The influence of clay-to-carbon ratio on soil physical properties in a humid sandy loam soil with contrasting tillage and residue management

Geoderma ◽  
2016 ◽  
Vol 264 ◽  
pp. 94-102 ◽  
Author(s):  
G.T. Getahun ◽  
L.J. Munkholm ◽  
P. Schjønning
Keyword(s):  
Physical Properties ◽  
Sandy Loam ◽  
Soil Physical Properties ◽  
Sandy Loam Soil ◽  
Residue Management ◽  
Loam Soil

Short-term effects of cover crops and tillage methods on soil physical properties and maize growth in a sandy loam soil

2019 ◽  
Vol 192 ◽  
pp. 76-86 ◽  
Author(s):  
Lidong Ren ◽  
Thijs Vanden Nest ◽  
Greet Ruysschaert ◽  
Tommy D’Hose ◽  
Wim M. Cornelis
Keyword(s):  
Physical Properties ◽  
Cover Crops ◽  
Sandy Loam ◽  
Soil Physical Properties ◽  
Sandy Loam Soil ◽  
Short Term ◽  
Maize Growth ◽  
Loam Soil ◽  
Tillage Methods ◽  
Short Term Effects

scholarly journals Influence of some Organic Manure and NPK 15:15:15 on Selected Physical Properties of Sandy Loam Soil in Mokwa Niger State Nigeria

Land Science ◽  
2020 ◽  
Vol 2 (1) ◽  
pp. p1
Author(s):  
Mohammed JIYA MAMMAN
Keyword(s):  
Physical Properties ◽  
Sandy Loam ◽  
Research Work ◽  
Poultry Manure ◽  
Infiltration Rate ◽  
Soil Physical Properties ◽  
Organic Manure ◽  
Sandy Loam Soil ◽  
Cow Dung ◽  
Loam Soil

The result of long time farming and poor soil management and conservation practices at Niger state college of Agriculture Mokwa Commercial farm which is the study area has led to serious soil degradation like nutrient depletion and soil erosion. There is the need for local content research and innovation to ameliorate the problem. This research work described the effect of organic manure and inorganic fertilizer (poultry manure, Cow dung and NPK fertilizer) on some soil physical properties i.e. the infiltration, porosity, bulk density and erodibility on a sandy loam soil of Mokwa North Central Nigeria. Four treatments of poultry, cow dung manure, NPK 15:15:15 fertilizer and non – application were applied in RCBD with 25t/ha of poultry manure and cow dung while NPK 15:15:15 was 150kg/ha and non- application as control replicated three times. Soil physical properties were measured and analyses were done to ascertain the soil aggregates. Ring infiltrometers were constructed and used to test the infiltration rate of the soil at each plot before soil treatments. Measurements were taken at time intervals for all the plots. The plots were then treated with manure and NPK and left for two weeks to decompose, after which infiltration measurements were taken again. Minitab 17 and Excel were used for the analysis. The cow Dung manure shows highest infiltration rate as compared to other treatments. The experiment shows that Cow Dung and poultry manure can be used to correct infiltration and soil physical anomalies especially when soil is compacted or clayey.

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.

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