Savanna-derived organic matter remaining in arable soils of the South African Highveld long-term mixed cropping:: Evidence from 13C and 15N natural abundance

被引:48
|
作者
Lobe, I
Bol, R [1 ]
Ludwig, B
Du Preez, CC
Amelung, W
机构
[1] Inst Grassland & Environm Res, Dept Soil Environm & Ecol Sci, N Wyke Res Stn, Okehampton EX20 2SB, Devon, England
[2] Univ Bayreuth, Inst Soil Sci & Soil Geog, D-95440 Bayreuth, Germany
[3] Univ Kassel, Dept Environm Chem, D-37213 Witzenhausen, Germany
[4] Univ Orange Free State, Dept Soil Crop & Climate Sci, ZA-9300 Bloemfontein, South Africa
[5] Univ Bonn, Inst Soil Sci & Soil Ecol, D-53115 Bonn, Germany
来源
SOIL BIOLOGY & BIOCHEMISTRY | 2005年 / 37卷 / 10期
基金
英国生物技术与生命科学研究理事会;
关键词
C-13 and N-15; duration of arable cropping; particle-size fractionation; alternating C3/C4 vegetation; SOM turnover; C model; Roth-C model;
D O I
10.1016/j.soilbio.2005.02.030
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Sustainable agriculture requires the formation of new humus from the crops. We utilized C-13 and N-15 signatures of soil organic matter to assess how rapidly wheat/maize cropping contributed to the humus formation in coarse-textured savanna soils of the South African Highveld. Composite samples were taken from the top 20 cm of soils (Plinthustalfs) cropped for lengths of time varying from 0 to 98 years, after conversion from native grassland savanna (C4). We performed natural 13C and 15N abundance measurements on bulk and particle-size fractions. The bulk soil delta C-13 values steadily decreased from -14.6 in (C4 dominated) grassland to -16.5%o after 90 years of arable cropping. This delta C-13 shift was attributable to increasing replacement of savanna-derived C by wheat crop (C3) C which dominated over maize (C4) inputs. After calculating the annual C input from the crop yields and the output from literature data, by using a stepwise C replacement model, we were able to correct the soil delta C-13 data for the irregular maize inputs for a period of about one century. Within 90 years of cropping 41-89% of the remaining soil organic matter was crop-derived in the three studied agroecosystems. The surface soil C stocks after 90 years of the wheat/maize crop rotation could accurately be described with the Rothamsted Carbon Model, but modelled C inputs to the soil were very low. The coarse sand fraction reflected temporal fluctuations in C-13 of the last C-3 or C-4 cropping and the silt fraction evidenced selective erosion loss of old savanna-derived C. Bulk soil N-15 did not change with increasing cropping length. Decreasing delta N-15 values caused by fertilizer N inputs with prolonged arable cropping were only detected for the coarse sand fraction. This indicated that the present N fertilization was not retained in stable soil C pool. Clearly, conventional cropping practices on the South African highlands neither contribute to the preservation of old savanna C and N, nor the effective humus reformation by the crops. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1898 / 1909
页数:12
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