The effects of tillage displaced soil on soil properties and wheat biomass

Citation
C. Kosmas et al., The effects of tillage displaced soil on soil properties and wheat biomass, SOIL TILL R, 58(1-2), 2001, pp. 31-44
Citations number
34
Categorie Soggetti
Agriculture/Agronomy
Journal title
SOIL & TILLAGE RESEARCH
ISSN journal
01671987 → ACNP
Volume
58
Issue
1-2
Year of publication
2001
Pages
31 - 44
Database
ISI
SICI code
0167-1987(200102)58:1-2<31:TEOTDS>2.0.ZU;2-F
Abstract
Tillage operations transport large amounts of soil from convex slopes and d eposit on concavities in hilly cultivated areas. Field experiment was condu cted to assess tillage induced soil displacement and its effects on soil pr operties and wheat (Triticum aestivum L.) biomass production. The study was done on 3.5 ha fertilized and wheat seeded hillslope (14-21% slope) locate d 100 km north of Athens. Greece. Numbered aluminum cylinders (700), each 1 0 mm diameter by 10 mm height. were buried in soil as soil movement tracers (SMTs) to estimate soil displacement as a function of moldboard plowing wi th two depths in up-slope and down-slope directions. Furthermore. clay, org anic matter, rock fragment content, phosphorus and Cs-137 were determined o n 81 soil bulk cores to estimate soil redistribution rates along the study hillslope. Soil depth and soil water storage were measured in 81 soil sites and related to the wheat biomass production. The mean SMT displacement distance due to 25-cm plow depth on 21% slope was 42 cm for down-slope tillage and 16 cm for up-slope tillage. Comparable va lues were 31 cm for down-slope and 14 cm for up-slope tillage on 14% slope gradient. The SMT distance for both tillage directions on 21% slope was abo ut 60% less for 18-cm plow depth compared with 25-cm plow depth. Shallow so il (depth <25 cm) was observed on convex slope with greater percentages of sand, rock fragments, organic matter and lower percentages of clay and avai lable water. In contrast, deeper soil (depth >70 cm) was found on lower con cavities where displaced soil was deposited. The spatial pattern of Cs-137 inventories suggests that tillage erosion is a major erosion process in the study area. The maximum leaf area index of wheat was 2.8 for convex slope and 3.6 for concave slope. Wheat biomass, ranging from 0.2 to 1.2 kg m(2), increased logarithmically with increased soil depth. Moldboard plowing disp laced large amounts of soil from convex slope which changed soil properties to less favorable fur wheat production. Application of the obtained empiri cal functions showed that under the existing climatic conditions and manage ment practices, the unprofitably productive area will increase from 4.1 to 6.8% in a period of 7 years. (C) 2001 Elsevier Science B.V. All rights rese rved.