Assessment of mining activity on arsenic contamination in surface water and sediments in southwestern area of Santurbán paramo, Colombia

2020 ◽  
Vol 264 ◽  
pp. 110478 ◽  
Author(s):  
David L. Alonso ◽  
Rodrigo Pérez ◽  
Coco K.Y.A. Okio ◽  
Elianna Castillo
2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Łukasz Stachnik ◽  
Bartosz Korabiewski ◽  
Jerzy Raczyk ◽  
Michał Łopuch ◽  
Iwo Wieczorek

Abstract Contamination of water and sediments with arsenic and heavy metals is a global issue affecting human health. Regions covered with Quaternary deposits have received little attention from the point of view of the flux of arsenic and heavy metals from sediments to surface water. This study aims to determine the flux of arsenic and other heavy metals from Quaternary sediments to surface waters in an area affected by the former Złoty Stok gold and arsenic mine. Contamination in surface waters and sediments was caused by arsenic, whereas concentrations of metals were usually within water quality standards. Arsenic contamination of surface water increased in the lower part of the basin covered by Quaternary sediments, and exceeded water quality standards by 2 orders of magnitude. Arsenic mass flux exceeded 8 kg/day near the confluence of the Trująca River with the Nysa Kłodzka, a main tributary of the Oder River. An increase in arsenic concentration in the lower part of the basin is related to mine tailings and preferential flow of groundwater through Quaternary sediments. In future, water resources scarcity may lead to an increase in arsenic contamination in surface and groundwater.


2017 ◽  
Vol 18 (1) ◽  
Author(s):  
John C. Ayers ◽  
Gregory George ◽  
David Fry ◽  
Laura Benneyworth ◽  
Carol Wilson ◽  
...  

Author(s):  
John M. Wehrung ◽  
Richard J. Harniman

Water tables in aquifer regions of the southwest United States are dropping off at a rate which is greater than can be replaced by natural means. It is estimated that by 1985 wells will run dry in this region unless adequate artificial recharging can be accomplished. Recharging with surface water is limited by the plugging of permeable rock formations underground by clay particles and organic debris.A controlled study was initiated in which sand grains were used as the rock formation and water with known clay concentrations as the recharge media. The plugging mechanism was investigated by direct observation in the SEM of frozen hydrated sand samples from selected depths.


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