Estimation of Spatial Groundwater Recharge Using WetSpass Model for East Wasit Province, Iraq

2021 ◽  
Vol 9 (2) ◽  
pp. 20-33
Author(s):  
Hassan Al-Badry ◽  
Mohammed S. Shamkhi
Keyword(s):  
Groundwater Recharge ◽  
Meteorological Data ◽  
Groundwater Resources ◽  
Water Source ◽  
Water Shortage ◽  
High Elevation ◽  
Annual Rainfall ◽  
Water Balance Components ◽  
Wetspass Model ◽  
Alternative Water

AbstractGroundwater is an important water source, especially in arid and semi-arid areas. Recharge is critical to managing and analyzing groundwater resources despite estimation difficulty due to temporal and spatial change. The study aim is to estimate annual groundwater recharge for the eastern Wasit Province part, Iraq. Where suffers from a surface water shortage due to the region's high elevation above Tigris River water elevation by about 60 m, it is necessary to search for alternative water sources, such as groundwater use. The spatially distributed WetSpass model was used to estimate the annual recharge. The inputs for the model were prepared using the ARC-GIS program, which includes the topography and slope grid, soil texture grid, land use, groundwater level grid, and meteorological data grids for the study area for the period (2014-2019). The result shows that the annual recharge calculated using the WetSpass model (2014-2019) varied of 0 to 65.176 mm/year at an average of 27.117 mm/year, about 10.8%, while the rate of the surface runoff was 5.2% and Evapotranspiration formed 83.33% of the annual rainfall rate of 251.192 mm. The simulation results reveal that the WetSpass model simulates the components of the hydrological water budget correctly. For managing and planning available water resources, a best grasp of the simulation of long-range average geographical distribution around the water balance components is beneficial.

scholarly journals Estimation of Spatial Groundwater Recharge Using WetSpass Model For east Wasit province ,Iraq

2021 ◽  
Vol 9 (2) ◽  
Author(s):  
Hassan Jameel AL-Badry ◽  
Mohammed S. Shamkhi
Keyword(s):  
Groundwater Recharge ◽  
Groundwater Resources ◽  
Water Source ◽  
Water Shortage ◽  
High Elevation ◽  
Oil Extraction ◽  
Tigris River ◽  
Wetspass Model ◽  
Alternative Water

Groundwater is an important water source, especially in arid and semi-arid areas. Recharge is critical to managing and analyzing groundwater resources despite estimation difficulty due to temporal and spatial change. the study aim is to estimate annual groundwater recharge for the eastern Wasit Province, Iraq. Where suffers from a surface water shortage due to the region's high elevation above Tigris River water elevation by about 60 m. It is necessary to search for alternative water sources, such as groundwater use, especially with the increased demand for water in light of the growth of oil extraction in the region, where oil extraction requires a quantity of water three times the amount of oil extracted. The result shows the annual recharge calculated using the WetSpass model for the period (2014-2019) ranged from 0 to 65.176  mm/year at a rate of 27.117 mm/year and a standard deviation of 21.498. The simulation results reveal that the WetSpass model simulates the components of the hydrological water budget correctly. For managing and planning available water resources, a better grasp of the simulation of long-term average geographical distribution around the components of the water balance is beneficial.

Estimation of Spatial and Temporal Groundwater Balance Components in Khadir Canal Sub-Division, Chaj Doab, Pakistan

Hydrology ◽  
2021 ◽  
Vol 8 (4) ◽  
pp. 178
Author(s):  
Muhammad Aslam ◽  
Ali Salem ◽  
Vijay P. Singh ◽  
Muhammad Arshad
Keyword(s):  
Land Use ◽  
Water Balance ◽  
Groundwater Recharge ◽  
Groundwater Resources ◽  
Balance Model ◽  
Annual Rainfall ◽  
Water Balance Components ◽  
Aquifer Management ◽  
Groundwater Balance ◽  
Semi Arid

Evaluation of the spatial and temporal distribution of water balance components is required for efficient and sustainable management of groundwater resources, especially in semi-arid and data-poor areas. The Khadir canal sub-division, Chaj Doab, Pakistan, is a semi-arid area which has shallow aquifers which are being pumped by a plethora of wells with no effective monitoring. This study employed a monthly water balance model (water and energy transfer among soil, plants, and atmosphere)—WetSpass-M—to determine the groundwater balance components on annual, seasonal, and monthly time scales for a period of the last 20 years (2000–2019) in the Khadir canal sub-division. The spatial distribution of water balance components depends on soil texture, land use, groundwater level, slope, and meteorological conditions. Inputs for the model included data on topography, slope, soil, groundwater depth, slope, land use, and meteorological data (e.g., precipitation, air temperature, potential evapotranspiration, and wind speed) which were prepared using ArcGIS. The long-term average annual rainfall (455.7 mm) is distributed as 231 mm (51%) evapotranspiration, 109.1 mm (24%) surface runoff, and 115.6 mm (25%) groundwater recharge. About 51% of groundwater recharge occurs in summer, 18% in autumn, 14% in winter, and 17% in spring. Results showed that the WetSpass-M model properly simulated the water balance components of the Khadir canal sub-division. The WetSpass-M model’s findings can be used to develop a regional groundwater model for simulation of different aquifer management scenarios in the Khadir area, Pakistan.

scholarly journals Investigation of the Current Situation and Prospects for the Development of Rainwater Harvesting as a Tool to Confront Water Scarcity Worldwide

Water ◽  
2019 ◽  
Vol 11 (10) ◽  
pp. 2168 ◽  
Author(s):  
Stavros Yannopoulos ◽  
Ioanna Giannopoulou ◽  
Mina Kaiafa-Saropoulou
Keyword(s):  
Water Scarcity ◽  
Rainwater Harvesting ◽  
Groundwater Resources ◽  
Water Source ◽  
Water Shortage ◽  
Global Scale ◽  
Current Situation ◽  
Frequency Peak ◽  
Alternative Water ◽  
Social Causes

Nowadays, available water resources face severe pressures due to demographic, economic, social causes, environmental degradation, climate change, and technological changes on a global scale. It is well known that rainwater harvesting, a simple and old method, has the potential to supplement surface and groundwater resources in areas that have inadequate water supply. In recent decades, many countries have supported the updated implementation of such a practice to confront the water demand increase and to reduce the frequency, peak, and volume of urban runoff. These considerations motivate interest in examining the current situation and the prospect of further development of this method worldwide. The present paper aims at the investigation of the current situation of rainwater harvesting (RWH) as an alternative water source to confront water scarcity in various countries around the world. In particular, the paper presents the following: (a) the causes of water shortage; (b) a concise historical overview of the temporal development of the RWH method; (c) the evolution of the concept of RWH; (d) the efforts to renew interest in RWH; and (e) incentives and perspectives for the spreading of the RWH method in various countries worldwide.

scholarly journals Climate Changes Impacts on Groundwater Recharge in the UAE

10.29007/kdpc ◽  
2018 ◽  
Author(s):  
Mohamed Mostafa Mohamed
Keyword(s):  
Groundwater Recharge ◽  
Groundwater Resources ◽  
Climate Change Impacts ◽  
Water Source ◽  
Eastern Region ◽  
Continuous Increase ◽  
Groundwater Availability ◽  
Groundwater Aquifer ◽  
Abu Dhabi Emirate ◽  
Desalination Plants

Despite the continuous increase in water supply from desalination plants in the UAE, groundwater remains the major source of fresh water satisfying domestic and agricultural demands. Additionally, groundwater has always been considered as a strategic water source towards groundwater security in the country. Quantification of groundwater recharge is a prerequisite for efficient and sustainable groundwater resources management in arid regions. Therefore, groundwater recharge from the ephemeral Wadi beds and subsurface flow from mountainous valley beds play an important role in water management. Although, both surface and groundwater resources in UAE are scarce; the anticipated climate change impacts could make these resources even scarcer. As such, the main aim of this paper is to assess the potential impacts of future climate variability and change on groundwater recharge in the eastern region of UAE. This paper will explore rainfall characteristics in the region, their projections and their impacts on Wadi hydrology and groundwater recharge processes. Another objective of the study is to identify groundwater recharge regions to the shallow unconfined groundwater aquifer in the northeastern part of Abu-Dhabi Emirate. Outcomes of this study will help to accurately estimate current and future sustainable extraction rates, assess groundwater availability, and identify pathways and velocity of groundwater flow as crucial information for determining the best locations for artificial recharge.

scholarly journals Evaluation of groundwater recharge by rice and crop rotation fields in Kumamoto, Japan

2019 ◽  
Vol 11 (4) ◽  
pp. 1042-1049
Author(s):  
Takehide Hama ◽  
Toshio Fujimi ◽  
Takeo Shima ◽  
Kei Ishida ◽  
Yasunori Kawagoshi ◽  
...  
Keyword(s):  
Groundwater Recharge ◽  
Paddy Field ◽  
Local Governments ◽  
Water Distribution ◽  
Groundwater Resources ◽  
Water Shortage ◽  
Distribution Model ◽  
Drought Risk ◽  
Large Contribution ◽  
Environmental Measures

Abstract In Kumamoto, Japan, about one million people depend for all their water on groundwater resources. Paddy fields and rice farming in the middle river watershed area make a large contribution to the groundwater recharge. In our research, an environmental measure (artificial flooding for groundwater recharge) conducted by local governments is evaluated. Hydrological measurement was conducted in a paddy plot in the area. A simple model of water distribution was developed on the basis of the field measurement. Then, drought risk in the paddy-field district was estimated using the model and GIS data. The results reveal that the fields with a high percolation rate of more than 30 mm/d result in inefficient use of irrigation water although they have large potential for groundwater recharge. In addition, the water distribution model suggests that environmental measures can increase the risk of water shortage in the paddy-field district due to the farmers' careless use of water.

scholarly journals Water Balance Estimation Using Integrated GIS-Based WetSpass Model in the Birki Watershed, Eastern Tigray, Northern Ethiopia

2019 ◽  
pp. 1-17
Author(s):  
Esayas Meresa ◽  
Abbadi Girmay ◽  
Amare Gebremedhin
Keyword(s):  
Water Balance ◽  
Groundwater Recharge ◽  
Surface Runoff ◽  
Winter Season ◽  
Secondary Data ◽  
Mean Value ◽  
Mean Annual Precipitation ◽  
Northern Ethiopia ◽  
Water Balance Components ◽  
Wetspass Model

This study aims to estimate long-term average annual and seasonal water balance components for Birki watershed using WetSpass model with the integrated geospatial modeling approach with ten years’ hydro-meteorological and biophysical data of the watershed. Both primary and secondary data were collected using both field survey and disk-based data collection methods. The WetSpass model was used for data analysis purposes. The finding showed that in the summer season the annual groundwater recharge is 24.1 mm year-1 (96.5%), winter season mean groundwater recharge is 0.8 mm year-1 (3.5%) and yearly mean groundwater recharge is 24.9 mm year-1, Surface runoff yearly mean value is 40.6 mm year-1, Soil evaporation yearly mean value is 10.8 mm year-1, Evapotranspiration yearly mean value is 60.8 mm year-1, Intersection loss yearly mean value is 17 mm year-1, and Transpiration loss yearly value is 6.8 mm year-1 in the entire watershed. The mean annual precipitation, which is 573 mm, is contributed to 7.4%, 7.1% and 85.5% recharge to the groundwater, to surface runoff, and evapotranspiration, respectively. Annually 1.1205 million m3 water recharges into the groundwater table as recharge from the precipitation on the entire watershed. The contribution of this study could be used as baseline information for regional water resource experts, policy makers and researchers for further investigation. It can also be concluded that integrated WetSpass and GIS-based models are good indicators for estimating and understanding of water balance components in a given watershed to implement an integrated watershed management plan for sustainable utilization and sustainable development.

scholarly journals Integrated Hydrological Analysis of Little Akaki Watershed Using SWAT-MODFLOW, Ethiopia

2021 ◽  
Vol 11 (13) ◽  
pp. 6011
Author(s):  
Mesfin Benti Tolera ◽  
Il-Moon Chung
Keyword(s):  
Groundwater Recharge ◽  
Groundwater Resources ◽  
Swat Model ◽  
Annual Rainfall ◽  
Integrated Analysis ◽  
Human Consumption ◽  
Pumping Rate ◽  
Groundwater Head ◽  
Main River ◽  
Examination Result

In Ethiopia, groundwater is the main source of freshwater to support human consumption and socio-economic development. Little Akaki watershed is located in Upper Awash basin, known for its high annual rainfall and considered as the potential groundwater recharge zone. On the contrary, urbanization and industrial expansion are increasing at an alarming rate in the area. This became a concern threatening the groundwater resources’ sustainability. To address these challenges, integrated analysis of groundwater recharge and groundwater numerical simulations were made. For groundwater recharge estimation, SWAT model was used. The result indicated that recharge in the watershed mostly occurs from July to October with maximum values in August. On average, the estimated annual catchment recharge was 179 mm. For the numerical simulation and prediction of the groundwater flow system, MODFLOW 2005 was used. The model simulations indicated that the groundwater head converges towards the main river and, finally, to the outlet of the watershed. The study indicated areas of interactions between the river and groundwater. The scenario examination result reveals increasing the present pumping rate by over fifty percent (by 50%, 100%, and 200%) will surely cause visible groundwater head decline near the outlet of the watershed, and substantial river baseflow reduction. The recharge reduction scenario also indicates the huge risk of groundwater sustainability in the area.

scholarly journals An assessment of potential groundwater recharge zones in Bulgaria

2019 ◽  
Vol 48 (1) ◽  
pp. 43-61
Author(s):  
Tanya Vasileva
Keyword(s):  
Data Base ◽  
Groundwater Recharge ◽  
Groundwater Resources ◽  
Drainage Density ◽  
Annual Rainfall ◽  
Thematic Maps ◽  
Thematic Layers ◽  
Potential Groundwater ◽  
Density Map ◽  
Gis Platform

Groundwater resources on the territory of Bulgaria are unevenly distributed in both spatial and temporal aspects. The effective usage of these valuable assets is of paramount importance, since any over-exploitation would eventually lead to their depletion. Remote sensing data and satellite images have increasingly been used in groundwater exploration and management. An integrated approach was applied in the present study in order to delineate potential groundwater recharge zones on the territory of Bulgaria. Data from various sources were used to prepare different thematic layers. These layers were then transformed into raster data of 1×1 km. Lineament and drainage density maps of the research area were made with the help of GIS technology. In addition, a map was made for the annual total precipitation for the period from 1931 to 1985. DEM (Digital Elevation Model) data on a global scale at 90 m horizontal resolution were used for the slope analysis. A groundwater potential map was produced, which integrates several thematic maps, such as annual rainfall, geology, lineament density, land use, slope, soils, and drainage density. The thematic maps were then converted into a raster graphic format in order to be easily integrated into a GIS platform. The raster maps of these factors were then allocated a fixed score and weight-computed. The weights of those factors contributing to the groundwater recharge were derived by using the following components: geological map, lineament-length density map, land cover data base, soil data base, drainage-length density map, and slope gradient map. Subjective weights were assigned to the respective thematic layers, and they were overlaid in a GIS platform for the identification of potential groundwater recharge zones within the study area. These potential recharge zones were then categorized as being very good, good, moderate, poor, and very poor.

scholarly journals Groundwater Recharge Potential Using GIS around the Land Development Facilities of Chulalongkorn University at Kaeng Khoi District, Saraburi Province, Thailand

2015 ◽  
pp. 75-83 ◽  
Author(s):  
Srilert Chotpantarat ◽  
Jaturon Konkul ◽  
Satika Boonkaewwan ◽  
Thanop Thitimakorn
Keyword(s):  
Groundwater Recharge ◽  
Crop Production ◽  
Groundwater Resources ◽  
Central Area ◽  
Land Development ◽  
Water Shortage ◽  
Drainage Density ◽  
Recharge Potential ◽  
Ground Water Recharge ◽  
Water Recharge

KaengKhoi District (SaraburiProvince, Thailand) suffers from a surface water shortage due to increasing demand from domestic use and crop production, particularly in the drought season. Groundwater resources are an additional source of freshwater in this area, especially for agricul-tural purposes, but to be sustainable its usage should not exceed long-term groundwater recharge. Evaluation of the groundwater recharge potential is therefore essential to determine the sustain-able use level for groundwater resources. This study aimed to determine the groundwater re-charge potential using the geographic information system (GIS) around the Land Development Facilities of Chulalongkorn University at KaengKhoi District, Thailand. The hydrologic and geo-logic features affecting groundwater recharge potential into the groundwater system are the linea-ments, drainage density, lithology and land cover/land use. The weighting of these factors were derived from integration of the interrelationship of the major and minor effects of each contri-buting factor. Then GIS overlay was used to determine the influence of the hydrologic and geo-logic effects on total groundwater recharge potentiality, classified into five categories: very high, high, moderate, low and very low. The highest recharge potentialzone was located in the down-stream areas. The map generated revealed that about 50% of the study area had a medium ground-water recharge potential, mainly located in the eastern upstream part and the central area.

scholarly journals A retrospective analysis of the climate change impact on the groundwater resources

2017 ◽  
pp. 42-50
Author(s):  
S. O. Grinevskiy ◽  
S. P. Pozdniakov
Keyword(s):  
Water Balance ◽  
Groundwater Recharge ◽  
Climate Changes ◽  
Meteorological Data ◽  
Groundwater Resources ◽  
Basin Modeling ◽  
Climate Trends ◽  
Climate Conditions ◽  
Change Impact ◽  
Annual Water

Water balance and groundwater recharge simulations based on meteorological data with climate trends were made for the South-western part of Moscow artesian basin. Modeling results comparison of mean annual water balance and recharge values for previous (1965-1988) and present (1989-2012) periods allow to estimate their changes due to transient climate conditions. Assessment of groundwater resources climate changes was made on the basis of mean annual groundwater recharge maps for the investigated region for previous and present time periods, which showed their increase of 9% (720 thousands m3/d).

Sign in / Sign up

Export Citation Format

Share Document