4.6 Article

Trace Metals and Metalloids Present in Springwater of a Mining Area: Assessment Based on Chemical and Isotopic Data (δ2H, δ18O, 3H and 87Sr/86Sr)

Journal

WATER
Volume 15, Issue 10, Pages -

Publisher

MDPI
DOI: 10.3390/w15101917

Keywords

springwater; water isotopes; water rock interactions; Sr-87/Sr-86 ratio; mixing processes

Ask authors/readers for more resources

The Taxco mining district in Mexico is internationally known for its production of silver, jewelry, and precious metal handicrafts. Improper disposal of waste from human activities has been causing contamination of the springwater, which is used for drinking and domestic purposes by the residents, thus posing a health threat. A study was conducted using a multi-tracer approach to analyze the springwater samples, including hydrochemical data, trace elements, and isotopes d(2)H, d(18)O, H-3, and Sr-87/Sr-86 ratios. The results showed the origin and age of the springwater, as well as the water-rock interactions and flow paths, highlighting the potential of using Sr-87/Sr-86 ratios as a fingerprint for further studies.
The Taxco mining district is a well-known international producer of silver, jewelry, and precious metal handicrafts. Inappropriate disposal wastes from anthropogenic activities have been deteriorating the hydric resources and threatening the inhabitants' health, since they use the springwater for human consumption and domestic activities. A multi-tracer approach combining measurements of hydrochemical data, trace elements, and isotopes d(2)H, d(18)O, H-3, and Sr-87/Sr-86 ratios was undertaken for 18 springwater samples. d(18)O and d(2)H indicate that the springwater comes from the rain and had experienced some degree of isotopic fractionation by atmospheric evaporation in some samples at lower altitudes. H-3 values on the springwater showed the existence of old and new water. Three groups of springwater were identified according to age: local flow in rhyolites, intermediate flow through red beds to the outcrop point in sandstone and shales, and deep flow in greenschist. The results of this study show the utility of Sr-87/Sr-86 ratios in identifying the water-rock interactions and springwater flow paths, suggesting that more widespread use of the strontium isotopic fingerprint is warranted.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.6
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available