首页> 外文期刊>Acta Geophysica >Delineating spring recharge areas inferred from morphological, lithological, and hydrological datasets on Quaternary volcanic landscapes at the southern flank of Rinjani Volcano, Lombok Island, Indonesia
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Delineating spring recharge areas inferred from morphological, lithological, and hydrological datasets on Quaternary volcanic landscapes at the southern flank of Rinjani Volcano, Lombok Island, Indonesia

机译:描绘从印度尼西亚龙目岛的林加尼火山南翼第四纪火山景观上的形态,岩性和水文数据集推断出的春季补给区

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Springs are a vital source of water supply in Quaternary volcanic environments, such as Rinjani Volcano on Lombok Island, and yet little is known about their emergence and recharge areas. Knowledge of spring recharge area can substantially support further spring analysis and management. This study was performed in two spring zones on the southern flank of Rinjani Volcano. It combined the available morphological, lithological, and hydrological datasets to build a conceptual model of the spring recharge areas. According to the analysis results, the conceptual model allowed to describe the flow medium, the aquifer type, and the characteristics of the flow system. The local morphology controlled the direction and gradient of groundwater flow to the springs. The analysis also revealed that the spring water in the study area was meteoric water, which mainly came from rainwater infiltration. Therefore, the boundaries of the spring recharge areas were represented by the morphological divides.
机译:温泉是第四纪火山环境中重要的水源,例如龙目岛上的林加尼火山,但对它们的出现和补给区知之甚少。弹簧补给区域的知识可以充分支持进一步的弹簧分析和管理。这项研究是在Rinjani火山南翼的两个春季区域进行的。它结合了可用的形态学,岩性和水文数据集,建立了春季补给区的概念模型。根据分析结果,该概念模型可以描述流动介质,含水层类型和流动系统的特征。局部形态控制着地下水流向泉水的方向和梯度。分析还显示,研究区的泉水是流水,主要来自雨水的渗透。因此,春季补给区的边界由形态学鸿沟来表示。

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