Hydrogeology and geochemistry of low-permeability oil-shales – Case study from HaShfela sub-basin, Israel

• Published in: Journal of hydrology (Amsterdam) Vol. 540; pp. 1105 - 1121
• Main Authors: Burg, Avihu, Gersman, Ronen
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.09.2016
• Subjects: Computational fluid dynamics; Flow Zone Indicator (FZI); Fluid flow; Hydraulics; Hydrogeology; Low hydraulic conductivity; Mathematical models; Oil shale; Permeability; Resistivity logs; Rocks; Slug tests: Kozeny-Carman approach; Slugs; Israel; Resistivity logs; Oil shale; Low hydraulic conductivity; Flow Zone Indicator (FZI); Slug tests: Kozeny-Carman approach
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2016.07.026

[Display omitted] •The oil shale (OSU) in central Israel form a thick aquiclude.•Slug tests confirm low hydraulic conductivity of the OSU despite its high porosity.•Despite the low conductivity, water flow is mostly gravitationally-driven.•The salinity originates from residual marine water, ancient as Pliocene.•Our results may help in risk evaluation model for waste burial in aquicludic units. Low permeability rocks are of great importance given their potential role in protecting underlying aquifers from surface and buried contaminants. Nevertheless, only limited data for these rocks is available. New appraisal wells drilled into the oil shale unit (OSU) of the Mt. Scopus Group in the HaShfela sub-basin, Central Israel, provided a one-time opportunity for detailed study of the hydrogeology and geochemistry of this very low permeability unit. Methods used include: slug tests, electrical logs, televiewer imaging, porosity and permeability measurements on core samples, chemical analyses of the rock column and groundwater analyses. Slug tests yielded primary indication to the low permeability of the OSU despite its high porosity (30–40%). Hydraulic conductivities as low as 10−10–10−12m/s were calculated, using both the Hvorslev and Cooper-Bredehoeft-Papadopulos decoding methods. These low conductivities were confirmed by direct measurements of permeability in cores, and from calculations based on the Kozeny-Carman approach. Storativity was found to be 1·10−6 and specific storage - 3.8·10−9m−1. Nevertheless, the very limited water flow in the OSU is argued to be driven gravitationally. The extremely slow recovery rates as well as the independent recovery of two adjacent wells, despite their initial large head difference of 214m, indicate that the natural fractures are tight and are impermeable due to the confining stress at depth. Laboratory measured permeability is similar or even higher than the field-measured values, thereby confirming that fractures and bedding planes do not form continuous flow paths. The vertical permeability along the OSU is highly variable, implying hydraulic stratification and extremely low vertical hydraulic conductivity. The high salinity of the groundwater (6300–8000 mgCl/L) within the OSU and its chemical and isotopic compositions are explained by the limited water flow, suggesting long residence time of the water, prolonged water-rock interaction and mixing with ancient trapped salty water. The current study demonstrates that targeted and detailed research of low permeability rocks can produce reliable hydraulic parameters using slug tests and accompanying methods. The data produced is of upmost importance for quantitative risk evaluations such as models for waste burial in low permeability units.