Journal article
Authors list: GAUNT, JL; NEUE, HU; CASSMAN, KG; OLK, DC; ARAH, JRM; WITT, C; OTTOW, JCG; GRANT, IF
Publication year: 1995
Pages: 333-342
Journal: Biology and Fertility of Soils
Volume number: 19
Issue number: 4
ISSN: 0178-2762
eISSN: 1432-0789
DOI Link: https://doi.org/10.1007/BF00336104
Publisher: Springer
Abstract:
A decline in rice yields has been associated with intensification of rice production. In continuously irrigated systems this has been attributed to a decline in soil N supply. Nutrient mineralisation and immobilisation is constrained by the quantity and nature of the organic substrates and the physico-chemical environment of the soil system itself. A flooded soil is very different from an aerobic one; electron acceptors other than oxygen have to be used. The transition to continuously anaerobic conditions associated with the intensification of wetland rice systems affects their organic matter turnover and may adversely affect their productivity.
Citation Styles
Harvard Citation style: GAUNT, J., NEUE, H., CASSMAN, K., OLK, D., ARAH, J., WITT, C., et al. (1995) MICROBIAL BIOMASS AND ORGANIC-MATTER TURNOVER IN WETLAND RICE SOILS, Biology and Fertility of Soils, 19(4), pp. 333-342. https://doi.org/10.1007/BF00336104
APA Citation style: GAUNT, J., NEUE, H., CASSMAN, K., OLK, D., ARAH, J., WITT, C., OTTOW, J., & GRANT, I. (1995). MICROBIAL BIOMASS AND ORGANIC-MATTER TURNOVER IN WETLAND RICE SOILS. Biology and Fertility of Soils. 19(4), 333-342. https://doi.org/10.1007/BF00336104
Keywords
CONTINUOUS FLOODING; HUMIFICATION; INTENSIVE PRODUCTION; ORYZA-SATIVA L; PLANT RESIDUES; YIELD DECLINE