Community food web, decomposition and nitrogen mineralisation in a stratified Scots pine forest soil

被引:92
作者
Berg, M
de Ruiter, P
Didden, W
Janssen, M
Schouten, T
Verhoef, H
机构
[1] Free Univ Amsterdam, Dept Anim Ecol, Inst Ecol Sci, NL-1081 HV Amsterdam, Netherlands
[2] Natl Inst Publ Hlth & Environm Protect, Lab Soil & Ground Water Res, NL-3720 BA Bilthoven, Netherlands
[3] Natl Inst Publ Hlth & Environm Protect, Radiat Res Lab, NL-3720 BA Bilthoven, Netherlands
[4] Univ Utrecht, Dept Environm Sci, NL-3508 TC Utrecht, Netherlands
[5] Univ Agr, Subdept Soil Qual, NL-6700 EC Wageningen, Netherlands
关键词
D O I
10.1034/j.1600-0706.2001.09121.x
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A soil community food web model was used to improve the understanding of what factors govern the mineralisation of nutrients and carbon and the decay of dead organic matter. The model derives the rates of C and N mineralisation by organisms by splitting their uptake rate of food resources into a rate at which faeces or prey remains are added to detritus. a rate at which elements are incorporated into biomass, and a rate at which elements are released by organisms as inorganic compounds. The functioning of soil organisms in the mineralisation of C and N was modelled in the soil horizon of a Scots pine forest. The organic horizon was divided into three distinct layers, representing successive stages of decay, i.e. litter, fragmented litter. and humus. Each of the layers had a different. quantitative, biota composition. For each laver the annual C and N mineralisation rates were simulated and compared to observed C and N mineralisation rates from organic matter in stratified litterbags. Simulated C and N mineralisation was relatively close to measured losses of C and N, but the fit was not perfect. Discrepancies between the observed and predicted mineralisation rates are discussed in terms of variation in model parameter values of those organisms that showed the highest contribution to mineralisation rates. The measured, and by the model predicted, significant decrease in mineralisation rates down the profile was not explained by the biomass of the primary decomposers and only partly by the total food web biomass. Modelling results indicated that indirect effects of soil fauna. due to trophic interactions with their resources, are an important explanatory factor. In addition, the analyses suggest that community food web structure is an important factor in the regulation of nutrient mineralisation. The model provided the means to evaluate the contribution of functionally defined groups of organisms, structured in a detrital food web. to losses of C and N from successive decay stages.
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收藏
页码:130 / 142
页数:13
相关论文
共 48 条
[1]   PHYSICAL FACTORS INFLUENCING DECOMPOSITION OF ORGANIC MATERIALS IN SOIL AGGREGATES [J].
ADU, JK ;
OADES, JM .
SOIL BIOLOGY & BIOCHEMISTRY, 1978, 10 (02) :109-115
[2]   MICROBIAL AND FAUNAL INTERACTIONS AND EFFECTS ON LITTER NITROGEN AND DECOMPOSITION IN AGROECOSYSTEMS [J].
BEARE, MH ;
PARMELEE, RW ;
HENDRIX, PF ;
CHENG, WX ;
COLEMAN, DC ;
CROSSLEY, DA .
ECOLOGICAL MONOGRAPHS, 1992, 62 (04) :569-591
[3]   THE EFFECT OF LIGNIN AND NITROGEN ON THE DECOMPOSITION OF LITTER IN NUTRIENT-POOR ECOSYSTEMS - A THEORETICAL APPROACH [J].
BERENDSE, F ;
BERG, B ;
BOSATTA, E .
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE, 1987, 65 (06) :1116-1120
[4]   Dynamics and stratification of functional groups of micro- and mesoarthropods in the organic layer of a Scots pine forest [J].
Berg, MP ;
Kniese, JP ;
Bedaux, JJM ;
Verhoef, HA .
BIOLOGY AND FERTILITY OF SOILS, 1998, 26 (04) :268-284
[5]   Dynamics and stratification of bacteria and fungi in the organic layers of a Scots pine forest soil [J].
Berg, MP ;
Kniese, JP ;
Verhoef, HA .
BIOLOGY AND FERTILITY OF SOILS, 1998, 26 (04) :313-322
[6]   Long-term decomposition of successive organic strata in a nitrogen saturated Scots pine forest soil [J].
Berg, MP ;
Kniese, JP ;
Zoomer, R ;
Verhoef, HA .
FOREST ECOLOGY AND MANAGEMENT, 1998, 107 (1-3) :159-172
[7]   Ecological characteristics of a nitrogen-saturated coniferous forest in the Netherlands [J].
Berg, MP ;
Verhoef, HA .
BIOLOGY AND FERTILITY OF SOILS, 1998, 26 (04) :258-267
[8]   DYNAMICS OF CARBON AND NITROGEN IN THE ORGANIC-MATTER OF THE SOIL - A GENERIC THEORY [J].
BOSATTA, E ;
AGREN, GI .
AMERICAN NATURALIST, 1991, 138 (01) :227-245
[9]   BIOLOGICAL STRATEGIES OF NUTRIENT CYCLING IN SOIL SYSTEMS [J].
COLEMAN, DC ;
REID, CPP ;
COLE, CV .
ADVANCES IN ECOLOGICAL RESEARCH, 1983, 13 :1-55
[10]   CALCULATION OF NITROGEN MINERALIZATION IN SOIL FOOD WEBS [J].
DERUITER, PC ;
VANVEEN, JA ;
MOORE, JC ;
BRUSSAARD, L ;
HUNT, HW .
PLANT AND SOIL, 1993, 157 (02) :263-273