Soil organic matter dynamics after addition of nitrogen-15-labeled leucaena and dactyladenia residues

被引:52
作者
Vanlauwe, B [1 ]
Sanginga, N
Merckx, R
机构
[1] IITA, Ibadan, Nigeria
[2] Lambourn, Croydon CR9 3EE, England
[3] CIAT, Miami, FL 33102 USA
[4] Fac Appl Agr Sci, Lab Soil Fertil & Soil Biol, B-3001 Louvain, Belgium
关键词
D O I
10.2136/sssaj1998.03615995006200020024x
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Quantification of the movement of residue N through various biologically meaningful soil organic matter (SOM) fractions is essential in low-input tropical cropping systems for the development of management practices aimed at optimizing N-use efficiency. The flow of N derived from N-15-labeled leucaena [Leucaena leucocephala (Lam.) de Wit] and dactyladenia [Dactyladenia barteri (Hook f ex Oliv.) Engl.] leaf residues was followed through the SOM of different particle-size fractions during 858 d, A bioassay study with maize (Zea mays L.) was carried out to assess the availability of residue-derived N (RDN) incorporated in the particle-size fractions. At 53 d after residue application (DAA), most of the RDN was found in the fraction between 0.250 and 2 mm (0250) in the leucaena treatment and in the fraction >2 mm and the surface litter (O2000 + SL) in the dactyladenia treatment. The RDN content of all fractions (0.250 mm was significantly higher in the leucaena than in the dactyladenia treatment up to 471 DAA, The proportion of the total amount of RDN recovered in the fractions <2 mm shifted toward the smaller particle-size classes near the end of the experiment. Highly significant (P < 0.001) relationships between RDN present in the particulate organic matter (POM) and uptake of RDN by maize indicated the relatively high availability of RDN in the POM. Fractionating the SOM pool into different particle-size classes yielded useful information on the relative contributions of the different SOM fractions to N turnover and availability. This information is needed in identifying SOM pools with direct relevance to plant nutrition in low-input cropping systems.
引用
收藏
页码:461 / 466
页数:6
相关论文
共 15 条
[1]   DETERMINATION OF CARBON-C-12 AND CARBON-C-14 IN PLANT AND SOIL [J].
AMATO, M .
SOIL BIOLOGY & BIOCHEMISTRY, 1983, 15 (05) :611-612
[2]   PARTICULATE SOIL ORGANIC-MATTER CHANGES ACROSS A GRASSLAND CULTIVATION SEQUENCE [J].
CAMBARDELLA, CA ;
ELLIOTT, ET .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (03) :777-783
[3]  
Christensen B.T., 1992, Advances in Soil Science, V20, P1, DOI DOI 10.1007/978-1-4612-2930-8_1
[4]   CARBON AND NITROGEN IN PARTICLE-SIZE FRACTIONS-ISOLATED FROM DANISH ARABLE SOILS BY ULTRASONIC DISPERSION AND GRAVITY-SEDIMENTATION [J].
CHRISTENSEN, BT .
ACTA AGRICULTURAE SCANDINAVICA, 1985, 35 (02) :175-187
[5]  
Hassink J., 1995, THESIS WAGENINGEN U
[6]  
Kachaka S., 1993, Soil organic matter dynamics and the sustainability of tropical agriculture: proceedings of an International Symposium, Leuven, Belgium, 4-6 November 1991., P199
[7]  
Lavelle P., 1994, The biological management of tropical soil fertility., P137
[8]  
McMULLEN F., 1966, AUSTRALIAN J EXP AGR ANIM HUSB, V6, P17, DOI 10.1071/EA9660017
[9]  
SAS Institute, 1985, SAS US GUID STAT
[10]  
STEVENSON FJ, 1989, DYNAMICS OF SOIL ORGANIC MATTER IN TROPICAL ECOSYSTEMS, P173