地表特征和降雨对入渗速率的影响——以加里干达基河流域为例

Janardan Joshi
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引用次数: 0

摘要

研究入渗特征对有效的流域管理至关重要,因为它有助于确定作物的水分可用性、灌溉需求、地下水补给和地表径流。本研究旨在利用水文模拟系统(HEC-HMS)确定尼泊尔Kaligandaki河流域的入渗速率与地表特征以及降雨速率之间的关系。HEC-HMS是一种基于物理的半分布式模型,它使用流域土壤和土地利用的天气和空间信息来导出模型的输入。建立了Kaligandaki河流域的水文降雨径流模型,该流域的出水口位于水文和气象部Kotgau的420水文站。然后在Kaligandaki河Angsing的DHM 420站验证了该模型。对模型生成的子流域入渗率和现有土地利用方式进行了分析,发现在主要土地利用类型中,以森林为主要土地利用方式的子流域入渗率较高。反之,以荒无区、雪/冰川和草地土地覆盖类型为主的子流域入渗速率较低。平均降雨强度呈指数增长,入渗率呈线性增长,降雨率与入渗率呈正相关。入渗速率与NRCS的水文土壤类群类型呈正相关。此外,研究表明地表覆盖对入渗速率的影响大于土壤类型。而流域坡度对入渗速率没有显著影响,这可能是由于多种地形特征的排除。了解降雨强度和地表特征对入渗的影响,可以通过地表状况评估提高入渗率,从而采取主动措施缓解滑坡等问题,减少洪水和土壤侵蚀。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Surface Characteristics and Rainfall in Infiltration Rate: A Case Study of Kaligandaki River Basin
Study of infiltration characteristics is crucial for effective watershed management, as it helps determine the water availability for crops, the need of irrigation, groundwater recharge, and surface runoff. This study is aimed at identifying the relation between infiltration rate and surface characteristics as well as rainfall rate in the Kaligandaki River basin of Nepal using Hydrologic Modelling System (HEC-HMS). HEC-HMS is a physically based, semi-distributed model that uses the weather and spatial information of soil and landuse of the basin for deriving the inputs for the model. A hydrological rainfall-runoff model is developed for the Kaligandaki River basin, with outlet at hydrological station 420, Kotgau, of Department of Hydrology and Meteorology (DHM). The model was then validated at DHM station 420, Angsing, of Kaligandaki River. Model generated subbasin wise infiltration rates and existing landuse were analysed and it was found that sub-basins with dominant landuse as forest had high infiltration rate among prevailing landuse types. Conversely, low infiltration rate was observed for barren area, snow/glacier and grassland landcover type dominated subbasins. A positive correlation among rainfall rate and infiltration rate was seen with linear increase in infiltration rate for an exponential increase of average rainfall intensity. Infiltration rate was found to have positive correlation with the Hydrologic Soil Group types as suggested by NRCS. Moreover, the study signified a greater impact of landcover over soil types on infiltration rates. Whereas, no significant impact of basin slope on infiltration rate could be identified, which may be due to preclusion of multiple topographic features. Understanding the impacts of rainfall intensity and surface characteristics on infiltration enables proactive measures to mitigate the issues like landslide and reduce flooding and soil erosion by improving infiltration rates through surface condition assessment.
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