在丘陵地带对含水层的免费体积预测,使用不同的方法

M. Juandi, Muhammad Syahputra Syahputra, Usman Malik
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引用次数: 0

摘要

利用有限差分法对武吉拉雅地区无承压含水层进行了预测研究。利用计算机程序MATLAB应用R2009a版本,对武吉拉雅地区2015年无约束含水层深度数据进行了等高线网格数值求解。本研究的目的是分析人口增长对武吉拉雅地区无承压含水层体积的影响。研究结果可告知武吉拉雅区如下:2017年地下水总量为10.931.060,63 m3, 2021年为10.931.060,63 m3。2017年居民地下水取水量为5.038.007,328m3, 2021年居民地下水取水量为5.334.525,03 m3。地下水(残余物)减少量的增加,使得2017年地下水减少量的增加高达5.361.608 m3, 2021年高达5.596.5355.6 m3。可以得出地下水量受含水层深度变化和绿地面积大小的影响
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PREDIKSI VOLUME AKUIFER BEBAS DI KECAMATAN BUKIT RAYA DENGAN METODE BEDA HINGGA
A research about prediction of  unconfined aquifer in Distrcit Bukit Raya have been done by using  finite difference method. The depth of unconfined aquifer data using contour grid District Bukit Raya in 2015 solved numerically by using computer program MATLAB application R2009a version. The aim of this research was to analyze the effect of population growth on the volume of unconfined aquifer in District Bukit Raya. The result of the research could be informed to District Bukit Raya as follows : the total volume of underground water in 2017 in the amount of 10.399.615,33 m3 and in 2021 in the amount of 10.931.060,63 m3. the volume of underground water that taken by residents in 2017 were in the amount of 5.038.007,328m3and in 2021 were in the amount of 5.334.525,03 m3. The inreasing of lowering the volume of underground water (residue), so that in 2017 The inreasing of loweringthe volume of underground wateras much as5.361.608 m3and in 2021 as much as 5.596.535,6 m3. It can be concluded that the volume of underground waterinfluenced by the changes of the dept of aquifer and the large of green open space
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