The influence of soil processes on carbon isotope distribution and turnover in the British uplands

Author:

Bol R. A.1,Harkness D. D.2,Huang Y.3,Howard D. M.4

Affiliation:

1. Institute of Grassland and Environmental Research, North Wyke, Okehampton, Devon EX20 2SB,

2. NERC Radiocarbon Laboratory, Scottish Enterprise Technology Park, East Kilbride G75 0QF,

3. Environmental and Analytical Section, School of Chemistry, University of Bristol, Bristol BS8 1RJ, and

4. Institute of Terrestrial Ecology, Merlewood Research Station, Grange‐over‐Sands LA11 6JU, Cumbria, UK

Publisher

Wiley

Subject

Soil Science

Reference27 articles.

1. Anderson J.M.1992Responses of soils to climate change. In:Advances in Ecological Research 22 163210.

2. Nutrient Cycling in Terrestrial Ecosystems: Field Methods Application and Interpretation 1990 Elsevier Applied Science F. Andreux C. Cerri P.B. Vose V.A. Vitorello A.F. Harrison P. Ineson O.W. Heal Potential of stable isotope 15 N and 13 C methods for determining input and turnover in soils 259 275

3. Mass Spectrometry of Soils 1996 Marcel Dekker J. Balesdent A. Mariotti T.W. Boutton S.I. Yamasaki Measurement of soil organic matter turnover using 13 C natural abundance 83 111

4. A Review of Soil Factors and Processes That Control Fluxes of Heat Moisture and Greenhouse Gases 1992 Technical Paper No 23 N.H. Batjes N.H. Batjes E.M. Bridges Organic matter and carbon dioxide 97 148

5. Thin layer δ13C and D14C monitoring of ‘lessive’ soil profiles.;Becker‐Heidmann P.;Radiocarbon,1986

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