Carbon and nitrogen mineralization of added particulate and macroorganic matter

被引:47
作者
YAkovchenko, VP [1 ]
Sikora, LJ [1 ]
Millner, PD [1 ]
机构
[1] ARS, Soil Microbial Syst Lab, USDA, Beltsville Agr Res Ctr, Beltsville, MD 20705 USA
关键词
D O I
10.1016/S0038-0717(98)00096-0
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Particulate organic matter (POM) is more sensitive than total SOM to changes in management practices and, accordingly, may indicate changes in soil quality. A soil incubation study was conducted to determine the effects of added POM (75 to 250 mu m size fraction), or macroorganic matter (MOM, 250 to 2000 mu m size fraction) on C and N mineralization and microbial and C and N content. A 1 kg composite made from 16 predominantly silt loam soils was amended with 10 g of POM, MOM or MOM ground to a reduced size of 75 to 250 mu m (GMOM). The MOM amendment equaled 4.55-fold and POM equaled 1.60-fold of total MOM and POM found in the composite soil. Carbon mineralization of MOM and POM after 8 weeks was approximately 9 and 4%, respectively of the total MOM and POM-C added. Reducing the size of MOM to 75 to 250 mu m did not affect mineralization. Nitrogen mineralization was slightly greater in the amended soils after 8 weeks and equaled 5 to 6% of the MOM or POM-total N added. Contribution of POM to total mineralized N from soil organic matter (SOM) in the composite soil was proportional to the POM content in SOM or approximately 12%. Amended soils had 25 to 42% more biomass-C than the control soil 2 weeks after amendment application. After 8 weeks, the amended soils contained about 32% more biomass-C. This increase in biomass-C at 8 weeks accounted for approximately 2% of the added C. At 8 weeks, microbial biomass-N in GMOM-, MOM- and POM-amended soils was about 56, 46 and 14% higher, respectively, than in the control soil. These increases were approximately 8% of the MOM-N added and 2% of the POM-N added. Increases in POM resulted in increases in soil respiration and microbial biomass-C and N, which also are suggested indicators of soil quality. Therefore, POM may be a suitable soil quality indicator that provides similar information as soil respiration or microbial biomass determinations. (C) 1998 Published by Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:2139 / 2146
页数:8
相关论文
共 45 条
[31]  
Ladd J. N., 1983, Soils: an Australian viewpoint., P589
[32]   MICROBIAL BIOMASS FORMED FROM C-14, N-15-LABELED PLANT-MATERIAL DECOMPOSING IN SOILS IN THE FIELD [J].
LADD, JN ;
OADES, JM ;
AMATO, M .
SOIL BIOLOGY & BIOCHEMISTRY, 1981, 13 (02) :119-126
[33]   Spatial variability of early season nitrogen availability indicators in corn [J].
Lengnick, LL .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1997, 28 (19-20) :1721-1736
[34]  
MONAGHAN R, 1993, SOIL BIOL BIOCHEM, V12, P1623
[35]   FIELD INCORPORATION OF STRAW AND ITS EFFECTS ON SOIL MICROBIAL BIOMASS AND SOIL INORGANIC-N [J].
OCIO, JA ;
BROOKES, PC ;
JENKINSON, DS .
SOIL BIOLOGY & BIOCHEMISTRY, 1991, 23 (02) :171-176
[36]  
SHAYMUKHAMETOV MS, 1984, SOV SOIL SCI+, V16, P117
[37]  
Sikora L.J., 1996, Soil Org. Matter Anal. Interpret, V46, P41, DOI DOI 10.2136/SSSASPECPUB46.C5
[38]   Soil organic matter mineralization after compost amendment [J].
Sikora, LJ ;
Yakovchenko, V .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1996, 60 (05) :1401-1404
[39]  
Skjemstad J. O., 1988, Advances in nitrogen cycling in agricultural ecosystems, P134
[40]   NET NITROGEN MINERALIZATION FROM LIGHT-FRACTION AND HEAVY-FRACTION FOREST SOIL ORGANIC-MATTER [J].
SOLLINS, P ;
SPYCHER, G ;
GLASSMAN, CA .
SOIL BIOLOGY & BIOCHEMISTRY, 1984, 16 (01) :31-37