Potential of Shallow Groundwater for Household Level Irrigation Practices in Tahtay Koraro Woreda, Tigray, Northern Ethiopia

IF 0.3 Q4 MULTIDISCIPLINARY SCIENCES
Ermias Hagos, Amare Girmay, Tesfamichael Gebreyohannes
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引用次数: 1

Abstract

This paper deals with the results of a pilot study conducted to estimate the shallow groundwater resource potential and irrigation capacity at the household level in Tahtay Koraro Woreda, northwestern zone of Tigray, Ethiopia. The potential evapotranspiration and actual evapotranspiration of the study area are estimated to be 1484 mm/year and 814 mm/year respectively. The runoff is approximately calculated to be 280 mm/year and the annual groundwater recharge is estimated to be 29 mm/year. The total annual groundwater abstraction for human, livestock, and irrigation is estimated to be 25 mm/year. It should be noted that the groundwater recharge rate is expected to remain constant while the total annual groundwater discharge is expected to increase from year to year. This relation when projected over a long period may result in a negative groundwater budget which can result in depletion of groundwater (lowering of groundwater levels), reduced baseflow to streams, and deterioration of water quality.  The computed values for hydraulic conductivity of the aquifers range from 1.63 m/day to 7.27 m/day with an average value of 4.9 m/day and transmissivity from 48.9 m2/day to 218.1 m2/day with an average value of 147.14 m2/day. The aquifers in the highly weathered basalt and highly weathered siltstone – sandstone intercalation have transmissivity values ranging from 99 m2/day to 218.1 m2/day with an average value of 157 m2/day and are grouped into the moderate potentiality aquifers category. The aquifers in the slightly weathered and fractured metavolcanics grouped under low potentiality based on the lower transmissivity values (<50 m2/day). The study area has low to moderate groundwater potentiality, hence, large-scale groundwater pumping is not possible. Therefore, the current activity of using hand dug wells for household-level irrigation is the best way of using groundwater for irrigation and other uses as well. Increasing the depth of the existing hand dug wells that are constructed in highly weathered basalt and highly weathered siltstone – sandstone intercalation can also enhance the yield of the hand dug wells. It is recommended to use water-saving irrigation technologies rather than increasing the number of wells. This will also help in increasing the irrigation area. Groundwater recharge enhancement structures such as trenches, percolation ponds, and check dams be constructed in scientifically selected localities to further enhance the groundwater potential.
埃塞俄比亚北部提格雷Tahtay Koraro Woreda浅层地下水在家庭水平灌溉实践中的潜力
本文介绍了一项试点研究的结果,该研究旨在评估埃塞俄比亚提格雷西北部Tahtay Koraro Woreda的浅层地下水资源潜力和家庭灌溉能力。研究区域的潜在蒸散量和实际蒸散量估计分别为1484 mm/年和814 mm/年。径流约为280毫米/年,地下水年补给量估计为29毫米/年。据估计,人类、牲畜和灌溉的年地下水总抽取量为25毫米/年。应注意的是,地下水补给率预计将保持不变,而地下水年排放总量预计将逐年增加。如果长期预测这种关系,可能会导致地下水预算为负,从而导致地下水枯竭(地下水位下降)、流向溪流的基流减少和水质恶化。含水层水力传导率的计算值范围为1.63米/天至7.27米/天,平均值为4.9米/天;透射率范围为48.9米/天到218.1米/天(平均值为147.14米/天)。强风化玄武岩和强风化粉砂岩-砂岩夹层中的含水层具有99 m2/天至218.1 m2/天的透射率,平均值为157 m2/天,属于中等潜力含水层类别。根据较低的透射率值(<50m2/天),轻度风化和断裂变质火山岩中的含水层属于低潜力组。研究区域地下水潜力低至中等,因此不可能大规模抽取地下水。因此,目前使用手井进行家庭灌溉的活动是将地下水用于灌溉和其他用途的最佳方式。增加在强风化玄武岩和强风化粉砂岩-砂岩夹层中建造的现有手井的深度也可以提高手井的产量。建议采用节水灌溉技术,而不是增加水井数量。这也将有助于增加灌溉面积。在科学选择的地点建造沟渠、渗水池和淤塞坝等地下水补给增强结构,以进一步提高地下水潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Momona Ethiopian Journal of Science
Momona Ethiopian Journal of Science MULTIDISCIPLINARY SCIENCES-
自引率
0.00%
发文量
13
审稿时长
12 weeks
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