Simulating seawater intrusion in a complex coastal karst aquifer using an improved variable-density flow and solute transport-conduit flow process model

被引:0
作者
Xu, Zhongyuan [1 ,2 ]
Hu, Bill X. [3 ,4 ]
Xu, Zexuan [5 ]
Wu, Xiujie [2 ]
机构
[1] Univ Delaware, Coll Earth Ocean & Environm, Newark, DE 19716 USA
[2] Chengdu Univ Technol, Coll Environm & Civil Engn, Chengdu 610059, Sichuan, Peoples R China
[3] China Univ Geosci Beijing, Sch Water Resources & Environm, Beijing 100083, Peoples R China
[4] Jinan Univ, Inst Groundwater & Earth Sci, Guangzhou 510632, Guangdong, Peoples R China
[5] Lawrence Berkeley Natl Lab, Climate & Ecosyst Sci Div, Berkeley, CA 94720 USA
基金
中国国家自然科学基金;
关键词
Karst; Numerical modeling; Seawater intrusion; VDFST-CFP; FRICTION FACTOR; APPROXIMATIONS;
D O I
10.1007/s10040-018-1903-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
VDFST-CFP (variable-density flow and solute transport-conduit flow process) is a density-dependent discrete-continuum numerical model for simulating seawater intrusion in a dual-permeability coastal karst aquifer. A previous study (Xu and Hu 2017) simulates variable-density flow only in a single conduit, and studies the parameter sensitivities only in the horizontal case (2D domain as horizontal section) by the VDFST-CFP model. This paper focuses on the density-dependent vertical case (2D domain as vertical section) with two major improvements: 1) when implementing double-conduit networks in the domain, simulated intruded plumes in the porous medium are extended in the double-conduit scenario, compared to the single-conduit system; 2) by quantifying micro-textures on the conduit wall by the Goudar-Sonnad equation and considering macro-structures as local head loss. Sensitivity analysis shows that medium hydraulic conductivity, conduit diameter and effective porosity are important parameters for simulating seawater intrusion in the discrete-continuum system. On the other hand, rougher micro-structures and additional macro-structure components on the conduit wall would reduce the distance of seawater intrusion to the conduit system, but, rarely affect salinity distribution in the matrix. Compared to the equivalent mean roughness height, the new method (with more detailed description of structure) simulates seawater intrusion slightly landward in the conduit system. The macro-structure measured by local head loss is more reasonable but needs further study on conduit flow. Xu and Hu (2017) Development of a discrete-continuum VDFST-CFP numerical model for simulating seawater intrusion to a coastal karst aquifer with a conduit system. Water Resources Research: 53, 688-711.
引用
收藏
页码:1277 / 1289
页数:13
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