Calculation of Potential Groundwater Resources in Orkhon River Basin

D. Batjargal, N. Batsukh
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引用次数: 2

Abstract

Available groundwater research work and data levels are very limited due to the wide territory of our country. Potential Groundwater resources need to be calculated by basin to implement Integrated Water Resources Management Plans. For this purpose, previously the calculations were done twice in the Orkhon River Basin. The last calculation was done 10 years ago, therefore Integrated Water Resources Management Plan needs to be redeveloped, using updated research work and data levels. The Orkhon River is one of the biggest rivers in Mongolia, rising from Khangai Mountain Range and flowing into the Selenge River. The Orkhon River Basin includes the Tuul, Kharaa, and Yeruu rivers basins which rise in the Khentii Mountains. For the first time, a hydrogeological structure map of the basin was developed which analyzed and systemized the hydrogeological structure, the morphostructure factors, and the hydraulic properties of the hydrogeological formations distributed in the Orkhon River Basin. There are two types of hydrogeological basins and three types of hydrogeological massifs in the basin. This paper presents the calculation of the Potential Groundwater Resources (PGR) in the Orkhon River Basin based on groundwater well data, reports of groundwater exploration and research works, and the hydrogeological maps at a scale of 1:500,000. As a result of this calculation, there are 1.99 km3 of PGR in this basin.The largest resources are found in the linear intermountain hydrogeological basin which occupies 98 percent of the total PGR. Further improvement of the quality and standards of water research remains an important issue for hydrogeologists today.
鄂尔浑河流域潜在地下水资源量计算
由于我国幅员辽阔,可用的地下水研究工作和数据水平非常有限。需要按流域计算潜在地下水资源,以实施水资源综合管理计划。为此,之前在奥尔洪河流域进行了两次计算。上一次计算是在10年前完成的,因此需要利用最新的研究工作和数据水平重新制定水资源综合管理计划。鄂尔浑河是蒙古国最大的河流之一,发源于汗盖山脉,汇入色兰热河。鄂尔浑河流域包括发源于肯特山脉的Tuul河、Kharaa河和Yeruu河流域。首次绘制了该流域的水文地质结构图,对鄂尔浑河流域分布的水文地质构造、形态结构因素和水文地质性质进行了分析和系统化。流域内有两类水文地质盆地和三类水文地质地块。本文根据地下水井数据、地下水勘探和研究工作报告以及比例尺为1:500000的水文地质图,计算了奥尔洪河流域的潜在地下水资源量。根据该计算结果,该盆地的PGR为1.99km3。资源量最大的是线性山间水文地质盆地,占总PGR的98%。进一步提高水研究的质量和标准仍然是当今水文地质学家面临的一个重要问题。
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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来源期刊
CiteScore
0.70
自引率
0.00%
发文量
4
审稿时长
8 weeks
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