Estimating belowground nitrogen inputs of pea and canola and their contribution to soil inorganic N pools using 15N labeling

被引:30
作者
Arcand, Melissa M. [1 ]
Knight, J. Diane [1 ]
Farrell, Richard E. [1 ]
机构
[1] Univ Saskatchewan, Dept Soil Sci, Saskatoon, SK S7N 5A8, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Crop residues; Rhizodeposition; Roots; N-15 isotope techniques; DYNAMIC CROPPING SYSTEMS; WINTER OILSEED RAPE; RHIZODEPOSITION; ROOT; CROPS; MINERALIZATION; RHIZOSPHERE; TISSUES; OATS; IMMOBILIZATION;
D O I
10.1007/s11104-013-1626-z
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Crop species grown in a diversified crop rotation can influence soil N dynamics to varying degrees due to differences in the quantity and quality of the residues returned to the soil. The aim of this study was to quantify the contribution of N rhizodeposition by canola (Brassica napus L.) and pea (Pisum sativum L.) to the crop residue N balance and soil inorganic N pool. Canola and pea were grown in a soil-sand mixture and were subject to cotton-wick N-15 labeling in a greenhouse experiment. Nitrogen-15 recovered in the soil and roots were used to estimate N rhizodeposition. Belowground N, including root N and N rhizodeposits, comprised 70 % and 61 % of total crop residue N for canola and pea, respectively. Canola released the greatest amount of total root-derived N to the soil, which was related to greater root biomass production by canola. However, root-derived N in the soil inorganic N pool was greater under pea (13 %) than canola (4 %). Our results show a significant belowground N contribution to total crop residue from pea and canola. Further investigation is required to determine whether input of the more labile N rhizodeposits of pea improves soil N supply to succeeding crops or increases the potential for N loss from the soil system relative to canola.
引用
收藏
页码:67 / 80
页数:14
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