The document summarizes a study on identifying anthropogenic factors contributing to flood events in Palembang City, Indonesia. Field surveys found that flooding occurred in areas not predicted to flood based on hydraulic modeling, indicating anthropogenic influences. Community perceptions suggested flooding was caused by both natural and human factors, including insufficient drainage capacity, waste clogging channels, and disconnected drainage systems. The study concluded that flood risk assessments need to consider both natural hazards and how human activities can exacerbate flooding.
This document provides an overview of floods including causes, effects, types, and management. It begins with an introduction to floods and then discusses the main causes of floods such as intense rainfall, topography, obstruction of river flows, and sedimentation. The effects of floods are categorized as primary, secondary, and tertiary. The types of floods covered are coastal floods, river floods, and flash floods. Flood management techniques include both hard engineering methods like embankments and dams as well as soft engineering methods like flood plain zoning and forecasting. A case study on the 2013 Uttarakhand floods in India details the impacts and damage caused by heavy rainfall and landslides in the region. In conclusion, some benefits of floods are
Cambodia Groundwater Irrigation - Exec SummaryMichael Roberts
油
This document summarizes a thesis on the physical and socioeconomic impacts of groundwater irrigation in Cambodia's Mekong Delta region. Physical investigations found that increased pumping is lowering the water table and could lead to saltwater contamination if not managed properly. Socioeconomic studies show groundwater irrigation benefits wealthy farmers most and may harm poorer communities as water tables decline. The author recommends controlling groundwater use, preparing for lower water tables, and further monitoring and research.
Integrated application of HEC-RAS and GIS and RS for flood risk assessment i...inventionjournals
油
International Journal of Engineering and Science Invention (IJESI) is an international journal intended for professionals and researchers in all fields of computer science and electronics. IJESI publishes research articles and reviews within the whole field Engineering Science and Technology, new teaching methods, assessment, validation and the impact of new technologies and it will continue to provide information on the latest trends and developments in this ever-expanding subject. The publications of papers are selected through double peer reviewed to ensure originality, relevance, and readability. The articles published in our journal can be accessed online.
Hydrogeological parameters refer to the physical and hydraulic characteristics of subsurface materials (e.g., soil, rock, aquifers) that affect the movement, storage, and availability of groundwater. These parameters are essential for understanding and modeling groundwater flow and contaminant transport. Here are some of the key hydrogeological parameters:
1. Porosity (n)
Definition: The ratio of void space (pores) in a material to the total volume.
Significance: Determines how much water a material can store.
Types:
Total porosity: Includes all pore spaces.
Effective porosity: The portion of porosity that contributes to fluid flow.
2. Permeability (k)
Definition: The ability of a material to transmit fluids through its pore spaces.
Significance: Higher permeability means easier water movement. It is usually measured in Darcy or millidarcy.
3. Hydraulic Conductivity (K)
Definition: The rate at which water can move through a permeable medium.
Units: Often measured in meters per second (m/s) or meters per day (m/day).
Significance: Higher hydraulic conductivity implies higher ease of groundwater movement.
4. Transmissivity (T)
Definition: The rate at which groundwater can move through an aquifer section of unit width.
Formula:
=
T=Kb, where
b is the saturated thickness of the aquifer.
Significance: Important for assessing the ability of an aquifer to supply water.
5. Storage Coefficient (S)
Definition: The amount of water released or stored per unit area of the aquifer per unit change in head (typically used in confined aquifers).
Significance: Indicates how much water an aquifer can yield or store in response to pressure changes.
6. Specific Yield (Sy)
Definition: The volume of water that a saturated material will yield by gravity per unit volume of the material.
Significance: Relevant for unconfined aquifers and determines the amount of water available for use.
7. Specific Retention (Sr)
Definition: The volume of water retained by the material after it has been drained by gravity.
Significance: The water held by capillary forces that doesnt drain under gravity.
8. Groundwater Velocity (v)
Definition: The speed at which groundwater moves through a porous medium.
Formula:
=
v=
n
e
K
i, where
i is the hydraulic gradient and
n
e
is the effective porosity.
9. Hydraulic Gradient (i)
Definition: The slope of the water table or potentiometric surface, defined as the change in hydraulic head per unit distance.
Formula:
=
i=
L
h
, where
h is the change in head and
L is the distance over which the change occurs.
10. Recharge and Discharge Rates
Definition: The rate at which water is added (recharge) or removed (discharge) from an aquifer.
Significance: Critical for water balance and sustainability of groundwater resources.
11. Diffusivity (D)
Definition: The ratio of transmissivity to storage coefficient.
This document provides an introduction to flooding and disaster management. It defines floods as the overflowing of water onto normally dry land, usually due to excessive rain. Causes of floods include both physical/natural factors like heavy rainfall as well as human/anthropogenic factors like urbanization, deforestation, and failures of man-made structures. The document discusses key terms, hydrographs, impacts of floods, and strategies for flood management including both hard engineering approaches using structures and soft engineering working with natural processes.
This document discusses using hydrogeochemistry as a tool to manage the coastal Bou Areg aquifer in Morocco. The aquifer faces issues like overexploitation, water scarcity, and pollution from agriculture and development. The study aims to understand the aquifer's natural water quality, impacts on the adjacent lagoon, and identify pollution sources. Methods include geochemical analysis and isotopic dating. Results show high natural salinity from rock dissolution, and agricultural return flows are the main cause of additional salinization. Nitrate levels often exceed standards due to septic effluents and fertilizers. While saline intrusion is minor, polluted groundwater discharges affect the lagoon's quality. Improved monitoring
This document discusses the functions and values of rivers. It defines a river and explains that a river's characteristics are influenced by its watershed area, surficial geology, soils, land use, vegetation, and stormwater management. Urbanization can negatively impact rivers by increasing impervious surfaces and altering natural hydrologic responses. Proper stormwater management and maintaining floodplains and natural corridors are important for preserving river ecosystems and habitats. The document stresses using accurate precipitation data to properly design infrastructure like culverts that affect river flows.
This document discusses the functions and values of rivers. It defines a river and explains that rivers are dependent on their watershed characteristics like geology, soils, land use, vegetation and stormwater management. Urbanization can negatively impact rivers by increasing impervious surfaces and altering natural hydrologic patterns. To maintain natural river conditions, development must balance pre- and post-development flows through techniques like floodplain preservation, stormwater basins, and using accurate precipitation data. Overall, the document emphasizes that rivers are complex ecosystems that require consideration of their full watershed to support natural hydrologic and ecological functions.
this presentation gives a brief about what are the different types of floods depending upon area & its cause.It is further aided with mitigation or management techniques to be implemented & types of damages.
SWaRMA_IRBM_Module1_#3, Upstream-Downstream linkages and Multi-scale IRBM, Sa...ICIMOD
油
This presentation is the part of 12-day (28 January8 February 2019) training workshop on Multi-scale Integrated River Basin Management (IRBM) from the Hindu Kush Himalayan Perspective organized by the Strengthening Water Resources Management in Afghanistan (SWaRMA) Initiative of the International Centre for Integrated Mountain Development (ICIMOD), and targeted at participants from Afghanistan.
Floods are a common natural disaster in India that occur annually, causing widespread damage to lives and property. Some key points about floods and their management in India include:
- The major flood-prone states are Uttar Pradesh, Bihar, Assam, and West Bengal.
- Floods are caused by heavy rainfall, river overflow, coastal flooding, and sometimes dam/reservoir failures. They impact lives, infrastructure, agriculture, and the economy.
- Flood management involves forecasting, structural measures like dams and levees, and non-structural plans to minimize damage and warn communities. Zoning also directs development away from high risk flood areas.
This document analyzes the runoff process at the outlet of the Kolondieba watershed in Mali. Monitoring of physicochemical parameters like pH, temperature, electrical conductivity, and total dissolved solids was conducted from 2009-2011 in rainfall, surface water, groundwater, and at the outlet. The deconvolution method EMMA was used to determine the origin of runoff based on electrical conductivity and total dissolved solids diagrams. This analysis showed a bipolar origin of runoff with rapid flows from rainfall (Qr) making up 77% and delayed flows from shallow aquifers (Qd) making up 23% during the high water period of 2010. In 2011, Qr increased to 80% while Qd decreased due
This document summarizes a study on deconvoluting the flood hydrograph at the outlet of the Kolondieba watershed in Mali to understand the runoff process. Monitoring of physicochemical parameters was conducted from 2009-2011 at rainfall, surface water, and groundwater sites. Analysis using electrical conductivity and total dissolved solids as tracers showed runoff was composed of 77% rapid flow from rainfall and 23% delayed flow from shallow aquifers during 2010's wet season. In 2011, rapid flow increased 3% as shallow aquifer discharge declined 6.8% due to lower rainfall. The study found groundwater contributes little to hydrologic balance at the outlet, and surface runoff from rainfall heavily influenced by degraded land
This document provides an overview of key concepts in watershed hydrology. It defines hydrology as the science concerned with the origin, circulation, distribution and properties of water on Earth. Forest hydrology specifically deals with the effects of land management and vegetation on water quantity, quality and timing. The document emphasizes that a watershed approach to management is important because all areas within a watershed are connected by water flow. Managing activities and land use at the watershed scale can help avoid negative downstream impacts on water resources.
The document discusses different types of flooding including coastal (storm surge), river (fluvial), flash floods, and surface water floods. It provides details on the causes and impacts of each type. Coastal flooding is caused by storm surge which is when high winds and low pressure push water inland, increasing water levels and flooding. River flooding occurs when heavy rain or snowmelt causes water levels to rise over river banks. Flash floods are sudden, high velocity floods caused by intense rainfall. Surface water floods happen when drainage systems are overwhelmed by rain.
The document discusses floods in India, including definitions, causes, impacts, management strategies, and case studies. It provides an overview of flood types, forecasting methods, zoning, and benefits. Major factors that cause floods are described. Impacts include loss of life, property damage, health issues, and economic disruption. Management involves mitigation, preparedness, response, and recovery. Case studies of specific flood events in India are also presented.
The ICAR Indian Institute of Water Management was established in 1988 and aims to develop improved water management technologies through research. It conducts research through five programs: rainwater management, canal water management, groundwater management, waterlogged area management, and on-farm research and technology transfer.
The document then discusses the design of creek irrigation systems. It defines tidal creeks and explains how salinity varies in creeks over tidal cycles. It also discusses factors that influence salinity changes like urbanization. The document outlines the process for designing creek irrigation systems which includes determining design discharge, selecting a cross-sectional shape based on soil type and erosion control needs, using Manning's formula to calculate dimensions, and adding freeboard
This document provides an overview of a hydrology course, including:
1. The course covers topics like the hydrologic cycle, precipitation, evaporation, infiltration, stream flow, and statistical methods in hydrology.
2. Recommended textbooks for the course are Applied Hydrology by Chow, Maidment, and Larry, and Engineering Hydrology by Subramanya.
3. The document also lists guidelines for student behavior in class, including turning off phones, no food, bringing ID cards, and not disturbing other students.
This doctoral thesis examines the regional hydrogeological framework of the Mesozoic aquifer system in Jordan. It analyzes the complex groundwater flow systems in the Western Highlands and Central Plateau, which reflect changes in climate and geology. The aquifer systems are developed in Upper Cretaceous to Cainozoic carbonate rocks, which were modified over time by tectonic, volcanic and erosional events. Based on hydraulic conductivity contrasts, the regional carbonate aquifer system is divided into three main aquifers separated by confining units. The thesis studies the aquifer properties, recharge mechanisms and patterns, and conceptualizes regional groundwater flow through numerical modeling.
This document provides an overview of flood causes, types, effects, and management in India. It discusses various structural and non-structural flood control measures used in the country. The key causes of flooding include heavy rainfall, snowmelt, wind, tidal effects, and infrastructure failures. Floods are classified based on duration as flash floods, slow-onset floods, and rapid-onset floods. They are also classified based on location as coastal, riverine, urban and other types of floods. Flood management involves both structural measures like dams, reservoirs, flood walls and non-structural measures like flood plain zoning, flood proofing and disaster relief. India is highly vulnerable to flooding due to the monsoon climate and flooding has increased
This document summarizes a study on the impacts of coastal floodplain sedimentation on net subsidence in the Ganges-Brahmaputra-Meghna Delta. The study uses a hydrodynamic model to simulate sedimentation and erosion rates in the delta's three estuarine systems between 2000-2100. It finds that while the eastern and western regions see net uplift by 2100 due to sedimentation outpacing subsidence, the central region continues subsiding due to higher erosion rates. The sedimentation modeled partially offsets predicted sea level rise impacts in the eastern and western regions but leaves the central region more vulnerable.
Ground Water Quality Assessment using Geo Spatial Technology in Part of Lower...IRJET Journal
油
This document summarizes a study that assessed groundwater quality in the lower Vaigai river basin in Madurai District, Tamil Nadu, India using geospatial technology. Water samples were collected from 10 locations and tested for parameters like pH, nitrate, sulfate, chloride, and total dissolved solids. Maps showing the spatial distribution of water quality in 2003 and 2015 were generated. It was found that the maximum nitrate level was 4800 mg/l in 2006, and that some areas had increasingly high levels of salts and nitrates over time due to factors like fertilizer use and wastewater. The study identified some areas as potable and others as moderate or non-potable. It concluded that water quality is
This document discusses key factors for watershed planning and management. It identifies important watershed characteristics that should be considered, including: climate, geology/physiography, soils, land use/cover, hydrology, and socioeconomic conditions. Specifically, it outlines how the watershed's size, shape, slope, drainage patterns, soil types, vegetation cover, and climatic factors like rainfall amounts can impact hydrologic processes and management approaches. The document also notes that understanding the local social conditions, land use practices, and water resources is crucial for effective watershed planning.
International Journal of Engineering Research and DevelopmentIJERD Editor
油
Electrical, Electronics and Computer Engineering,
Information Engineering and Technology,
Mechanical, Industrial and Manufacturing Engineering,
Automation and Mechatronics Engineering,
Material and Chemical Engineering,
Civil and Architecture Engineering,
Biotechnology and Bio Engineering,
Environmental Engineering,
Petroleum and Mining Engineering,
Marine and Agriculture engineering,
Aerospace Engineering.
Floodplain Modelling Materials and MethodologyIDES Editor
油
A floodplain is the normally dry land area adjoining
river or stream that is inundated during flood events. The
most common reason for flooding could be overtopping of river
or stream due to heavy downfall. The floodplain carries flow
in excess of the river or stream capacity. Flood frequency and
flood water-surface elevations are the crucial components for
the evaluation of flood hazard. This paper presents the
methodology that incorporates advanced technologies for
hydrologic and hydraulic analyses that are needed to be carried
out to predict the flood water-surface elevations for any
ungaged watershed.
This document analyzes the effects of the depth of confined aquifer III on groundwater quality in the Yancheng Coastal Alluvial Plain region of China. It finds that the depth of aquifer III ranges from -118.9 to -85.45 meters. Statistical analysis shows moderate to strong correlations between the depth and certain water quality factors, including mineralization, total alkalinity, total bacterial count, and total hardness. The correlation strengths differ between areas of varying depth classifications, indicating dynamic evolution of groundwater quality over time and space.
Rate of sediment yield in the conveyance canals of kano river irrigation proj...Alexander Decker
油
This document summarizes a study that examined the rate of sedimentation in the conveyance canals of the Kano River Irrigation Project in northwestern Nigeria. Five canals were sampled to analyze sediment texture, suspended sediment concentration, canal discharge rates, and the impact of sediment accumulation. Testing found the sediment deposits mainly consisted of fine sand with some clay and silt. Suspended sediment concentration averaged 8,474 tons per year. Canal discharge rates had reduced by 47% on average, affecting irrigated land area. Factors like poor farming practices, tractor movement in canals, and lack of maintenance were found to contribute to increased sedimentation, highlighting the need for regular dissilting and cleaning of canals.
Best KNow Hydrogen Fuel Production in the World The cost in USD kwh for H2Daniel Donatelli
油
The cost in USD/kwh for H2
Daniel Donatelli
Secure Supplies Group
Index
Introduction - Page 3
The Need for Hydrogen Fueling - Page 5
Pure H2 Fueling Technology - Page 7
Blend Gas Fueling: A Transition Strategy - Page 10
Performance Metrics: H2 vs. Fossil Fuels - Page 12
Cost Analysis and Economic Viability - Page 15
Innovations Driving Leadership - Page 18
Laminar Flame Speed Adjustment
Heat Management Systems
The Donatelli Cycle
Non-Carnot Cycle Applications
Case Studies and Real-World Applications - Page 22
Conclusion: Secure Supplies Leadership in Hydrogen Fueling - Page 27
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This presentation is the part of 12-day (28 January8 February 2019) training workshop on Multi-scale Integrated River Basin Management (IRBM) from the Hindu Kush Himalayan Perspective organized by the Strengthening Water Resources Management in Afghanistan (SWaRMA) Initiative of the International Centre for Integrated Mountain Development (ICIMOD), and targeted at participants from Afghanistan.
Floods are a common natural disaster in India that occur annually, causing widespread damage to lives and property. Some key points about floods and their management in India include:
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This document provides an overview of key concepts in watershed hydrology. It defines hydrology as the science concerned with the origin, circulation, distribution and properties of water on Earth. Forest hydrology specifically deals with the effects of land management and vegetation on water quantity, quality and timing. The document emphasizes that a watershed approach to management is important because all areas within a watershed are connected by water flow. Managing activities and land use at the watershed scale can help avoid negative downstream impacts on water resources.
The document discusses different types of flooding including coastal (storm surge), river (fluvial), flash floods, and surface water floods. It provides details on the causes and impacts of each type. Coastal flooding is caused by storm surge which is when high winds and low pressure push water inland, increasing water levels and flooding. River flooding occurs when heavy rain or snowmelt causes water levels to rise over river banks. Flash floods are sudden, high velocity floods caused by intense rainfall. Surface water floods happen when drainage systems are overwhelmed by rain.
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2. Recommended textbooks for the course are Applied Hydrology by Chow, Maidment, and Larry, and Engineering Hydrology by Subramanya.
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This document provides an overview of flood causes, types, effects, and management in India. It discusses various structural and non-structural flood control measures used in the country. The key causes of flooding include heavy rainfall, snowmelt, wind, tidal effects, and infrastructure failures. Floods are classified based on duration as flash floods, slow-onset floods, and rapid-onset floods. They are also classified based on location as coastal, riverine, urban and other types of floods. Flood management involves both structural measures like dams, reservoirs, flood walls and non-structural measures like flood plain zoning, flood proofing and disaster relief. India is highly vulnerable to flooding due to the monsoon climate and flooding has increased
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flood water-surface elevations are the crucial components for
the evaluation of flood hazard. This paper presents the
methodology that incorporates advanced technologies for
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out to predict the flood water-surface elevations for any
ungaged watershed.
This document analyzes the effects of the depth of confined aquifer III on groundwater quality in the Yancheng Coastal Alluvial Plain region of China. It finds that the depth of aquifer III ranges from -118.9 to -85.45 meters. Statistical analysis shows moderate to strong correlations between the depth and certain water quality factors, including mineralization, total alkalinity, total bacterial count, and total hardness. The correlation strengths differ between areas of varying depth classifications, indicating dynamic evolution of groundwater quality over time and space.
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Household combustion devices, motor vehicles, industrial facilities and forest fires are common sources of air pollution. Pollutants of major public health concern include particulate matter, carbon monoxide, ozone, nitrogen dioxide and sulfur dioxide. Outdoor and indoor air pollution cause respiratory and other diseases and are important sources of morbidity and mortality.
WHO data show that almost all of the global population (99%) breathe air that exceeds WHO guideline limits and contains high levels of pollutants, with low- and middle-income countries suffering from the highest exposures.
Air quality is closely linked to the earths climate and ecosystems globally. Many of the drivers of air pollution (i.e. combustion of fossil fuels) are also sources of greenhouse gas emissions. Policies to reduce air pollution, therefore, offer a win-win strategy for both climate and health, lowering the burden of disease attributable to air pollution, as well as contributing to the near- and long-term mitigation of climate change.
15. Smart Cities Big Data, Civic Hackers, and the Quest for a New Utopia.pdfNgocThang9
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Antropogenic Factors of Flood in Palembang.pptx
1. Identification of Anthropogenic Factors
in Flood Events in Palembang City
Eddy Santana Putra, Anis Saggaff, Febrian Hadinata, Sarino,
Febrinasti Alia, and Raden Ayu Marlina Sylvia
PALEMBANG, 17 OKTOBER 2023
International Conference
Palembang, 17 Oktober 2023
4. BACKGROUND
Palembang City has an area of 400.61 km2, with generally flat terrain (less than 1:100) in
most areas, and is marked by the Musi River which divides the city from west to east.
Elevations starts from 4 m above sea level (MSL) in the area near the Musi River, to
around 12 MSL in the north and northwest (Sukarami to Ilir Barat districts), with the
terrain tending to be more naturally undulating and flat.
The Musi River has a number of streams, namely the Keramasan, Ogan, and Komering
rivers in the south. In the North, there are many smaller rivers that flow into the Musi
River.
The Musi River is influenced by tidal fluctuations upstream of the city so the water level
rises and falls during the day.
Even though there are embankments throughout the city, inundation still occurs
frequently, especially in swampy areas in the eastern part such as Kalidoni and
Seberang Ulu II.
There are 19 drainage catchments in Palembang City, with catchment areas varying
between 2 ha to more than 7,000 ha;
With these geographical conditions, Palembang City has many areas that are inundated
Source:
https://www.mongabay.co.id/,
Viewed on August 17, 2023
Source:
https://www.antaranews.com/,
Viewed on August 17, 2023
5. LITERATURE
Xie and Zhao (2013) stated that there is a relationship between topographic relief and flood disasters, where the
low elevation of the terrain and the small rate of terrain change increase vulnerability to flood disasters;
Palembang has a monsoon climate with distinct wet and dry seasons. The average rainfall for 2022 ranges from
97.2 mm (July) to 407.30 mm (January), with a total precipitation of 2,917.9 mm and a total of 309 rainy days
(Palembang City Central Bureau of Statistics, 2023);
Both natural and anthropogenic factors can cause flooding and inundation.
Natural factors that cause flood danger include:
Extreme Rainfall, where runoff occurs if the intensity of rain falling in a watershed exceeds the infiltration
capacity of the soil in that area;
Topography, where areas with impervious surfaces (such as concrete and asphalt) produce greater runoff.
The flat topography results in the spread of water, which causes long-duration flooding over large areas;
River tides, which influence the profile of flood water levels around the banks of the Musi River (Andayani
and Marlina, 2021).
6. LITERATURE
Linking floods to anthropogenic factors can be beneficial for policymakers and resource
managers, as it can lead to improvements in flood management and a reduction in flood
damage and risk (Rahman et. al, 2021).
Anthropogenic factors that can cause flooding include:
Changes in land cover, population growth, and road density (Rahman et. al, 2021);
Reduced water catchment areas due to swamp reclamation and reduction in green
open space (Horisky et. al, 2018);
Land subsidence due to development and massive extraction of groundwater (Hamim
et. al, 2019);
Deforestation in upstream areas;
Poor waste management (Ijaz et. al, 2021).
8. This research is quantitative descriptive research.
Field surveys are carried out by looking directly at the field and conducting interviews with
local residents to obtain data: location, causes of flooding or inundation, availability and
condition of drainage, as well as characteristics of flooding that occurs.
The sampling technique (without chance) used was purposive sampling, by selecting
residents who had experienced flooding as respondents.
The number of respondents was not targeted, because it was adjusted to the flood points
found.
The variables asked in the questionnaire include:
Inundation point/location;
Height, duration, and estimated area of inundation;
Documentation picture;
Damage to buildings or roads due to flooding; and
Causes of inundation or flooding (more than one answer is possible).
Research Methods
9. For variables that cause inundation or flooding, more than one answer may be
provided, to see whether flooding is caused by a single or multiple factors.
The location of inundation and/or flooding will be compared with a map of
potential flooding at maximum tide (hydraulic analysis), obtained from Putri and
Alia (2023) for the Seberang Ilir area, and Almirah and Alia (2023) for the
Seberang Ulu area.
If the flood point resulting from field tracking is outside the area of potential
flooding or inundation at maximum tide, there is an indication that flooding
and/or inundation is not only caused by natural factors (which can be modeled
in hydraulic modeling), but also by anthropogenic factors.
Photo documentation is used as validation that there is an anthropogenic
disturbance in drainage channels, such as channels that are not available or
discontinuous, rubbish and mud, and channels that are too small, and others;
The answer was obtained from 92 respondents who experienced floods, spread
throughout the 17 sub -district in Palembang City.
Research Methods
11. Based on the results of field surveys, tracking the location of floods and/or inundations, and interviews with people affected
by flooding, floods and/or inundation can be caused by natural factors and anthropogenic factors.
The total number of answers for the flood cause variable was 223 answers from 92 respondents, where on average each
respondent answered that there were 2 - 3 factors that caused floods, and floods were perceived not only to be caused by
one single factor but by multiple factors.
Natural factors in the form of high rainfall and overflowing rivers (due to tides and/or flood discharge) are quite dominantly
perceived as causes of flooding. High rainfall is perceived by the community as the dominant factor causing floods (=
39.91%), as well as overflowing rivers are perceived as one of the main factors causing floods (= 8.97%).
But cumulatively, anthropogenic factors are more dominantly perceived by the community as the cause of flooding and/or
inundation, namely:
Insufficient channel capacity, which can be caused by channel design errors, increased surface runoff due to land use
changes;
Solid waste/others that obstruct the flow of channels or rivers. Plastic waste will not degrade and will clog the drains for
a long time. degradable waste will decompose, some of which will become sediment/mud and reduce the channel's
drainage capacity;
Disconnected or unavailable drainage system.
RESULT OF THE FIELD SURVEYS
12. High intensity of rainfall,
39.91%
River overflowing., 8.97%
Insufficient channel
capacity, 26.01%
Solid waste/others that obstructs the
flow of channels or rivers, 13.45%
Domestic wastewater that enters
the drainage channel, 2.24%
Drainage network that is not
connected or not exist, 4.48%
Filling in swamps/wet land areas, 2.24%
The building covers/above
the drainage channel , 0.45%
Flooding from other areas,
1.35%
Overflow of retention ponds,
0.90%
Community perceptions are affected by the causes of flooding and/or inundation
This initial study found that flooding and/or inundation were perceived not only to be caused by natural
factors but also by anthropogenic factors;
Thus, flood risk studies are needed that combine flood hazard factors due to natural factors and
anthropogenic factors.
13. Source: Putri and Alia (2023) Source: Almirah and Alia (2023)
Location of floods and/or inundation in
Palembang City based on field surveys (2023)
Potential flooding area at maximum tide from hydraulic modeling
Field survey results show that there are flooding events and/or inundation
outside the predicted flood area at maximum tide
14. DOCUMENTATION
Ilir Barat Gandus SU I Kertapati Jakabaring IT II IB I
Kemuning Bukit Kecil
Some documentation of the survey
of flood/inundation locations
Plaju Kalidoni IT III Sako
Sematang Borang Sukarame Alang-alang Lebar SU II
16. Floods can be caused by natural and anthropogenic factors.
The flood area resulting from hydraulic modeling, which indicates the potential for flooding due
to natural factors, is different from the results of flood/inundation field surveys in Palembang
City.
Based on field surveys, several areas that should not have the potential for flooding, during
maximum tides, were recorded as experiencing flooding or inundation;
This flood and/or inundation can be caused by anthropogenic factors, such as insufficient
channel capacity, solid waste that obstructs the flow of channels, disconnected or unavailable
drainage systems, filling in swamps/wetland areas, and domestic wastewater that enters the
drainage channel;
Flooding and/or inundation occurred in unpredictable areas, including in the sub-district:
Sukarami, AlangAlang Lebar, Sako, Sematang Borang, and Kemuning. These four districts
experienced rapid economic growth with the emergence of new settlements;
CONCLUSION
17. Xie L and Zhao H 2013 Correlation between flood disaster and topography: A case study of Zhaoqing City Journal of Natural Disasters 22(6):240-245.
Palembang City Central Bureau of Statistics 2023 Palembang in Figures 2022.
Andayani, R and Marlina A 2021 Pengaruh Pasang Surut Terhadap Profil Muka Air Banjir Bantaran Sungai Musi Kota Palembang. Cantilever: Jurnal
Penelitian dan Kajian Bidang Teknik SIpil, 10(2), 119-126.
Rahman M Ningsheng C Mahmud G I Islam M M Pourghasemi H R Ahmad H Habumugisha J M Washakh R M AAlam M Liu E Han Z Ni H Shufeng T and
Dewan A 2021 Flooding and its relationship with land cover change, population growth, and road density. Geoscience Frontiers, 129(6), 1-20.
Horisky C Rahmadi & Harahap T 2018 Pengaruh Perubahan Pola Pengunaan Lahan Terhadap Banjir di DAS Buah Kota Palembang. Prosiding Seminar
Nasional Hari Air Dunia 2018, Palembang 20 Maret 2018.
Hamim S A Usman F and Shalihat A K 2019 Determination of Land Subsidence Caused by Land-Use Changing in Palembang City using Remote Sensing
Data. Advances in Engineering Research, 187, 101-106.
Ijaz S Miandad M Mehdi S S Anwar M M and Rahman G 2021 Solid waste management as a response to urban flood risk in Gujrat city, Pakistan
GEOGRAFIA: Malaysian Journal of Society and Space, 17(1), 1-13.
Putri D J and Alia F 2023 Pemodelan Banjir Wilayah Seberang Ilir Kota Palembang Dengan Pemanfaatan Model Hidrolika dan Sistem Informasi Geografis
Undergraduate thesis Sriwijaya University.
Almirah S R and Alia F 2023 Pemetaan Banjir Wilayah Seberang Ulu Kota Palembang Menggunakan HEC-RAS dan SIG Undergraduate thesis Sriwijaya
University.
REFERENCES