Maize plant contributions to root zone available carbon and microbial transformations of nitrogen

被引:120
作者
Qian, JH
Doran, JW
Walters, DT
机构
[1] UNIV NEBRASKA,USDA ARS,LINCOLN,NE 68583
[2] UNIV NEBRASKA,DEPT AGRON,LINCOLN,NE 68583
[3] UNIV CALIF BERKELEY,DEPT PLANT & MICROBIAL BIOL,BERKELEY,CA 94720
关键词
D O I
10.1016/S0038-0717(97)00043-6
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Root-derived C influences soil microbial activities that regulate N transformations and cycling in soil. The change in C-13 abundance of soil microbial biomass was used to quantify contributions from maize (Zea mays L.), a C-4 plant, to root zone-available C during growth in soil with a long history of C-3 vegetation. Effects of root-derived available C on microbial transformations of N were also evaluated using a (NH)-N-15:5NO(3) fertilizer, tracer. Root-released C (microbial respired C-4-C + soil residue C-4-C) accounted for 12% (210 kg C ha(-1)) of measured C fixed by, maize at 4 wk and 5% at maturity when root-released C totaled 1135 kg C ha(-1). Of the C-4-C remaining in soil, only 18-23% was found in microbial biomass, indicating either a rapid turnover rate of biomass or a lower availability of C-4 substrates. Average daily production of root-derived available C was greatest during 4-8 wk maize growth (7 kg C ha(-1) d(-1)) when 4-11% of the soil microbial biomass came from this C source. At maize maturity, 15% of the microbial biomass (161 kg C ha(-1)) came from root-derived available C, which totaled 402 kg ha(-1). Of the N-15 remaining in bare and cropped soils, averages of 23 and 16% (IO and 2 kg N ha(-1)) were found in microbial biomass, and 64 and 2% (28 and 0.2 kg N ha(-1)) were in inorganic N-15 form, leaving 13 and 82% (6 and 10 kg N ha(-1)) as non-biomass organic N, respectively; this suggests that N cycling through microbial biomass was enhanced by root-derived C. Denitrification and N2O losses from planted soils were low (1-136 g N ha(-1) d(-1)) when soil water-filled pore space (WFPS) was (50%, but increased to 0.02-3.4 kg N ha(-1) d(-1) when soils were wetted to 85-95% WFPS when N-2 comprised 70-99% of denitrification products. The maximum denitrification rate was 1.5 times greater, and the cumulative denitrification losses 77% greater during early growth stages in planted soil as compared to bare soil when adequate NO3--N (> 2-3 mg kg(-1)) present in the soil. The presence of maize plants increased denitrification losses from soil by 19 to 57% (average of 29%) during early growth stages when the release of root-derived C was greatest. Published by Elsevier Science Ltd.
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页码:1451 / 1462
页数:12
相关论文
共 46 条
[1]  
*AB CONC, 1989, SUPERANOVA
[2]   FIELD-EVALUATION OF 4 METHODS FOR MEASURING DENITRIFICATION [J].
AULAKH, MS ;
DORAN, JW ;
MOSIER, AR .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1991, 55 (05) :1332-1338
[3]   RELEASE OF ORGANIC-SUBSTANCES BY CEREAL ROOTS INTO SOIL [J].
BARBER, DA ;
MARTIN, JK .
NEW PHYTOLOGIST, 1976, 76 (01) :69-80
[4]   CARBON AND NITROGEN LOSSES THROUGH ROOT EXUDATION BY AGROPYRON-CRISTATUM, AGROPYRON-SMITHII AND BOUTELOUA-GRACILIS [J].
BIONDINI, M ;
KLEIN, DA ;
REDENTE, EF .
SOIL BIOLOGY & BIOCHEMISTRY, 1988, 20 (04) :477-482
[5]   NITROUS-OXIDE EMISSIONS IN IRRIGATED CORN AS AFFECTED BY NITRIFICATION INHIBITORS [J].
BRONSON, KF ;
MOSIER, AR ;
BISHNOI, SR .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1992, 56 (01) :161-165
[6]   DIFFUSION METHOD TO PREPARE SOIL EXTRACTS FOR AUTOMATED N-15 ANALYSIS [J].
BROOKS, PD ;
STARK, JM ;
MCINTEER, BB ;
PRESTON, T .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (06) :1707-1711
[7]   RELATIONSHIPS BETWEEN DENITRIFICATION CAPACITIES OF SOILS AND TOTAL, WATER-SOLUBLE AND READILY DECOMPOSABLE SOIL ORGANIC-MATTER [J].
BURFORD, JR ;
BREMNER, JM .
SOIL BIOLOGY & BIOCHEMISTRY, 1975, 7 (06) :389-394
[8]   CARBON PARTITIONING AND RHIZODEPOSITION IN CORN AND BROMEGRASS [J].
DAVENPORT, JR ;
THOMAS, RL .
CANADIAN JOURNAL OF SOIL SCIENCE, 1988, 68 (04) :693-701
[9]  
ECKERT DJ, 1988, N CENTRAL REGIONAL P, V221, P6
[10]  
HAILER T, 1985, PLANT SOIL, V86, P207