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• W2056375134 startingPage "478" @default.
• W2056375134 abstract "Climate models predict an increase in global surface temperature and a change in precipitation intensity during this century. For Europe, extended drought periods followed by heavy rainfall are expected. The consequences for soil organic matter (SOM) dynamics are poorly understood. In this study, we investigated the effect of changing soil moisture regime on SOM quality under field conditions. For this purpose, a throughfall exclusion (TE) experiment was conducted in the summers 2006 and 2007 on a Haplic Podzol under a 140 years old Norway spruce stand using a roof installation followed by re-wetting compared to non-manipulated control plots. Total organic carbon, lignin (stable carbon pool), plant and microbial sugars (labile carbon pool) and microbial biomass (phospholipid fatty acids) were determined before, during and after the experiment in the L, O, A and B horizons. No significant treatment effects could be observed for SOM quantity. Amounts of lignin and soil microbial biomass were also not affected by the moisture regime but structure of soil microbial community. In the L and organic layers, gram + bacteria and actinomycetes were reduced during water stress, while gram- bacteria, fungi and protozoa increased during drought. Warmer and drier weather led to a dominance of fungi while a cooler and moister regime favoured bacteria, at least in the L horizon. An increasing PLFA (cy17:0 + cy19:0)/(16:1ω7c + 18:1ω7c) ratio in the O layer and A horizon suggests that the microbes suffered from water stress in these horizons. This agrees with a decreasing contribution of microbial sugars to SOM with decreasing water content in the O and A horizons. Although the original plant material exhibited increasing plant sugar content with increasing dryness, the contribution of the plant sugars to total soil organic carbon (SOC) generally decreased with decreasing water content. Physical-chemical changes of soil structure can theoretically change the sugar extractability from soils and/or chemical changes of sugars structure can probably affect the analysis. Therefore, chemical alteration and stabilization could be responsible for sugar decrease in soil with increasing dryness explaining the contrast compared to the original plant material." @default.
• W2056375134 created "2016-06-24" @default.
• W2056375134 creator A5027366737 @default.
• W2056375134 creator A5071652778 @default.
• W2056375134 date "2011-03-01" @default.
• W2056375134 modified "2023-10-18" @default.
• W2056375134 title "Organic matter dynamics in a temperate forest soil following enhanced drying" @default.
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• W2056375134 cites W1963792977 @default.
• W2056375134 cites W1964994969 @default.
• W2056375134 cites W1967051022 @default.
• W2056375134 cites W1973975357 @default.
• W2056375134 cites W1974501714 @default.
• W2056375134 cites W1976753904 @default.
• W2056375134 cites W1978684995 @default.
• W2056375134 cites W1979967464 @default.
• W2056375134 cites W1980849219 @default.
• W2056375134 cites W1982653203 @default.
• W2056375134 cites W1984178651 @default.
• W2056375134 cites W1990964750 @default.
• W2056375134 cites W1991432734 @default.
• W2056375134 cites W1992300099 @default.
• W2056375134 cites W1992389052 @default.
• W2056375134 cites W1994108458 @default.
• W2056375134 cites W1996106763 @default.
• W2056375134 cites W1996738342 @default.
• W2056375134 cites W1997294324 @default.
• W2056375134 cites W2002685708 @default.
• W2056375134 cites W2012361838 @default.
• W2056375134 cites W2014456287 @default.
• W2056375134 cites W2018250157 @default.
• W2056375134 cites W2020590731 @default.
• W2056375134 cites W2029754901 @default.
• W2056375134 cites W2032093200 @default.
• W2056375134 cites W2032236397 @default.
• W2056375134 cites W2033936588 @default.
• W2056375134 cites W2037238318 @default.
• W2056375134 cites W2037478874 @default.
• W2056375134 cites W2037865793 @default.
• W2056375134 cites W2038926247 @default.
• W2056375134 cites W2041671416 @default.
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• W2056375134 cites W2051463327 @default.
• W2056375134 cites W2051643809 @default.
• W2056375134 cites W2054105701 @default.
• W2056375134 cites W2056926674 @default.
• W2056375134 cites W2057613840 @default.
• W2056375134 cites W2059075856 @default.
• W2056375134 cites W2060552225 @default.
• W2056375134 cites W2064331123 @default.
• W2056375134 cites W2064998766 @default.
• W2056375134 cites W2067412004 @default.
• W2056375134 cites W2069269466 @default.
• W2056375134 cites W2075882525 @default.
• W2056375134 cites W2077328275 @default.
• W2056375134 cites W2077437103 @default.
• W2056375134 cites W2080097142 @default.
• W2056375134 cites W2082807376 @default.
• W2056375134 cites W2083578873 @default.
• W2056375134 cites W2087456348 @default.
• W2056375134 cites W2089126796 @default.
• W2056375134 cites W2090791530 @default.
• W2056375134 cites W2090963808 @default.
• W2056375134 cites W2094098259 @default.
• W2056375134 cites W2094757334 @default.
• W2056375134 cites W2095589143 @default.
• W2056375134 cites W2097279262 @default.
• W2056375134 cites W2098320958 @default.
• W2056375134 cites W2098332042 @default.
• W2056375134 cites W2100442254 @default.
• W2056375134 cites W2120124544 @default.
• W2056375134 cites W2124620822 @default.
• W2056375134 cites W2130057128 @default.
• W2056375134 cites W2130725690 @default.
• W2056375134 cites W2131873925 @default.
• W2056375134 cites W2133904157 @default.
• W2056375134 cites W2137018917 @default.
• W2056375134 cites W2140335015 @default.
• W2056375134 cites W2157110683 @default.
• W2056375134 cites W2163462941 @default.
• W2056375134 cites W2165669094 @default.
• W2056375134 cites W4238787840 @default.
• W2056375134 cites W4251264506 @default.
• W2056375134 doi "https://doi.org/10.1016/j.soilbio.2010.09.037" @default.
• W2056375134 hasPublicationYear "2011" @default.
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