Fate and recovery of N-15 derived from grass/clover residues when incorporated into a soil and cropped with spring or winter wheat for two succeeding seasons

被引:21
作者
Haynes, RJ [1 ]
机构
[1] CROP & FOOD RES,CHRISTCHURCH,NEW ZEALAND
关键词
grass/clover residues; nitrogen N-15; N mineralization-immobilization; N recovery; particle size fractionation; wheat;
D O I
10.1007/s003740050292
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The fate of N when N-15-labelled perennial ryegrass/white clover residues were incorporated into field lysimeters (rate equivalent to 150 kg N ha(-1)) and two successive crops of winter or spring wheat were grown was investigated. Loss of N-15 over the first winter amounted to 23% and 22% respectively for winter and spring wheat and corresponding losses in the 2nd year were 10% and 14%. Both winter- and spring-sown crops recovered about 10% of residue N-15 in the first season and about 1.5% in the second. The percentage of total crop N uptake originating from residue N-15 was only 14% and 12% respectively for winter and spring wheat in the first season and 2.5% and 1.9% respectively for the second season. The bulk of the N-15 recovered was incorporated into the soil organic matter fraction and at harvest of the 2nd year 55% of added N-15 was present as soil organic N. In order to investigate the nature of this soil organic N-15, soil was fractionated into different particle size separates. Both N-14 and N-15 were concentrated in the medium and fine silt and coarse, and to a lesser extent, medium and fine clay fractions. However, in spring of the first season, N-15 was preferentially present in the floating organic matter and to a lesser extent sand-sized fractions (i.e. as particles of decomposing residue). Between then and harvest of the second season there was a redistribution of N-15 from these fractions and the medium- and fine-sized clay particles toward the coarse and medium silt-sized fractions. This suggested a movement of N-15 toward more aromatic humified material in silt-sized fractions and away from decomposing organic material in sand separates and away from labile organic material in the clay-sized fractions. A laboratory incubation experiment showed that the availability (percentage mineralization) of recently immobilized N-15 was greater than that of native soil N-14.
引用
收藏
页码:130 / 135
页数:6
相关论文
共 27 条
[1]  
Buresh R. J., 1982, Fertilizer Research, V3, P37, DOI 10.1007/BF01063408
[2]  
CASTROUX G, 1987, SOIL SCI SOC AM J, V51, P1200
[3]  
Christensen B.T., 1992, Advances in Soil Science, V20, P1, DOI DOI 10.1007/978-1-4612-2930-8_1
[4]   MINERALIZATION OF N-15-LABELED ORGANIC-COMPOUNDS ADSORBED ON SOIL SIZE FRACTIONS - EFFECT OF SUCCESSIVE WHEAT CROPPING [J].
CORTEZ, J ;
HAMEED, R .
SOIL BIOLOGY & BIOCHEMISTRY, 1992, 24 (02) :113-119
[5]  
FIELDS M, 1968, SOIL BUREAU B, V27
[6]   THE NITROGEN MINERALIZATION RATE OF LEGUME RESIDUES IN SOIL AS INFLUENCED BY THEIR POLYPHENOL, LIGNIN, AND NITROGEN CONTENTS [J].
FOX, RH ;
MYERS, RJK ;
VALLIS, I .
PLANT AND SOIL, 1990, 129 (02) :251-259
[7]  
Franceschi C, 1995, Int Rev Immunol, V12, P1, DOI 10.3109/08830189509056697
[8]   NITROGEN MINERALIZATION, NITRATE LEACHING AND CROP GROWTH FOLLOWING CULTIVATION OF A TEMPORARY LEGUMINOUS PASTURE IN AUTUMN AND WINTER [J].
FRANCIS, GS ;
HAYNES, RJ ;
SPARLING, GP ;
ROSS, DJ ;
WILLIAMS, PH .
FERTILIZER RESEARCH, 1992, 33 (01) :59-70
[9]  
HAYNES GS, 1986, MINERAL NITROGEN PLA, P55
[10]  
Haynes R. J., 1994, Soil biota: management in sustainable farming systems., P172