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The response of soil microbial biomass and activity of a Norway spruce forest to liming and drought
Author(s) -
Lorenz Klaus,
Feger KarlHeinz,
Kandeler Ellen
Publication year - 2001
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/1522-2624(200102)164:1<9::aid-jpln9>3.0.co;2-q
Subject(s) - topsoil , lime , soil water , chemistry , picea abies , spatial variability , biomass (ecology) , soil horizon , agronomy , cambisol , environmental science , experimental forest , soil science , ecology , biology , paleontology , statistics , mathematics
Long‐term effects of liming and short‐term effects of an experimentally induced drought on microbial biomass and activity were investigated in samples from the O‐layer (Of/Oh) and uppermost mineral soil (0—10 cm) in a spruce forest near Schluchsee (Black Forest, South‐West Germany). Seven years after lime application a marked increase of pH values was restricted to the O‐layer. The contents of C and N in the O‐layer of the limed plot appeared to be lower, whereas in the A‐horizon from the limed plot the contents of C and N appeared to be higher than on the control. However, these differences were statistically not significant due to a distinct spatial variability of topsoil conditions. On the limed plots C mic , N mic , and P mic in the O‐layer were lower in comparison to the control whereas differences in the A‐horizon were negligible. In both sampling depths of the limed plot protease activity was higher while N‐mineralization was lower. The other microbial activities studied (basal respiration, catalase activity) followed no consistent pattern after liming. Drought and drought in combination with liming, respectively, had no clear effects on microbial biomass and activity. Only in the A‐horizon of the control, there is some evidence for drought stress for microorganisms. The high variability of results from the drought experiment (roof installation) is likely due to the marked spatial variability of top soil properties as well as imperfect and uneven achievement of experimental drought. Nevertheless, our study indicates that long‐term effects of liming on microorganisms highly depend on site conditions. Thus, liming operations which currently affect vast areas of forest land should be accompanied by monitoring of soil organisms and their activities to reduce the possibility of a loss in functional diversity of soil organisms.