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首页> 外文期刊>Arabian journal of geosciences >Evaluating factors responsible for contrasting signature of wasteland development in northern and southern Ganga Plains (Bihar State, India) with focus on waterlogging
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Evaluating factors responsible for contrasting signature of wasteland development in northern and southern Ganga Plains (Bihar State, India) with focus on waterlogging

机译:评价因素使冈加平原北部和南部(印度比哈尔邦)的荒地开发标志形成对比,重点是内涝

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The present study provides assessment of wasteland development in Bihar State based on satellite data. Wasteland covers 6.90 % (6,501 km~2) of the state area and exhibits dominance of waterlogged areas in North Bihar (25.28 %) and scrubland (26.61 %) in South Bihar. The waterlogged areas in the state are dominantly associated with northern Bihar plains (94 %) with minor development (6 %) in southern Bihar plains. Such unequal distribution of waterlogged land areas in northern and southern Bihar plains is largely governed by high cumulative discharge generated in the large catchment area in Himalayan mountain ranges in the upland areas of northern Bihar plains in contrast to low cumulative discharge generated within small catchments in the Chota Nagpur Plateau in the southern Bihar plains. It is evaluated that the relief and groundwater level define the primary controlling factors, whereas rainfall, watershed area, and upland/plain ratio exert secondary control. Lower relief areas with high rainfall exhibit high soil moisture thereby inducing conditions of waterlogging. The study signifies the potential of satellite image-based evaluation of waterlogging through the use of Digital Elevation Model, Tropical Rainfall MeasuringMission-based rainfall measurement, and temporal waterlogging assessment together with other terrain parameters for conceptual understanding of waterlogging in northern Bihar plains.
机译:本研究根据卫星数据评估了比哈尔邦的荒地。荒原占州面积的6.90%(6,501 km〜2),在北比哈尔邦(25.28%)和南比哈尔邦(South Bihar)的灌丛地区(26.61%)中表现出突出的涝灾地区优势。该州的涝灾地区主要与比哈尔邦北部平原(94%)相关,而比哈尔邦南部平原则略有发展(6%)。比哈尔邦北部和南部平原的这种涝渍地分布不均,主要是由于比哈尔邦北部平原高地喜马拉雅山脉大集水区产生的累积流量高,而比哈尔邦小集水区产生的累积流量低。比哈尔邦平原南部的Chota那格浦尔高原。据评估,救济和地下水位是主要的控制因素,而降雨,流域面积和高地平原比例则是次要控制因素。降雨多的低洼地带表现出高土壤湿度,从而引发了涝灾的条件。这项研究表明,通过使用数字高程模型,基于热带降雨的测量,基于任务的降雨测量,以及临时的涝灾评估以及其他地形参数,可以对基于卫星图像的涝灾评估进行概念性理解,从而对比哈尔邦北部平原的涝灾进行概念性理解。

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