Improving large-scale groundwater models by considering fossil gradients
Improving large-scale groundwater models by considering fossil gradients
复制标题
通过考虑化石梯度改进大规模地下水模型
DOI:
10.1016/j.advwatres.2017.02.010
复制
发表时间:
2017
影响因子:
4.7
通讯作者:
C. Schüth
中科院分区:
文献类型:
--
作者:
S. Schulz;M. Walther;N. Michelsen;R. Rausch;H. Dirks;M. Al;R. Merz;O. Kolditz;C. Schüth
Due to limited availability of surface water, many arid to semi-arid countries rely on their groundwater resources. Despite the quasi-absence of present day replenishment, some of these groundwater bodies contain large amounts of water, which was recharged during pluvial periods of the Late Pleistocene to Early Holocene. These mostly fossil, non-renewable resources require different management schemes compared to those which are usually applied in renewable systems. Fossil groundwater is a finite resource and its withdrawal implies mining of aquifer storage reserves. Although they receive almost no recharge, some of them show notable hydraulic gradients and a flow towards their discharge areas, even without pumping. As a result, these systems have more discharge than recharge and hence are not in steady state, which makes their modelling, in particular the calibration, very challenging. In this study, we introduce a new calibration approach, composed of four steps: (i) estimating the fossil discharge component, (ii) determining the origin of fossil discharge, (iii) fitting the hydraulic conductivity with a pseudo steady-state model, and (iv) fitting the storage capacity with a transient model by reconstructing head drawdown induced by pumping activities. Finally, we test the relevance of our approach and evaluated the effect of considering or ignoring fossil gradients on aquifer parameterization for the Upper Mega Aquifer (UMA) on the Arabian Peninsula.
影响因子:
2.2
作者:
Engel, Max;Brueckner, Helmut;Frenzel, Peter
通讯作者:
Frenzel, Peter