Stoichiometry of the soil microbial biomass in response to amendments with varying C/N/P/S ratios

被引:64
作者
Khan, Khalid Saifullah [1 ,2 ]
Joergensen, Rainer Georg [1 ]
机构
[1] Univ Kassel, Dept Soil Biol & Plant Nutr, Nordbahnhofstr 1a, D-37213 Witzenhausen, Germany
[2] PMAS Arid Agr Univ, Inst Soil Sci, Murree Rd, Rawalpindi 46300, Pakistan
关键词
Microbial biomass; Ergosterol; Nutrient limitation; Stoichiometry; Homeostasis; CARBON-USE EFFICIENCY; FUMIGATION-EXTRACTION METHOD; SUGARCANE FILTER CAKE; ORGANIC-MATTER; BACTERIAL RESIDUES; NUTRIENT AVAILABILITY; S MINERALIZATION; HEAVY-METALS; SULFUR; PHOSPHORUS;
D O I
10.1007/s00374-019-01346-x
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The interacting effects of N, P, and S limitation were investigated by applying four different organic components, i.e., cysteine, chitosan, glucose-6-phosphate, and glucose, to a soil at two different clearly defined N, P, and S levels in a 5-fold range, one with sufficient and one with limited nutrient supply. Initially, MB-CN, MB-CP, and MB-CS ratios were lower after organic substrate amendments with the higher concentration of N, P, and S. The close relationship between the nutrient supply and elemental MB ratios was strongly modified within the next 14days for the MB-CN ratio, probably due to a strong shift in the microbial community composition towards fungi, determined by the ergosterol content of soil. This shift was promoted by high N and low P and S availability, contrasting the view that S is important for the formation of fungal biomass. However, the negative interactions between P limitation and MB-CS ratio suggest that the microbial S metabolism has specific importance under P-limiting conditions. Low substrate CN ratio increased carbon use efficiency (CUE) by 20% in comparison with high substrate CN ratio, calculated at day 5, solely due to an increased formation of microbial residues, as the formation of MBC was not affected by differences in substrate CN ratio. In contrast, high substrate CP and CS ratios reduced MBC formation but did not affect CUE values.
引用
收藏
页码:265 / 274
页数:10
相关论文
共 100 条
[1]  
Allison SD, 2014, FRONT MICROBIOL, V5, DOI [10.3389/fmicb.2014.00571, 10.3389/fmicb.2014.00169]
[2]   QUANTITIES OF PLANT NUTRIENTS IN THE MICROBIAL BIOMASS OF SELECTED SOILS [J].
ANDERSON, JPE ;
DOMSCH, KH .
SOIL SCIENCE, 1980, 130 (04) :211-216
[3]  
[Anonymous], 2014, WORLD SOIL RESOURCES, V103
[4]   The significance of microbial biomass sulphur in soil [J].
Banerjee, MR ;
Chapman, SJ .
BIOLOGY AND FERTILITY OF SOILS, 1996, 22 (1-2) :116-125
[5]   Sulfur forms in organic substrates affecting S mineralization in soil [J].
Blum, Susana Churka ;
Lehmann, Johannes ;
Solomon, Dawit ;
Caires, Eduardo Favero ;
Ferracciu Alleoni, Luis Reynaldo .
GEODERMA, 2013, 200 :156-164
[6]   MEASUREMENT OF MICROBIAL BIOMASS PHOSPHORUS IN SOIL [J].
BROOKES, PC ;
POWLSON, DS ;
JENKINSON, DS .
SOIL BIOLOGY & BIOCHEMISTRY, 1982, 14 (04) :319-329
[7]   CHLOROFORM FUMIGATION AND THE RELEASE OF SOIL-NITROGEN - A RAPID DIRECT EXTRACTION METHOD TO MEASURE MICROBIAL BIOMASS NITROGEN IN SOIL [J].
BROOKES, PC ;
LANDMAN, A ;
PRUDEN, G ;
JENKINSON, DS .
SOIL BIOLOGY & BIOCHEMISTRY, 1985, 17 (06) :837-842
[8]   Elemental contents in vacuolar granules of ectomycorrhizal fungi measured by EELS and EDXS. A comparison of different methods and preparation techniques [J].
Bucking, H ;
Beckmann, S ;
Heyser, W ;
Kottke, I .
MICRON, 1998, 29 (01) :53-61
[9]  
Bunemann EK, 2011, SOIL BIOL, V26, P37, DOI 10.1007/978-3-642-15271-9_2
[10]   Soil enzymes in a changing environment: Current knowledge and future directions [J].
Burns, Richard G. ;
DeForest, Jared L. ;
Marxsen, Juergen ;
Sinsabaugh, Robert L. ;
Stromberger, Mary E. ;
Wallenstein, Matthew D. ;
Weintraub, Michael N. ;
Zoppini, Annamaria .
SOIL BIOLOGY & BIOCHEMISTRY, 2013, 58 :216-234