Is growth of soil microorganisms in boreal forests limited by carbon or nitrogen availability?

被引:126
作者
Ekblad, A [1 ]
Nordgren, A
机构
[1] SLU, Dept Forest Ecol, Sect Soil Sci, SE-90183 Umea, Sweden
[2] Univ Orebro, Dept Nat Sci, S-70182 Orebro, Sweden
关键词
carbon isotopes; C-13; microbial biomass; nitrogen limitation; root respiration; soil respiration;
D O I
10.1023/A:1019698108838
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
To study whether the biomass of soil microorganisms in a boreal Pinus sylvestris-Vaccinium vitis-idaea forest was limited by the availability of carbon or nitrogen, we applied sucrose from sugar cane, a C-4 plant, to the organic mor-layer of the C-3-C dominated soil. We can distinguish between microbial mineralization of the added sucrose and respiration of endogenous carbon (root and microbial) by using the C-4-sucrose as a tracer, exploiting the difference in natural abundance of C-13 between the added C-4-sucrose (delta(13)C -10.8parts per thousand) and the endogenous C-3-carbon (delta(13)C -26.6 parts per thousand). In addition to sucrose, NH4Cl (340 kg N ha(-1)) was added factorially to the mor-layer. We followed the microbial activity for nine days after the treatments, by in situ sampling of CO2 evolved from the soil and mass spectrometric analyses of delta(13)C in the CO2. We found that microbial biomass was limited by the availability of carbon, rather than nitrogen availability, since there was a 50% increase in soil respiration in situ between 1 h and 5 days after adding the sucrose. However, no further increase was observed unless nitrogen was also added. Analyses of the delta(13)C ratios of the evolved CO2 showed that increases in respiration observed between 1 h and 9 days after the additions could be accounted for by an increase in mineralization of the added C-4-C.
引用
收藏
页码:115 / 122
页数:8
相关论文
共 46 条
[1]   THE ROLE OF PROTEINS IN THE NITROGEN NUTRITION OF ECTOMYCORRHIZAL PLANTS .3. PROTEIN-UTILIZATION BY BETULA, PICEA AND PINUS IN MYCORRHIZAL ASSOCIATION WITH HEBELOMA-CRUSTULINIFORME [J].
ABUZINADAH, RA ;
READ, DJ .
NEW PHYTOLOGIST, 1986, 103 (03) :507-514
[2]   PHYSIOLOGICAL METHOD FOR QUANTITATIVE MEASUREMENT OF MICROBIAL BIOMASS IN SOILS [J].
ANDERSON, JPE ;
DOMSCH, KH .
SOIL BIOLOGY & BIOCHEMISTRY, 1978, 10 (03) :215-221
[3]  
[Anonymous], 1991, J ECOL, DOI DOI 10.2307/2260680
[4]   Soil microbial activity in eleven Swedish coniferous forests in relation to site fertility and nitrogen fertilization [J].
Arnebrant, K ;
Baath, E ;
Soderstrom, B ;
Nohrstedt, HO .
SCANDINAVIAN JOURNAL OF FOREST RESEARCH, 1996, 11 (01) :1-6
[5]  
BAATH E, 1981, ZBL BAKT MIK HYG I C, V2, P90
[6]   NITROGEN LEVEL AND DECOMPOSITION IN SCOTS PINE NEEDLE LITTER [J].
BERG, B ;
WESSEN, B ;
EKBOHM, G .
OIKOS, 1982, 38 (03) :291-296
[7]  
BERG B, 1980, IS LITTER DECOMPOSIT
[8]  
BINGHAM IJ, 1993, PHYSIOL PLANTARUM, V88, P149, DOI 10.1111/j.1399-3054.1993.tb01772.x
[9]   PREFERENTIAL USE OF ORGANIC NITROGEN FOR GROWTH BY A NONMYCORRHIZAL ARCTIC SEDGE [J].
CHAPIN, FS ;
MOILANEN, L ;
KIELLAND, K .
NATURE, 1993, 361 (6408) :150-153
[10]  
CHENG WX, 1993, SOIL BIOL BIOCHEM, V25, P1189, DOI 10.1016/0038-0717(93)90214-V