IDENTIFIKASI KUALITAS CADANGAN AIR TANAH DI KECAMATAN SEKARAN KABUPATEN LAMONGAN

Rifko Harny Dwi Cahyo, I. Rahayu
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Abstract

Groundwater is part of the hydrological cycle located below the earth's surface in the pores and crevices of rocks and soil. Water scarcity is increasing around the world and the need for water presence is increasing due to growing demands in several fields. Geologically, Sekaran District is composed of alluvium formations where this formation consists of kerakal, gravel, silt sand, clay, local fragments of fossil shells and mud. This study was conducted to determine the quality of groundwater reserves based on the value of solute solids. The method carried out by taking water samples in the wells of residents' houses in Sekaran District.After data processing was carried out, it was found that the quality of groundwater reserves based on the value of dissolved materials in Sekaran District ranged from 50-950 ppm and based on electrical conductivity values ranging from 100-2000 ?S/cm.
地下水是水文循环的一部分,位于地表以下的岩石和土壤的孔隙和裂缝中。世界各地的水资源短缺正在加剧,由于几个领域的需求不断增长,对水存在的需求也在增加。在地质上,Sekaran地区由冲积层组成,冲积层由喀拉喀尔、砾石、粉砂、粘土、当地的化石贝壳碎片和泥浆组成。本研究是基于溶质固体的数值来确定地下水储量的质量。该方法通过在Sekaran区居民住宅的水井中采集水样进行。经过数据处理,发现Sekaran地区地下水储量的质量范围为50-950 ppm,电导率范围为100-2000 μ S/cm。
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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