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Estimation of Probable Groundwater Recharge Under Semi-arid Agro Climatic Conditions of Raichur Region

机译:干旱地区半干旱农业气候条件下地下水补给量的估算

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Explosion in population, has led to increase in demand of various natural resources i.e. water, especially for agricultural purposes. Over exploitation of water affects the ecology of the region and affects the sustainability. Thus, a judicious use ofwater in semi-arid and rural areas is must. Even though India has good average annual precipitation, but its poor distribution in space and time has lead to the scarcity of groundwater. Thus an attempt has been made to study the probable groundwater recharge for agricultural utilization in the Patapur micro-watershed, which is located in semi-arid region ofRaichur district. For the investigation rainfall, runoff and peak discharge of the micro-watershed were estimated and it was found to be about 211 mm, 85, 6, 95.00 (cum) and 793.07 (cum/min) respectively. Total crop evapotranspiration (ETc in mm) values at different stages of crop development were also estimated, it was found about 2, 6, 06.77 mm. Available moisture holding capacity of clay loam was35.28 cm and sandy clay loam was 19 cm. Estimated recharge quantity in area of clay loam soils was found to be about 90.43 mm or 265601.94 m~3- in area of sandy clay loam soils it was found to be about 100.41mm or 248695.5 m~3.The total estimated recharge quantity in the micro-watershed was about 514297.4 m~3or 94.99 mm. From the investigation it was concluded that the groundwater availability was good and even though it was suggested to construct the groundwater recharge structures (check dams, nala bunding, form ponds etc.) for storage of this precious resource.
机译:人口激增导致对各种自然资源(即水)的需求增加,特别是用于农业目的。过度开采水会影响该地区的生态并影响可持续性。因此,必须明智地在半干旱和农村地区用水。尽管印度的年平均降水量很好,但其时空分布不均导致地下水短缺。因此,已经尝试研究位于Raichur区半干旱地区的Patapur微流域中可能用于农业利用的地下水补给。为了进行调查,估计了小流域的径流和峰值流量,分别约为211 mm,85、6、95.00(cum / min)和793.07(cum / min)。还估计了作物生长不同阶段的总作物蒸散量(ETc,单位为mm),大约为2、6、06.77 mm。粘土壤土的有效持水量为35.28 cm,沙质壤土为19 cm。砂质壤土地区的估算补给量约为90.43 mm或265601.94 m〜3-,而砂质壤土地区的估算补给量约为100.41mm或248695.5 m〜3。微流域约为514297.4 m〜3或94.99 mm。从调查中得出的结论是,尽管有人建议建造地下水补给结构(检查水坝,纳拉堤坝,蓄水池等)以存储这种宝贵的资源,但地下水的可利用性很好。

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