Spatial assessment of major ion geochemistry in the groundwater around Suryapet Region, Southern Telangana, India

2020 ◽  
Author(s):  
Shankaraiah Katla ◽  
Sakram Gugulothu ◽  
Ratnakar Dhakate
Keyword(s):  
Spatial Assessment ◽  
Major Ion ◽  
Major Ion Geochemistry

STABLE ISOTOPE AND MAJOR ION GEOCHEMISTRY OF URBAN PRECIPITATION

2017 ◽  
Author(s):  
Devin F. Smith ◽  
◽  
Elsa Saelens ◽  
Deborah Leselie ◽  
Marcus Liston ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Major Ion ◽  
Major Ion Geochemistry

scholarly journals Major ion geochemistry in Na-Ca-Mg-K-Cl-SO4 brines using portable X-ray fluorescence spectrometry

2020 ◽  
Vol 558 ◽  
pp. 119865
Author(s):  
Evan L. Kipnis ◽  
Brenda B. Bowen ◽  
Sean J. Hutchings ◽  
Scott A. Hynek ◽  
Kathleen C. Benison
Keyword(s):  
Fluorescence Spectrometry ◽  
X Ray ◽  
Major Ion ◽  
Major Ion Geochemistry

scholarly journals Characterization of Flowpath Using Geochemistry and 87Sr/86Sr Isotope Ratios in the Yalahau Region, Yucatan Peninsula, Mexico

Water ◽  
2020 ◽  
Vol 12 (9) ◽  
pp. 2587
Author(s):  
Jessica McKay ◽  
Melissa Lenczewski ◽  
Rosa Maria Leal-Bautista
Keyword(s):  
Yucatan Peninsula ◽  
Isotope Ratios ◽  
Water Withdrawal ◽  
Flow Paths ◽  
Major Ion ◽  
Yucatán Peninsula ◽  
Major Ion Geochemistry ◽  
The Impact ◽  
Yalahau Region

The Yalahau region, located in the northeastern portion of the Yucatán Peninsula, hosts a series of elongated depressions trending north/south in the direction of Isla Holbox, identified as the Holbox Fracture Zone. Previous studies have explored the geomorphology and various hydrologic characteristics of the Yucatán Peninsula; however, there is a paucity of data concerning the interior region where the fractures are located. Strontium isotope ratios and major ion geochemistry data of the surface water and groundwater of this region serve as a hydrogeochemical fingerprint, aiding in constraining the hydrological boundaries, determining flow paths, and characterizing hydrogeochemical processes that impact the composition of the groundwater within the region. 87Sr/86Sr isotope ratios indicate a different signature than the surrounding bedrock Sr ratio, suggesting that the flow throughout the Yalahau region is moving through channels faster than that of much of the Yucatán. Through major ion geochemistry and 87Sr/86Sr isotope ratios, we were able to delineate at least two flow paths within the Yalahau region and identify a point of saline intrusion at least 35 km from the coast. Gaining an understanding of the hydrogeochemistry and water flow regions is crucial in determining the impact of various activities (e.g., extensive tourism, drinking water withdrawal, wastewater discharge/injection) that occur within the Yucatán Peninsula.

Strontium isotope characterization and major ion geochemistry of karst water flow, Shentou, northern China

2006 ◽  
Vol 328 (3-4) ◽  
pp. 592-603 ◽  
Author(s):  
Yanxin Wang ◽  
Qinghai Guo ◽  
Chunli Su ◽  
Teng Ma
Keyword(s):  
Water Flow ◽  
Northern China ◽  
Strontium Isotope ◽  
Karst Water ◽  
Major Ion ◽  
Major Ion Geochemistry

Major ion geochemistry of Godavari River at Rajahmundry, India

2006 ◽  
Vol 25 (S1) ◽  
pp. 268-269
Author(s):  
K. Balakrishna ◽  
S. S. Suvarna ◽  
G. Srinikethan ◽  
G. Mugeraya ◽  
P. K. Krishnakumar
Keyword(s):  
Major Ion ◽  
Godavari River ◽  
Major Ion Geochemistry

Major Ion Geochemistry of Nam Co Lake and its Sources, Tibetan Plateau

2008 ◽  
Vol 14 (4) ◽  
pp. 321-336 ◽  
Author(s):  
Qianggong Zhang ◽  
Shichang Kang ◽  
Feiyue Wang ◽  
Chaoliu Li ◽  
Yanwei Xu
Keyword(s):  
Tibetan Plateau ◽  
Nam Co ◽  
Major Ion ◽  
Major Ion Geochemistry ◽  
Nam Co Lake
Sign in / Sign up

Export Citation Format

Share Document