吉林西部盐碱化土壤碳酸盐的碳稳定同位素特征

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The Stable Carbon Isotopic Characteristics of Carbonates in Salini alkani Soil in the West Jilin Province

YANG Jun-peng¹, HU Ke², LIU Yu-ying¹

1.College of Earth Sciences, Jilin University, Changchun 130061,China;2.School of Marine Sciences, China University of Geosciences, Beijing 100083,China

Received:2005-05-25 Revised:1900-01-01 Online:2006-03-26 Published:2006-03-26
Contact: HU Ke

Abstract

Abstract: Through the field investigation of physical properties of the salinialkani soil in West Jilin Province and the stable carbon isotopic analysis of carbonates in salinialkani soil,the results show that the δ¹³C value of the soil carbonates can reflect the developing tendency of the soil saliniation.In the shallow soil with the depth of 0~50 cm below the ground surface,the extent from 0 to 50 centimeters, the change of the δ¹³C of the soil carbonate is positively related with the depth in the upper soil profile from 0~30 cm,but it will increase rapidly in the lower soil profile as the result of the existence of salined and alkali soil layer.

Key words: West Jilin Province, salinialkani soil, soil carbonate, stable carbon isotope

CLC Number:

X142

YANG Jun-peng, HU Ke, LIU Yu-ying. The Stable Carbon Isotopic Characteristics of Carbonates in Salini alkani Soil in the West Jilin Province[J].J4, 2006, 36(02): 245-0249.

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The Stable Carbon Isotopic Characteristics of Carbonates in Salini alkani Soil in the West Jilin Province

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