Watershed approach for studying soil preferential flow: A case study

Appoothy Angayarkanni, A. Dhimate, Sannaila, Arun Kumar
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Abstract

Preferential flow (PF) is a generic term used for water flow paths through biopores, fractures and macro pores. Many studies and models were already established to describe the PF. In semi-arid regions, the connecting aboveground and below ground processes to investigate how soil redistribute rainfall and nutrient and their impact on subsurface flow, is a fairly overlooked phenomenon. In this era of fast changing climate, erratic rainfall and rain water management, soil constitution plays an important role. In semi-arid regions, watershed is the basic hydrologic unit which gives study of the soil preferential flow a holistic look. In this regard, a study was conducted in Hayath nagar micro-watershed, Hyderabad, during 2020-2021.results revealed that the micro-watershed mainly comprises of heterogeneous matrix flow and fingering at surface while at sub surface macropore flow with low and mixed interaction prevails. This suggested that subsurface soils were mainly responsible for spatial redistribution of flows and generating lateral flow than vertical flow. Thus, the watershed under study requires better management practice to harvest water and check runoff at the time of high intensity rainfall. The results and the methodology of the present study have relevance in studying the preferential flow of diverse watersheds.
研究土壤优先流的流域方法:一个案例研究
优先流(PF)是一个通称,用于水通过生物孔隙、裂缝和宏观孔隙的流动路径。已经建立了许多研究和模型来描述PF。在半干旱地区,连接地上和地下的过程来研究土壤如何重新分配降雨和养分及其对地下流的影响,是一个相当被忽视的现象。在这个气候快速变化、降雨不稳定和雨水管理的时代,土壤构成起着重要的作用。在半干旱区,流域作为基本的水文单元,使土壤优先流研究具有整体性。在这方面,2020-2021年期间在海得拉巴的Hayath nagar小流域进行了一项研究。结果表明,微流域主要以地表非均质基质流和指动流为主,而亚地表大孔流则以低相互作用和混合相互作用为主。这表明地下土壤主要负责流动的空间再分配和产生横向流动,而不是垂直流动。因此,研究中的流域需要更好的管理实践,以便在高强度降雨时收集水并控制径流。本研究的结果和方法对研究不同流域的优先流具有重要意义。
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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