ice and crystallizes in the form of nodules, layers or within faults and in the porous space of marine sediments. They are distributed along the continental margins around the world or in permafrost zones, located in the polar circles. Hydrates originate through the movement of gaseous molecules during migration within the sedimentary column or in the water, through an exothermic reaction that freezes the water immediately surrounding each gas molecule. This molecule, usually methane, is then trapped within a crystalline structure composed of a trap of water molecules. For this reason, hydrates are also known as methane clathrates. However, other natural components such as ethane, propane and carbon dioxide can be observed in this form. The maximum temperature for this structure to be stable depends on the combination of temperature and pressure in the gas hydrate stability zone and, secondarily, on the composition of the gas and the salinity of the water contained in the pores of marine sediment. Methane, trapped as a hydrate, may be biogenic or thermogenic. Experimental studies indicate that 1 m3 of methane hydrate, dissociated under pressure and atmospheric temperature, releases 164 m3 of natural methane, in addition to 0.8 m3 of fresh water. For this reason, estimates of the amount of natural gas contained in hydrates far exceed the known reserves of natural gas in the world, ranging from 105 trillion cubic feet (TCF) to more than 3x109 TCF. The volume of carbon contained in this form is estimated to be twice the total amount of all the earth's fossil organic carbon, including oil, gas, and coal. Gas hydrates have been attracting interest as a potential energy resource, in addition to being considered as a possible cause of greenhouse effect and of instability of marine slopes. However, little is known about the factors controlling the formation and stability of hydrates on the marine seafloor, although significant advances have been achieved thanks to the continued study of the subject by academies and research institutions. The interaction between gas hydrates dissociation and methane plumes at the seawater column is a natural phenomenon that modifies seafloor scenario, transforming the landscape by the precipitation of carbonates and pyrite on the shallow sedimentary pores, resulting in nucleous of hardgrounds for living benthic organisms, known as chemosynthetic communities. For this reason, methane seeps related with gas hydrates dissociation creates a micro environment for living species, important for the marine ecosystem. This is an open and exciting study field for geologists, geochemical researchers and biologists.]]> Sat, 01 Jul 2017 01:38:02 GMT /slideshow/freire-alago-20170621/77414208 afmfreire62@slideshare.net(afmfreire62) Freire ALAGO 2017-06-21 afmfreire62 Natural gas hydrates are solids formed by the combination of water and gases, which may be hydrocarbons or not. It has the appearance of snow or dry ice and crystallizes in the form of nodules, layers or within faults and in the porous space of marine sediments. They are distributed along the continental margins around the world or in permafrost zones, located in the polar circles. Hydrates originate through the movement of gaseous molecules during migration within the sedimentary column or in the water, through an exothermic reaction that freezes the water immediately surrounding each gas molecule. This molecule, usually methane, is then trapped within a crystalline structure composed of a trap of water molecules. For this reason, hydrates are also known as methane clathrates. However, other natural components such as ethane, propane and carbon dioxide can be observed in this form. The maximum temperature for this structure to be stable depends on the combination of temperature and pressure in the gas hydrate stability zone and, secondarily, on the composition of the gas and the salinity of the water contained in the pores of marine sediment. Methane, trapped as a hydrate, may be biogenic or thermogenic. Experimental studies indicate that 1 m3 of methane hydrate, dissociated under pressure and atmospheric temperature, releases 164 m3 of natural methane, in addition to 0.8 m3 of fresh water. For this reason, estimates of the amount of natural gas contained in hydrates far exceed the known reserves of natural gas in the world, ranging from 105 trillion cubic feet (TCF) to more than 3x109 TCF. The volume of carbon contained in this form is estimated to be twice the total amount of all the earth's fossil organic carbon, including oil, gas, and coal. Gas hydrates have been attracting interest as a potential energy resource, in addition to being considered as a possible cause of greenhouse effect and of instability of marine slopes. However, little is known about the factors controlling the formation and stability of hydrates on the marine seafloor, although significant advances have been achieved thanks to the continued study of the subject by academies and research institutions. The interaction between gas hydrates dissociation and methane plumes at the seawater column is a natural phenomenon that modifies seafloor scenario, transforming the landscape by the precipitation of carbonates and pyrite on the shallow sedimentary pores, resulting in nucleous of hardgrounds for living benthic organisms, known as chemosynthetic communities. For this reason, methane seeps related with gas hydrates dissociation creates a micro environment for living species, important for the marine ecosystem. This is an open and exciting study field for geologists, geochemical researchers and biologists. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/freirealago2017-06-21-170701013803-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Natural gas hydrates are solids formed by the combination of water and gases, which may be hydrocarbons or not. It has the appearance of snow or dry ice and crystallizes in the form of nodules, layers or within faults and in the porous space of marine sediments. They are distributed along the continental margins around the world or in permafrost zones, located in the polar circles. Hydrates originate through the movement of gaseous molecules during migration within the sedimentary column or in the water, through an exothermic reaction that freezes the water immediately surrounding each gas molecule. This molecule, usually methane, is then trapped within a crystalline structure composed of a trap of water molecules. For this reason, hydrates are also known as methane clathrates. However, other natural components such as ethane, propane and carbon dioxide can be observed in this form. The maximum temperature for this structure to be stable depends on the combination of temperature and pressure in the gas hydrate stability zone and, secondarily, on the composition of the gas and the salinity of the water contained in the pores of marine sediment. Methane, trapped as a hydrate, may be biogenic or thermogenic. Experimental studies indicate that 1 m3 of methane hydrate, dissociated under pressure and atmospheric temperature, releases 164 m3 of natural methane, in addition to 0.8 m3 of fresh water. For this reason, estimates of the amount of natural gas contained in hydrates far exceed the known reserves of natural gas in the world, ranging from 105 trillion cubic feet (TCF) to more than 3x109 TCF. The volume of carbon contained in this form is estimated to be twice the total amount of all the earth&#39;s fossil organic carbon, including oil, gas, and coal. Gas hydrates have been attracting interest as a potential energy resource, in addition to being considered as a possible cause of greenhouse effect and of instability of marine slopes. However, little is known about the factors controlling the formation and stability of hydrates on the marine seafloor, although significant advances have been achieved thanks to the continued study of the subject by academies and research institutions. The interaction between gas hydrates dissociation and methane plumes at the seawater column is a natural phenomenon that modifies seafloor scenario, transforming the landscape by the precipitation of carbonates and pyrite on the shallow sedimentary pores, resulting in nucleous of hardgrounds for living benthic organisms, known as chemosynthetic communities. For this reason, methane seeps related with gas hydrates dissociation creates a micro environment for living species, important for the marine ecosystem. This is an open and exciting study field for geologists, geochemical researchers and biologists.
Freire ALAGO 2017-06-21 from Fernando Freire
]]> 280 6 https://cdn.slidesharecdn.com/ss_thumbnails/freirealago2017-06-21-170701013803-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Correlacao de eventos tectônico-magmático-deposicionais das principais bacias sedimentares brasileiras https://pt.slideshare.net/slideshow/correlacao-de-eventos-tectnicomagmticodeposicionais-das-principais-bacias-sedimentares-brasileiras/71500688 correlacaodeeventos-170129000419
Poster apresentado durante o 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012)]]>
Poster apresentado durante o 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012)]]> Sun, 29 Jan 2017 00:04:19 GMT https://pt.slideshare.net/slideshow/correlacao-de-eventos-tectnicomagmticodeposicionais-das-principais-bacias-sedimentares-brasileiras/71500688 afmfreire62@slideshare.net(afmfreire62) Correlacao de eventos tectônico-magmático-deposicionais das principais bacias sedimentares brasileiras afmfreire62 Poster apresentado durante o 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012) <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/correlacaodeeventos-170129000419-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Poster apresentado durante o 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012)
from Fernando Freire
]]> 112 3 https://cdn.slidesharecdn.com/ss_thumbnails/correlacaodeeventos-170129000419-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 #46 cgb forum f4 https://pt.slideshare.net/slideshow/46-cgb-forum-f4/71500633 46cgbforumf4-170128235821
Apresentação no 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012)]]>
Apresentação no 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012)]]> Sat, 28 Jan 2017 23:58:21 GMT https://pt.slideshare.net/slideshow/46-cgb-forum-f4/71500633 afmfreire62@slideshare.net(afmfreire62) #46 cgb forum f4 afmfreire62 Apresentação no 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012) <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/46cgbforumf4-170128235821-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Apresentação no 46º Congresso Brasileiro de Geologia, Santos-SP, Brasil (2012)
from Fernando Freire
]]> 218 2 https://cdn.slidesharecdn.com/ss_thumbnails/46cgbforumf4-170128235821-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Integrated Study Low Res /slideshow/integrated-study-low-res/15578624 integratedstudylowres-13551795495431-phpapp02-121210164648-phpapp01
Poster presented during the AAPG 2008 at Cape Town, South Africa]]>
Poster presented during the AAPG 2008 at Cape Town, South Africa]]> Mon, 10 Dec 2012 16:46:41 GMT /slideshow/integrated-study-low-res/15578624 afmfreire62@slideshare.net(afmfreire62) Integrated Study Low Res afmfreire62 Poster presented during the AAPG 2008 at Cape Town, South Africa <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/integratedstudylowres-13551795495431-phpapp02-121210164648-phpapp01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Poster presented during the AAPG 2008 at Cape Town, South Africa
Integrated Study Low Res from Fernando Freire
]]> 155 4 https://cdn.slidesharecdn.com/ss_thumbnails/integratedstudylowres-13551795495431-phpapp02-121210164648-phpapp01-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Correlacao De Eventos Low Res https://pt.slideshare.net/slideshow/correlacao-de-eventos-low-res/15550942 correlacaodeeventoslowres-13550008747399-phpapp01-121208150938-phpapp02
Presented during the 46th Brazilian Geological Congress, Santos, 2012]]>
Presented during the 46th Brazilian Geological Congress, Santos, 2012]]> Sat, 08 Dec 2012 15:09:10 GMT https://pt.slideshare.net/slideshow/correlacao-de-eventos-low-res/15550942 afmfreire62@slideshare.net(afmfreire62) Correlacao De Eventos Low Res afmfreire62 Presented during the 46th Brazilian Geological Congress, Santos, 2012 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/correlacaodeeventoslowres-13550008747399-phpapp01-121208150938-phpapp02-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presented during the 46th Brazilian Geological Congress, Santos, 2012
from Fernando Freire
]]> 473 2 https://cdn.slidesharecdn.com/ss_thumbnails/correlacaodeeventoslowres-13550008747399-phpapp01-121208150938-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Poster 6th ICGH 2008 /slideshow/poster-6th-icgh-2008/15550818 postericgh2008a0-13550000830172-phpapp01-121208145601-phpapp02
Presented during the 6th International Conference on Gas Hydrates, Vancouver, Canada, 2008]]>
Presented during the 6th International Conference on Gas Hydrates, Vancouver, Canada, 2008]]> Sat, 08 Dec 2012 14:55:58 GMT /slideshow/poster-6th-icgh-2008/15550818 afmfreire62@slideshare.net(afmfreire62) Poster 6th ICGH 2008 afmfreire62 Presented during the 6th International Conference on Gas Hydrates, Vancouver, Canada, 2008 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/postericgh2008a0-13550000830172-phpapp01-121208145601-phpapp02-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presented during the 6th International Conference on Gas Hydrates, Vancouver, Canada, 2008
Poster 6th ICGH 2008 from Fernando Freire
]]> 413 5 https://cdn.slidesharecdn.com/ss_thumbnails/postericgh2008a0-13550000830172-phpapp01-121208145601-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 http://www.46cbg.com.br/0510/terra/08h30_1_antonio_freire_05-10_slterra.pdf https://pt.slideshare.net/slideshow/presentation-about-gas-hydrates/15550158 08h301antoniofreire0510slterra-1354995682411-phpapp01-121208134320-phpapp01
Presentation during the 46º Brazilian Geological Congress, Special Forum F-4]]>
Presentation during the 46º Brazilian Geological Congress, Special Forum F-4]]> Sat, 08 Dec 2012 13:43:08 GMT https://pt.slideshare.net/slideshow/presentation-about-gas-hydrates/15550158 afmfreire62@slideshare.net(afmfreire62) http://www.46cbg.com.br/0510/terra/08h30_1_antonio_freire_05-10_slterra.pdf afmfreire62 Presentation during the 46º Brazilian Geological Congress, Special Forum F-4 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/08h301antoniofreire0510slterra-1354995682411-phpapp01-121208134320-phpapp01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presentation during the 46º Brazilian Geological Congress, Special Forum F-4
from Fernando Freire
]]> 686 2 https://cdn.slidesharecdn.com/ss_thumbnails/08h301antoniofreire0510slterra-1354995682411-phpapp01-121208134320-phpapp01-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 https://cdn.slidesharecdn.com/profile-photo-afmfreire62-48x48.jpg?cb=1604176371 www.researchgate.net/profile/Fernando_Freire10 https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-07densidadeepe2020-1-201031203822-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/egg10086-aula-07densidade-e-pe20201/239036671 Egg10086 aula 07-densi... https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-06dipmeter2020-1-201031203720-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/egg10086-aula-06dipmeter20201/239036667 Egg10086 aula 06-dipme... https://cdn.slidesharecdn.com/ss_thumbnails/egg10086aula-05resistividade2020-1-201031203618-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/egg10086-aula-05resistividade20201/239036662 Egg10086 aula 05-resis...