scholarly journals Micro-geochemistry and Micro-geomechanics towards understanding proppant shale rock interaction: A Caney shale case study, USA

2021 ◽  
Author(s):  
Allan Katende ◽  
Jonny Rutqvist ◽  
Margaret Benge ◽  
Abbas Seyedolali ◽  
Andrew Bunger ◽  
...  
Keyword(s):  
Rock Interaction ◽  
Shale Rock

scholarly journals Groundwater Baseline Water Quality in a Shale Gas Exploration Site and Fracturing Fluid - Shale Rock Interaction

2017 ◽  
Vol 17 ◽  
pp. 638-641 ◽  
Author(s):  
Tianming Huang ◽  
Yiman Li ◽  
Zhonghe Pang ◽  
Yingchun Wang ◽  
Shuo Yang
Keyword(s):  
Water Quality ◽  
Shale Gas ◽  
Fracturing Fluid ◽  
Rock Interaction ◽  
Shale Rock

scholarly journals On the use of Li isotopes as a proxy for water–rock interaction in fractured crystalline rocks: A case study from the Gotthard rail base tunnel

2017 ◽  
Vol 198 ◽  
pp. 396-418 ◽  
Author(s):  
Christoph Wanner ◽  
Kurt Bucher ◽  
Philip A.E. Pogge von Strandmann ◽  
H. Niklaus Waber ◽  
Thomas Pettke
Keyword(s):  
Crystalline Rocks ◽  
Rock Interaction ◽  
Fractured Crystalline Rocks ◽  
Water Rock Interaction

scholarly journals Silicon in ultrafresh groundwater: a case study of the Imandra Lake catchment, The Kola Peninsula

2019 ◽  
Vol 98 ◽  
pp. 01018
Author(s):  
Natalia V. Guseva ◽  
Yuliya G. Kopylova ◽  
Daria A Vorobeva ◽  
Albina A. Khvashchevskaya ◽  
Zinaida A. Evtyugina
Keyword(s):  
Kola Peninsula ◽  
Catchment Area ◽  
Water Exchange ◽  
Rock Interaction ◽  
Silicon Oxides ◽  
Short Period ◽  
Lake Catchment ◽  
Imandra Lake ◽  
Water Rock Interaction

The ultrafresh groundwater (with TDS values less than 200 mg/L) of the Imandra Lake catchment, Kola Peninsula, is from an intensive water exchange zone, where the water has a short period of contact with the rock. Therefore, the considered water is at the initial stages of the water–rock interaction. The water is saturated with respect to oxides and hydroxides of aluminium and iron. In the groundwater of the Imandra Lake catchment area, the silicon concentrations significantly exceed the concentrations of magnesium and especially potassium. Nevertheless, water is undersaturated with respect to with respect to silicon oxides. The shown enrichment of water with cations is explained by time of water-rock interaction.

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