Effect of substrate quality on the N uptake routes of soil microorganisms in different soil depths

被引:13
作者
Pinggera, Johanna [1 ,2 ]
Geisseler, Daniel [1 ,3 ]
Piepho, Hans-Peter [4 ]
Joergensen, Rainer Georg [2 ]
Ludwig, Bernard [1 ]
机构
[1] Univ Kassel, Dept Environm Chem, D-37213 Witzenhausen, Germany
[2] Univ Kassel, Soil Biol & Plant Nutr, D-37213 Witzenhausen, Germany
[3] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA
[4] Univ Hohenheim, Inst Crop Sci, Biostat Unit, D-70599 Stuttgart, Germany
关键词
Amino acid mineralization; Direct route; MIT route; Gross N mineralization; Protease activity; Soil depth; MICROBIAL BIOMASS; EXTRACTION METHOD; NITROGEN-UTILIZATION; AMINO-ACIDS; MINERALIZATION; CARBON; GROSS; IMMOBILIZATION; ASSIMILATION; RESPIRATION;
D O I
10.1016/j.pedobi.2015.10.002
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A few studies have indicated that substrate quality is an important factor affecting the N uptake route of soil microorganisms, but less is known about the effect of soil depth on the N uptake route under different nutrient conditions. Objectives were to investigate (i) the effects of corn residues with different C to N ratios in the presence and absence of mineral N and (ii) the effects of soil depth on the N uptake route of soil microorganisms. An incubation experiment with surface soils (0-5 cm, C/N = 10) and subsoils (30-40 cm, C/N = 9) from three German loess sites was carried out for 21 days at 20 degrees C and 60% of their water-holding capacity. The following treatments were used: no addition (control), addition of corn residues with a C/N ratio of 20, 40, and 40 + (NH4)(2)SO4. To distinguish between the N uptake routes, the mineralization rate of amino acids was determined using N-15-labeled amino acids. In the control surface soil and subsoil the direct uptake of organic N was favored with no significant (p < 0.05) differences between depths despite significantly higher microbial activity, protease activity, gross N mineralization rate and availability of inorganic N in the surface soil, suggesting that N availability relative to C was similar at both depths. Substrate additions resulted in significantly increased protease activities at both depths after 3-7 days. Addition of corn residue with a high C/N ratio resulted in an increased direct uptake (97% and 94% in the surface soil and subsoil, respectively), compared with addition of corn residue with a low C/N ratio or addition of corn residue and inorganic N (79 to 91% direct uptake). This suggests that the enzyme system involved in the direct uptake was slightly repressed under conditions of sufficient mineralizable N (C/N of 20) or increased concentrations of NH4+. Substrate additions resulted in an initial significantly higher increase in the direct uptake in the surface soil than in the subsoil. (C) 2015 Elsevier GmbH. All rights reserved.
引用
收藏
页码:211 / 218
页数:8
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