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Influence of salinity and water content on soil microorganisms

Nan YanDepartment of Sediment Research, China Institute of Water Resources and Hydropower Research, Beijing 100048, ChinaPetra MarschnerSchool of Agriculture, Food & Wine, The Waite Research Institute, The University of Adelaide, Adelaide, SA 5005, AustraliaWenhong CaoDepartment of Sediment Research, China Institute of Water Resources and Hydropower Research, Beijing 100048, ChinaChangqing ZuoDepartment of Sediment Research, China Institute of Water Resources and Hydropower Research, Beijing 100048, ChinaWei QinDepartment of Sediment Research, China Institute of Water Resources and Hydropower Research, Beijing 100048, China
2015en
ABI

Аннотация

Salinization is one of the most serious land degradation problems facing world. Salinity results in poor plant growth and low soil microbial activity due to osmotic stress and toxic ions. Soil microorganisms play a pivotal role in soils through mineralization of organic matter into plant available nutrients. Therefore it is important to maintain high microbial activity in soils. Salinity tolerant soil microbes counteract osmotic stress by synthesizing osmolytes which allows them to maintain their cell turgor and metabolism. Osmotic potential is a function of the salt concentration in the soil solution and therefore affected by both salinity (measured as electrical conductivity at a certain water content) and soil water content. Soil salinity and water content vary in time and space. Understanding the effect of changes in salinity and water content on soil microorganisms is important for crop production, sustainable land use and rehabilitation of saline soils. In this review, the effects of soil salinity and water content on microbes are discussed to guide future research into management of saline soils.

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