C1 - Edited contributions to conferences/learned societies
Jenkinson, D. 1963. The turnover of organic matter in soil. Report of the FAO/IAEA Technical Meeting Organized by the Food and Agriculture Organization of the United Nations and the International Atomic Energy Agency in cooperation with the International Soil Society Brunswick-Volkenrode, 9-14 September, 1963. Volkenrode 09 Sep 1963 Pergamon Press.
There is little quantitative data on the turnover of soil organic matter even for parts of the world where long-term field experiments have been carried out. Comparisons of turnover under different climatic conditions, under different systems of agriculture, under different plant associations, at different pH's, in soils differing mechanical composition would be of pedological and agricultural interest. Although many turnover problems, particularly gross turnover ones can (and should) be studied by non-isotopic methods, isotopes used in conjunction with long term field experiments are potentially capable of giving quantitative information obtainable in no other way. Isotopes are particular useful under steady state conditions, and experiments under steady state conditions have the additional advantage that many sampling problems, uncertainties about constancy of plant return etc., are avoided. Long term field experiments on turnover are practicable, and should be set up in different parts of the world.
|Keywords||Long term experiments|
|Year of Publication||1963|
|Open access||Published as non-open access|
|Journal citation||pp. 187-208|
|09 Sep 1963|
Permalink - https://repository.rothamsted.ac.uk/item/96z5q/the-turnover-of-organic-matter-in-soil