西爪哇茂物潘卡山降雨入渗率分析

Syahra Kamila Khairani, M. Apriniyadi, Muhammad Adimas Amri
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引用次数: 0

摘要

入渗速率和降雨量是确定集水区的参数之一。在降雨量大的地区,成为集水区是非常好的。必须对集水区进行维护和保护,使其能够用于增加地下水储量和防止洪水,因此在确定集水区时需要一个空间规划。本研究旨在确定西爪哇茂物潘加尔山地区的渗透率。采用双环入渗仪直接在田间采集入渗速率数据,降雨数据由Citeko站BMKG数据获取。这些数据的最终结果将制成入渗率图和降雨量图。研究区入渗速率为0.096 m/d ~ 0.553 m/d,年降雨量在3000 mm以上。从这些数据可以看出,在确定集水区时,入渗速率与降雨量是密切相关的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALYSIS OF INFILTRATION RATE OF RAINFALL IN MOUNT PANCAR, BOGOR, WEST JAVA
Infiltration rate and rainfall are one of the parameters in determining water catchment areas. In an area that has a high level of rainfall, it is very good to be a water catchment area. Water catchment areas must be maintained and protected so that they can be used to incrase groundwater reserves and prevent flooding, so a spatial plan is needed in determining water catchment areas. This study aims to determine the rate of infiltration in the ara of Mount Pancar, Bogor, West Java. Infiltration rate data was collected directly in the field using a double ring infiltrometer and rainfall data was obtained from BMKG data at Citeko Station. The final result of these data will be made a map of the infiltration rate and rainfall map. The results of the study in the study area obtained an infiltration rate of 0,096 m/day – 0,553 m/day with rainfaal of more than 3000 mm/year. From these data, it can be concluded that the rate og infiltration and rainfall are closely related to each other in determining water catchment areas.
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