2023
DOI: 10.1016/j.chemer.2023.125974
|View full text |Cite
|
Sign up to set email alerts
|

Geochemical characterization, its controlling factors, and comparison between the upstream and downstream segments of the Himalayan Satluj River basin, India

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2024
2024
2024
2024

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 8 publications
(2 citation statements)
references
References 144 publications
0
2
0
Order By: Relevance
“…Gibbs defined the mechanisms controlling world surface water chemistry as three end-members: atmospheric precipitation, rock dominance, and the evaporation-crystallization process. To distinguish the contribution of the three end-members, TDS versus Na + /(Na + +Ca 2+ ) or Cl -/(Cl -+HCO 3 -) are used [75]. The Gibbs schematic diagram is shown in Figure 7.…”
Section: Analysis Of Hydrochemical Characteristics and Main Control F...mentioning
confidence: 99%
See 1 more Smart Citation
“…Gibbs defined the mechanisms controlling world surface water chemistry as three end-members: atmospheric precipitation, rock dominance, and the evaporation-crystallization process. To distinguish the contribution of the three end-members, TDS versus Na + /(Na + +Ca 2+ ) or Cl -/(Cl -+HCO 3 -) are used [75]. The Gibbs schematic diagram is shown in Figure 7.…”
Section: Analysis Of Hydrochemical Characteristics and Main Control F...mentioning
confidence: 99%
“…Due to the influence of geology, climate, and human activities [1,2], the ion composition and distribution of river water could directly reflect the basic characteristics of the basin, even the history of water formation and migration [3]. After different physical and geochemical processes, the content and distribution of different ions not only reflected the different hydrochemical characteristics, but also reflected the relationship between the source, migration, and transformation of solutes and regional natural conditions [4][5][6]. Generally, the solutes of surface water are mainly derived from rock weathering and the erosion of soils in the drainage basin; these processes are the major components of the exogenic cycle of elements in the continent-river-ocean system [7,8].…”
Section: Introductionmentioning
confidence: 99%