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Application of numerical modeling to study the circulation pattern of groundwater flow systems in the Cretaceous Basin of the Ordos Basin

机译:数值模拟在鄂尔多斯盆地白垩纪盆地地下水流动系统循环模式研究

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In the study on groundwater flow in large-scale basins, the first step is to understanding the regional patterns of groundwater formation and distribution. In this paper, groundwater flow, age and temperature were simulated for a cross-section in the Cretaceous Basin of the Ordos Basin. The 240 Km-long cross-section consists of the main aquifers of the study zone, and is one of the representative hydrogeological section. The results show that there are three groundwater flow systems. Discussions were presented on scaling features of the local, intermediate and regional flow system, on groundwater circulation amount, on groundwater age and on hydrogeological conditions. Circulation patterns of groundwater system in the Cretaceous Basin of the Ordos Basin were identified from the point of Spatial and temporal view.
机译:在大规模盆地地下水流的研究中,第一步是理解地下水形成和分布的区域模式。在本文中,模拟了鄂尔多斯盆地的白垩纪盆地横截面的地下水流动,年龄和温度。 240公里长的横截面由研究区的主要含水层组成,是代表水文层之一。结果表明,有三种地下水流量系统。在地下水年龄和水文地质条件下,讨论了本地,中级和区域流动系统的缩放特征,对地下水循环量。从空间和时间视图中鉴定了鄂尔多斯盆地白垩纪盆地地下水系统的循环模式。

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