Publication Details

Category Text Publication
Reference Category Journals
DOI 10.1016/j.soilbio.2005.02.030
Title (Primary) Savanna-derived organic matter remaining in arable soils of the South African Highveld long-term mixed cropping: Evidence from 13C and 15N natural abundance
Author Lobe, I.; Bol, R.; Ludwig, B.; Du Preez, C.C.; Amelung, W.
Source Titel Soil Biology & Biochemistry
Year 2005
Department FLOEK
Volume 37
Issue 10
Page From 1898
Page To 1909
Language englisch
Abstract

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(13)C values steadily decreased from -14.6 in (C4 dominated) grassland to -16.5%o after 90 years of arable cropping. This delta(13)C 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(13)C 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(15)N 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.
Persistent UFZ Identifier https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=3583
Lobe, I., Bol, R., Ludwig, B., Du Preez, C.C., Amelung, W. (2005):
Savanna-derived organic matter remaining in arable soils of the South African Highveld long-term mixed cropping: Evidence from 13C and 15N natural abundance
Soil Biol. Biochem. 37 (10), 1898 - 1909 10.1016/j.soilbio.2005.02.030