Prospective policy safeguards to mitigate hydrogeological risk pathways in advance of shale gas development in the Karoo basin, South Africa

被引:3
|
作者
Pietersen, Kevin [1 ]
Chevallier, Luc [2 ]
Levine, Audrey [1 ,3 ]
Maceba, Thandokazi [1 ]
Gaffoor, Zaheed [1 ]
Kanyerere, Thokozani [1 ]
机构
[1] Univ Western Cape, Private Bag X17, ZA-7535 Bellville, South Africa
[2] Council Geosci, POB 572, ZA-7535 Bellville, South Africa
[3] Cty Santa Cruz Hlth Serv Agcy, Environm Hlth Div, 701 Ocean St,Room 312, Santa Cruz, CA 95060 USA
关键词
Shale gas; Hydrogeologic risk pathways; Karoo basin; Adaptive management policies; POTENTIAL CONTAMINANT PATHWAYS; HYDRAULICALLY FRACTURED SHALE; PERMIAN BLACK SHALES; DRINKING-WATER; METHANE CONTAMINATION; GROUNDWATER; WELLS; MIGRATION; AQUIFERS; FLUID;
D O I
10.1016/j.gsd.2020.100499
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Policies surrounding energy development are frequently implemented in response to known or perceived problems. South Africa is in a unique position to develop prospective policies that build on knowledge gained from elsewhere. This paper provides a prospective analysis of hydrogeological risk pathways and vulnerability attributes in advance of anticipated shale gas operations in the Karoo Basin of South Africa. The 'hazard-pathways-receptors' approach is applied to define the hydrogeologic system in the context of potential sources of water resource contamination. This case study focuses on two critical hydrogeological risk pathways: regional groundwater flow and discrete structural features. Depending on the targeted area (hydro-litho-structural domain, depth of target, presence of aquitard, intrusion ratio), the capacity of deep natural pathways to enable hydraulic fracturing fluids, chemicals, or produced water to reach shallow groundwater, will be reduced or difficult. Deep artesian water could however be intercepted at different depths and, based on past groundwater exploration in the Karoo, water could flow into horizontal fractures or openings characterising the shallow aquifers: sills-ring complexes, lithological contacts, and transgressive fractures across dolerite dykes. However, above-ground water and wastewater management safeguards are needed to protect shallow groundwater from potential water quality degradation due to a) flowback or produced water b) stray gas and/or c) spills or illicit discharges that could introduce contaminants into groundwater resources. This paper describes a systematic approach to evaluate hydrogeologic risk pathways and informs adaptive management policies to protect South African groundwater resources.
引用
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页数:11
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