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Hydro-geomorphological Analysis of a Water Logged area of South Tripura District using RS and GIS Technology

机译:基于RS和GIS技术的南Tripura区涝区水文地貌分析。

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The main objective of the study was two-fold. First, to map the natural drainage course in the wetland and its catchments area and to prepare geo-morphological and ground water prospective map to explore and utilize the subsurface water potential for irrigation during Rabi season using RS and GIS Technology. Second, to compare the results of RS and GIS data with ground truth to explore the possible causes of water logging. The total watershed area contributing water to the wetland system is about 265001 ha. The core waterlogged area of the wetland ecosystem having an area of 1750 ha (31.46 %) is covering five revenue villages. Hydro-geomorphologic maps have been prepared depicting the important geomorphic units, landforms and underlying geology. Geomorphological and geological (lithology and structural geological) interpretations (visual) were made on LISS III as well as LISS IV imagery on 1:25,000 scale. These maps were verified with limited field checks. Geomorphologically the area is young and immature and landforms are mainly of erosional and depositional origin. Average depth to water level during pre-monsoon is 2.50m bgl and during post-monsoon season is 1.5m bgl. Because of alternate sandstone and shale layers of Dupitila and Tipam Sandstone formation, ground water prospect in this region is very good to moderate but in few places it is excellent. Presence of shale layer in near surface condition created water logging in some places especially where proper drainage is absent. It is found that most of the study area is good to very good in ground water prospect. So ground water can be used extensively for various purposes taking required measures for timely recharge of the aquifers.
机译:该研究的主要目标是双重的。首先,绘制湿地及其集水区的自然排水路线图,并制作地貌和地下水前瞻图,以利用RS和GIS技术探索和利用拉比季灌溉下的地下水潜力。其次,将RS和GIS数据的结果与地面真实情况进行比较,以探讨可能引起涝灾的原因。为湿地系统贡献水的总流域面积约为265001公顷。湿地生态系统的内涝核心区域面积为1750公顷(31.46%),覆盖了五个收入村庄。已经绘制了水文-地貌图,描绘了重要的地貌单位,地貌和潜在的地质情况。在LISS III和LISS IV影像上以1:25,000的比例进行了地貌和地质(岩性和结构地质)解释(可视化)。这些地图已通过有限的现场检查得到了验证。从地貌上看,该地区年轻且不成熟,地貌主要来自侵蚀和沉积。季风前的平均水位深度为2.50m bgl,季风后的季节为1.5m bgl。由于Dupitila和Tipam砂岩形成了交替的砂岩和页岩层,该地区的地下水前景非常好至中等,但在少数地方它是极好的。页岩层在近地表条件下的存在在某些地方特别是在缺乏适当排水的地方造成了水淹。研究发现,大多数研究区域在地下水前景方面都非常好。因此,采取必要的措施及时为含水层补水,可将地下水广泛用于各种目的。

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