Drying and rewetting of a loamy sand soil did not increase the turnover of native organic matter, but retarded the decomposition of added 14C-labelled plant material
- 1 April 1999
- journal article
- Published by Elsevier in Soil Biology and Biochemistry
- Vol. 31 (4) , 595-602
- https://doi.org/10.1016/s0038-0717(98)00164-3
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Priming effect of some organic additions to 14C-labelled soilPublished by Elsevier ,2002
- Reduction in microbial activity in Birch litter due to drying and rewetting eventSoil Biology and Biochemistry, 1994
- Modeling the Flush of Nitrogen Mineralization Caused by Drying and Rewetting SoilsSoil Science Society of America Journal, 1993
- Microbial numbers and activity in dried and rewetted arable soil under integrated and conventional managementSoil Biology and Biochemistry, 1992
- Effect of drying and rewetting on mineralization and distribution of bacterial constituents in soil fractionsBiology and Fertility of Soils, 1989
- Aggregate Structure and Carbon, Nitrogen, and Phosphorus in Native and Cultivated SoilsSoil Science Society of America Journal, 1986
- Response of microbial biomass to alternate moist and dry conditions in a soil incubated with 14C- and 15N-labelled plant materialSoil Biology and Biochemistry, 1985
- Simple procedure for the determination of total carbon and its radioactivity in soils and plant materialsThe Analyst, 1979
- Mineralisation of plant nitrogen following alternate wet and dry conditionsPlant and Soil, 1964
- Humus Decomposition in East African SoilsNature, 1956