ANALYSIS OF GROUNDWATER FACIES IN PARAKAN OMAS AND SURROUNDING REGIONS, RUMPIN DISTRICT, BOGOR REGENCY, WEST JAVA, TO DETERMINE GROUNDWATER FACIES.

Ruli Firmanda, S. D. Nuryana, Muhammad Adimas Amri
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Abstract

The research area is located in Parakan Omas Village, Rumpin District, Bogor Regency, West Java Province. The background of this research was to determine the chemical properties of groundwater in the springs in the Parakan Omas area. The method used is taking samples of springs from springs and chemical analysis of the main ions (Mg⁺, Ca²⁺, Na⁺, K⁺, Cl⁻, SO₄²⁻, HCO₃⁻, CO₃⁻) and getting 5 samples of springs entered into the laboratory. The purpose of this study was to determine the chemical characteristics of groundwater in Rumpin sub-district. Lithological conditions affect groundwater facies, volcanic rocks cause groundwater to contain mineral cations Mg⁺ and Ca²⁺ with varying anions while alluvium layers in land areas will cause groundwater to be rich in sodium (Na⁺) minerals with anions in the form of chloride (Cl⁻) or sulfate ( SO₄²⁻). Data analysis using piper trilinear diagram. The diagram shows that there are 2 types of facies in the dominant research area, namely Sodium Potassium Bicarbonate (Na+ + K+ HCO3- ) and Calcium Magnesium Bicarbonate (Ca2+ + Mg2+HCO3⁻).
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西爪哇茂物县朗平区parakan omas及其周边地区地下水相分析,确定地下水相。
研究区域位于西爪哇省茂物县Rumpin区Parakan Omas村。本研究的背景是确定Parakan Omas地区泉水中地下水的化学性质。所用的方法是从泉水中取样,并对主要离子(Mg⁺、Ca²⁺、Na⁺、K⁺、Cl⁻、SO₄²⁻、HCO₃⁻、CO₃⁻)进行化学分析,得到5个样品进入实验室。本研究的目的是确定龙坪街道地下水的化学特征。岩性条件影响地下水相,火山岩使地下水含有矿物阳离子Mg +和Ca 2 +,它们含有不同的阴离子,而陆地上的冲积层会使地下水含有丰富的钠(Na +)矿物,其阴离子以氯化物(Cl⁻)或硫酸盐(SO₄²⁻)的形式存在。数据分析使用piper三线性图。从图中可以看出,研究区主要存在两种相,即碳酸氢钠钾(Na+ + K+ HCO3-)和碳酸氢钙镁(Ca2+ + Mg2+HCO3 -)。
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