The Main Factors Affecting Isotopes of Yellow River Water in China
Variation of δ 18 O, δD, and 3 H in the Yellow River water were analyzed based on the isotope test results of water samples in 18 sections of the Yellow River in rainy and dry seasons. The results show the trend of the ratios of the stable isotopes increases while the 3 H concentration decreases pro...
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| Published in | Water international Vol. 29; no. 4; pp. 475 - 482 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Taylor & Francis Group
01.12.2004
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| Subjects | |
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| Abstract | Variation of δ
18
O, δD, and
3
H in the Yellow River water were analyzed based on the isotope test results of water samples in 18 sections of the Yellow River in rainy and dry seasons. The results show the trend of the ratios of the stable isotopes increases while the
3
H concentration decreases progressively from the river source to the estuary. The main factors affecting the isotopes in the river water are the mixing of foreign water bodies, evaporation, and human activities. River runoff mostly comes from the source and the middle reaches of the river. The changes of the isotopes in the river water could be served as a good indicator of the recharge of different foreign water to the Yellow River. |
|---|---|
| AbstractList | Variation of δ
18
O, δD, and
3
H in the Yellow River water were analyzed based on the isotope test results of water samples in 18 sections of the Yellow River in rainy and dry seasons. The results show the trend of the ratios of the stable isotopes increases while the
3
H concentration decreases progressively from the river source to the estuary. The main factors affecting the isotopes in the river water are the mixing of foreign water bodies, evaporation, and human activities. River runoff mostly comes from the source and the middle reaches of the river. The changes of the isotopes in the river water could be served as a good indicator of the recharge of different foreign water to the Yellow River. Variation of d18O, dD, and 3H in the Yellow River water were analyzed based on the isotope test results of water samples in 18 sections of the Yellow River in rainy and dry seasons. The results show the trend of the ratios of the stable isotopes increases while the 3H concentration decreases progressively from the river source to the estuary. The main factors affecting the isotopes in the river water are the mixing of foreign water bodies, evaporation, and human activities. River runoff mostly comes from the source and the middle reaches of the river. The changes of the isotopes in the river water could be served as a good indicator of the recharge of different foreign water to the Yellow River. |
| Author | Su, Xiaosi Wang, Jinsheng Lin, Xueyu Liao, Zisheng |
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| CitedBy_id | crossref_primary_10_1016_j_marpolbul_2022_113532 crossref_primary_10_1016_j_apgeochem_2017_12_016 crossref_primary_10_1007_s10967_018_6272_8 crossref_primary_10_3390_ijerph16244932 crossref_primary_10_1016_j_ecolind_2021_108422 crossref_primary_10_1007_s00254_007_1059_1 crossref_primary_10_1029_2023JC020590 crossref_primary_10_2166_nh_2017_027 |
| Cites_doi | 10.1016/B978-0-444-81546-0.50010-0 10.1111/j.2153-3490.1953.tb01076.x 10.1111/j.2153-3490.1964.tb00181.x 10.1177/030913339401800102 10.1126/science.133.3465.1702 10.1016/0022-1694(86)90047-8 |
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| EndPage | 482 |
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| References | Wei K. (CIT0009) 1983; 10 Clark I. (CIT0002) 1997 Ingraham N. (CIT0007) 1998 Zhang X. (CIT0010) 2001; 31 CIT0001 CIT0003 CIT0005 CIT0004 Zhang X. (CIT0011) 1996; 18 CIT0006 CIT0008 Zhu X. (CIT0012) 1999 |
| References_xml | – ident: CIT0006 – volume: 31 start-page: 353 year: 2001 ident: CIT0010 publication-title: Science in China, Series D contributor: fullname: Zhang X. – start-page: 87 volume-title: Isotope Tracers in Catchment Hydrology. year: 1998 ident: CIT0007 doi: 10.1016/B978-0-444-81546-0.50010-0 contributor: fullname: Ingraham N. – ident: CIT0004 doi: 10.1111/j.2153-3490.1953.tb01076.x – volume: 18 start-page: 360 year: 1996 ident: CIT0011 publication-title: Journal of Glaciology and Geocryology contributor: fullname: Zhang X. – volume-title: Environmental Isotopes in Hydrogeology. year: 1997 ident: CIT0002 contributor: fullname: Clark I. – volume: 10 start-page: 467 year: 1983 ident: CIT0009 publication-title: Science Bulletin contributor: fullname: Wei K. – ident: CIT0005 doi: 10.1111/j.2153-3490.1964.tb00181.x – volume-title: Research about the variation of the water resources in the Yellow River water. year: 1999 ident: CIT0012 contributor: fullname: Zhu X. – ident: CIT0001 doi: 10.1177/030913339401800102 – ident: CIT0003 doi: 10.1126/science.133.3465.1702 – ident: CIT0008 doi: 10.1016/0022-1694(86)90047-8 |
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| Snippet | Variation of δ
18
O, δD, and
3
H in the Yellow River water were analyzed based on the isotope test results of water samples in 18 sections of the Yellow River... Variation of d18O, dD, and 3H in the Yellow River water were analyzed based on the isotope test results of water samples in 18 sections of the Yellow River in... |
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| Title | The Main Factors Affecting Isotopes of Yellow River Water in China |
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