Effect of tillage and residue management of maize and wheat yield and on physical properties of an irrigated sandy loam soil in Northern Nigeria

1986 ◽  
Vol 8 ◽  
pp. 161-170 ◽  
Author(s):  
P.R. Maurya
Keyword(s):  
Physical Properties ◽  
Sandy Loam ◽  
Wheat Yield ◽  
Sandy Loam Soil ◽  
Residue Management ◽  
Northern Nigeria ◽  
Loam Soil

Surface physical properties of a sandy loam soil under different tillage practices

Soil Research ◽  
1988 ◽  
Vol 26 (3) ◽  
pp. 549 ◽  
Author(s):  
KY Chan ◽  
JA Mead
Keyword(s):  
Organic Carbon ◽  
Physical Properties ◽  
Sandy Loam ◽  
Sandy Loam Soil ◽  
Organic Carbon Content ◽  
Moisture Profile ◽  
Tillage Practices ◽  
Pasture Soil ◽  
Cultivated Soil ◽  
Loam Soil

The infiltration behaviour and physical properties of a hardsetting sandy loam soil at Cowra, N.S.W., following 2 years of different tillage treatments are reported. Soil that had not been cultivated for 25 years was also investigated at an adjacent pasture site. Infiltration of simulated rainfall at the end of the wheat-growing season gave moisture profiles that were quite different for cultivated, direct drilled and pasture soils. The moisture profile for the cultivated soil suggested the presence of an impeded layer which retarded the movement of infiltrated rain to the subsoil. Porosity measurements confirmed the presence of a layer with significantly fewer macropores (> 300 �m diameter) at the 50-100 mm depth in the cultivated soil, when compared with the direct drilled soil. The old pasture soil had significantly higher porosity (> 300 �m diameter) in the top 100 mm. Aggregate stabilities and organic carbon contents were measured in narrow increments to 150 mm depth for the three different soils, and revealed that a surface 25 mm layer of high organic carbon and highly stable macro-aggregates was present in the pasture and direct drilled soils but absent in the cultivated soil. The unstable surface layer in the conventionally cultivated soil was a consequence of the mixing and inverting action of cultivation and was not due to a net loss of organic carbon from the profile. The organic carbon content of the pasture soil was not significantly different from the direct drilled soil below 50 mm; however, it was significantly lower than the conventionally cultivated soil between 50 and 150 mm depth. These results indicate a need to adopt tillage practices that can preserve the top 25 mm layer of such fragile soils.

Impact of Tillage and Residue Management on Water and Thermal Regimes of a Sandy Loam Soil under Pigeonpea-Wheat Cropping System

2018 ◽  
Vol 66 (1) ◽  
pp. 40 ◽  
Author(s):  
Surajit Mondal ◽  
Anupam Das ◽  
Sanatan Pradhan ◽  
R.K. Tomar ◽  
U.K. Behera ◽  
...  
Keyword(s):  
Sandy Loam ◽  
Cropping System ◽  
Sandy Loam Soil ◽  
Residue Management ◽  
Thermal Regimes ◽  
Loam Soil

Carbon availability limits the denitrification potential of sandy loam soil from corn agroecosystems with long-term tillage and residue management

2020 ◽  
pp. 1-5 ◽  
Author(s):  
Leanne Ejack ◽  
Joann K. Whalen ◽  
Chandra A. Madramootoo
Keyword(s):  
Crop Residues ◽  
Sandy Loam ◽  
Conservation Tillage ◽  
Conventional Tillage ◽  
Sandy Loam Soil ◽  
Residue Management ◽  
Carbon Availability ◽  
Denitrification Potential ◽  
Soluble Organic Carbon ◽  
Loam Soil

Conservation tillage and crop residues should increase the soluble organic carbon and nitrate concentration in agricultural soil, which increases the denitrification potential. Basal denitrification (72 h laboratory incubation) was 2.1–2.7 times higher in a sandy loam soil under 15 yr of conservation tillage than conventional tillage and 1.8–2.0 times higher with high-residue (additional input 8.6–9.4 Mg dry matter·ha−1·yr−1) than low-residue inputs. Adding glucose and nitrate increased the soil denitrification potential 3- to 14-fold. Denitrification was limited by carbon availability, even in soil with 15 yr of conservation tillage and high-residue inputs.

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