Allocation of carbon to shoots, roots, soil and rhizosphere respiration by barrel medic (Medicago truncatula) before and after defoliation

被引:24
作者
Crawford, MC
Grace, PR
Oades, JM
机构
[1] Univ Adelaide, Dept Soil Sci, Glen Osmond, SA 5064, Australia
[2] CRC Soil & Land Management, Glen Osmond, SA 5064, Australia
关键词
carbon; C-13; C-14; defoliation; partitioning; pasture legumes; roots;
D O I
10.1023/A:1026599229920
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The allocation of carbon to shoots, roots, soil and rhizosphere respiration in barrel medic (Medicago truncatula Gaertn.) before and after defoliation was determined by growing plants in pots in a labelled atmosphere in a growth cabinet. Plants were grown in a (CO2)-C-14-labelled atmosphere for 30 days, defoliated and then grown in a (CO2)-C-13-labelled atmosphere for 19 days. Allocation of C-14-labelled C to shoots, roots, soil and rhizosphere respiration was determined before defoliation and the allocation of C-14 and C-13 was determined for the period after defoliation. Before defoliation, 38.4% of assimilated C was allocated below ground, whereas after defoliation it was 19.9%. Over the entire length of the experiment, the proportion of net assimilated carbon allocated below ground was 30.3%. Of this, 46% was found in the roots, 22% in the soil and 32% was recovered as rhizosphere respiration. There was no net translocation of assimilate from roots to new shoot tissue after defoliation, indicating that all new shoot growth arose from above-ground stores and newly assimilated carbon. The rate of rhizosphere respiration decreased immediately after defoliation, but after 8 days, was at comparable levels to those before defoliation. It was not until 14 days after defoliation that the amount of respiration from newly assimilated C (C-13) exceeded that of C assimilated before defoliation (C-14).
引用
收藏
页码:67 / 75
页数:9
相关论文
共 23 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]  
[Anonymous], 1988, WORLD CROPS COOL SEA, DOI DOI 10.1007/978-94-009-2764-3_68
[3]  
CHENG WX, 1993, SOIL BIOL BIOCHEM, V25, P1189, DOI 10.1016/0038-0717(93)90214-V
[4]   Root production of a barrel medic (Medicago truncatula) pasture, a barley grass (Hordeum leporinum) pasture, and a faba bean (Vicia faba) crop in southern Australia [J].
Crawford, MC ;
Grace, PR ;
Bellotti, WBD ;
Oades, JM .
AUSTRALIAN JOURNAL OF AGRICULTURAL RESEARCH, 1997, 48 (08) :1139-1150
[5]  
CRAWFORD MC, 1997, MANAGEMENT CARBON SE, P381
[6]  
ISBELL RF, 1996, PLANT SOIL, V151, P11
[7]   INPUT OF CARBON TO SOIL FROM WHEAT PLANTS [J].
KEITH, H ;
OADES, JM ;
MARTIN, JK .
SOIL BIOLOGY & BIOCHEMISTRY, 1986, 18 (04) :445-449
[8]   REMOVAL OF ETHYLENE FROM THE ATMOSPHERE OF CONTROLLED ENVIRONMENT CHAMBERS OPERATED WITH FULL AIR RECIRCULATION [J].
MARTIN, JK ;
SINNAEVE, J .
SOIL BIOLOGY & BIOCHEMISTRY, 1987, 19 (05) :651-651
[9]  
MAY L. H., 1958, AUSTRALIAN JOUR AGRIC RES, V9, P767, DOI 10.1071/AR9580767
[10]   CARBON DYNAMICS AND ESTIMATES OF PRIMARY PRODUCTION BY HARVEST, C-14 DILUTION, AND C-14 TURNOVER [J].
MILCHUNAS, DG ;
LAUENROTH, WK .
ECOLOGY, 1992, 73 (02) :593-607