Carbon biogeochemistry of ground water, Guiyang, southwest China

Variations in the concentrations and isotopic compositions (delta13C(DIC)) of dissolved inorganic carbon (DIC) reflect contamination and biogeochemical cycling of the carbon in ground water. In order to understand contamination and biogeochemical cycling of DIC, we carried out research on the geoche...

Ausführliche Beschreibung

Bibliographische Detailangaben
Veröffentlicht in:Ground water. - 1979. - 43(2005), 4 vom: 15. Juli, Seite 494-9
1. Verfasser: Li, Si-Liang (VerfasserIn)
Weitere Verfasser: Liu, Cong-Qiang, Tao, Fa-Xiang, Lang, Yun-Chao, Han, Gui-Lin
Format: Aufsatz
Sprache:English
Veröffentlicht: 2005
Zugriff auf das übergeordnete Werk:Ground water
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Chlorides Nitrates Oxygen Isotopes Sulfates Sodium 9NEZ333N27 Magnesium I38ZP9992A mehr... Potassium RWP5GA015D Calcium SY7Q814VUP
LEADER 01000caa a22002652c 4500
001 NLM156653389
003 DE-627
005 20250206133358.0
007 tu
008 231223s2005 xx ||||| 00| ||eng c
028 5 2 |a pubmed25n0522.xml 
035 |a (DE-627)NLM156653389 
035 |a (NLM)16029175 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Li, Si-Liang  |e verfasserin  |4 aut 
245 1 0 |a Carbon biogeochemistry of ground water, Guiyang, southwest China 
264 1 |c 2005 
336 |a Text  |b txt  |2 rdacontent 
337 |a ohne Hilfsmittel zu benutzen  |b n  |2 rdamedia 
338 |a Band  |b nc  |2 rdacarrier 
500 |a Date Completed 15.11.2005 
500 |a Date Revised 21.11.2013 
500 |a published: Print 
500 |a Citation Status MEDLINE 
520 |a Variations in the concentrations and isotopic compositions (delta13C(DIC)) of dissolved inorganic carbon (DIC) reflect contamination and biogeochemical cycling of the carbon in ground water. In order to understand contamination and biogeochemical cycling of DIC, we carried out research on the geochemistry of ground water of Guiyang, the capital city of Guizhou Province, China. Results show that ground water is mainly characterized by SO4.HCO3-Ca.Mg and HCO3-Ca.Mg chemical compositions. The hydrochemical characteristics of these types of water are mainly controlled by lithology of the aquifers. HCO3- is the dominant species of DIC in ground water and has lower concentrations and more negative values of delta13C(DIC) in the high-flow (summer monsoon) season, as compared to the low-flow season. This indicates that DIC is relatively enriched in carbon of biological origin in the high-flow season as compared to the low-flow season and that biological activities are the predominant control on shifts of stable carbon isotope values. The evidence that the delta13C(DIC) values of ground water decrease with increasing concentrations of anthropogenic species shows that the carbon isotopic composition of DIC can be a useful tracer of contamination, in addition to biogeochemical cycling of inorganic carbon in ground water. Results from this study show that ground water is impacted by significant levels of contamination from human activities, especially in the urban areas, as well as the northeast and west suburbs, in Guiyang city, southwest China 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 7 |a Chlorides  |2 NLM 
650 7 |a Nitrates  |2 NLM 
650 7 |a Oxygen Isotopes  |2 NLM 
650 7 |a Sulfates  |2 NLM 
650 7 |a Sodium  |2 NLM 
650 7 |a 9NEZ333N27  |2 NLM 
650 7 |a Magnesium  |2 NLM 
650 7 |a I38ZP9992A  |2 NLM 
650 7 |a Potassium  |2 NLM 
650 7 |a RWP5GA015D  |2 NLM 
650 7 |a Calcium  |2 NLM 
650 7 |a SY7Q814VUP  |2 NLM 
700 1 |a Liu, Cong-Qiang  |e verfasserin  |4 aut 
700 1 |a Tao, Fa-Xiang  |e verfasserin  |4 aut 
700 1 |a Lang, Yun-Chao  |e verfasserin  |4 aut 
700 1 |a Han, Gui-Lin  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Ground water  |d 1979  |g 43(2005), 4 vom: 15. Juli, Seite 494-9  |w (DE-627)NLM098182528  |x 1745-6584  |7 nnas 
773 1 8 |g volume:43  |g year:2005  |g number:4  |g day:15  |g month:07  |g pages:494-9 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 43  |j 2005  |e 4  |b 15  |c 07  |h 494-9