Patterns of SOC and soil 13C and their relations to climatic factors and soil characteristics on the Qinghai–Tibetan Plateau

Author:

Wang Shaoqiang,Fan Jiangwen,Song Minghua,Yu Guirui,Zhou Lei,Liu Jiyuan,Zhong Huaping,Gao Lupeng,Hu Zhongmin,Wu Weixing,Song Ting

Publisher

Springer Science and Business Media LLC

Subject

Plant Science,Soil Science

Reference61 articles.

1. Accoe F, Beockx P, Van Cleemput O, Hofman G, Hui X, Bin H, Guanxion C (2002) Characterization of soil organic matter fractions from grassland and cultivated soils via C content and 13δC signature. Rapid Commun Mass Spectrom 16:2157–2164

2. Andreux F, Cerri C, Vose PB, Vitorello VA (1990) Potential of stable isotope, 15N and 13C methods for determining input and turnover in soils. In: Harrison AF (ed) Nutrient cycling in terrestrial ecosystems, field methods, application and interpretation. Elsevier Applied Science, London, pp 259–275

3. Balesdent J, Mariotti A (1988) Measurement of soil organic matter turnover using 13C natural abundance. In: Boutton TW, Yama-saki S (eds) Mass spectrometry of soil. Marcel Dekker, New York, pp 83–111

4. Barrios E, Buresh RJ, Sprent JI (1996) Organic matter in soil particle size and density fractions from maize and legume cropping systems. Soil Biol Biochem 28:185–193

5. Bernoux M, Cerri CC, Neill C, de Moraes JFL (1998) The use of stable carbon isotopes for estimating soil organic matter turnover rates. Geoderma 82:43–58

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