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פותח על ידי קלירמאש פתרונות בע"מ -
Organic matter and aggregate size interactions in infiltration, seal formation, and soil loss
Year:
2004
Authors :
בן-חור, מני
;
.
Volume :
68
Co-Authors:
Lado, M., Inst. Soil, Water, and Environ. Sci., Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel
Paz, A., Faculty of Sci., Univ. of La Coruna, A Zapateira s/n, 15071 La Coruna, Spain
Ben-Hur, M., Inst. Soil, Water, and Environ. Sci., Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel
Facilitators :
From page:
935
To page:
942
(
Total pages:
8
)
Abstract:
The objectives of this study were to investigate (i) the effect of soil organic matter (OM) content on the mechanisms that form a seal, and (ii) the OM content and aggregate size interactions in seal properties, infiltration rate (IR), anil soil loss. Two samples of sandy loam (Humic Dystrudept) designated low-OM soil (2.3% by weight OM) and high-OM soil (3.5% OM) were studied. Aggregate sizes <2, 2 to 4, and 4 to 6 mm of each soil were exposed to 80 mm of simulated rainfall with an intensity of 42 mm h-1. The final IR increased with increasing aggregate size from 4.2 to 5.2 mm h-1 in the low-OM soil, and from 5.8 to 10.8 mm h-1 in the high-OM soil. There was a significant interaction between OM content and aggregate size in seal formation and final IR. The low aggregate stability and the high dispersivity of the low-OM soil allowed the development of a dense and thick crust for all the aggregate sizes. Conversely, the high aggregate stability and the low dispersivity of the high-OM soil limited the seal formation. Consequently, the IR values were high and differences in IR among the three aggregate sizes in this soil were relatively high. The soil losses increased with increasing aggregate size, ranging from 4.5 × 10-3 to 6.6 × 10-3 kg m-2 mm-1 in the low-OM soil, and from 1.2 to 3.8 × 10-3 kg m-2 mm-1 in the high-OM soil. In this case, no significant interaction was found between soil OM content and aggregate size.
Note:
Related Files :
Aggregates
Aggregate size
Organic matters (OM)
rain
sandy loam
Seal formation
sealing
soil erosion
soil organic matter
Soils
עוד תגיות
תוכן קשור
More details
DOI :
Article number:
Affiliations:
Database:
סקופוס
Publication Type:
מאמר
;
.
Language:
אנגלית
Editors' remarks:
ID:
32795
Last updated date:
02/03/2022 17:27
Creation date:
17/04/2018 01:12
Scientific Publication
Organic matter and aggregate size interactions in infiltration, seal formation, and soil loss
68
Lado, M., Inst. Soil, Water, and Environ. Sci., Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel
Paz, A., Faculty of Sci., Univ. of La Coruna, A Zapateira s/n, 15071 La Coruna, Spain
Ben-Hur, M., Inst. Soil, Water, and Environ. Sci., Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel
Organic matter and aggregate size interactions in infiltration, seal formation, and soil loss
The objectives of this study were to investigate (i) the effect of soil organic matter (OM) content on the mechanisms that form a seal, and (ii) the OM content and aggregate size interactions in seal properties, infiltration rate (IR), anil soil loss. Two samples of sandy loam (Humic Dystrudept) designated low-OM soil (2.3% by weight OM) and high-OM soil (3.5% OM) were studied. Aggregate sizes <2, 2 to 4, and 4 to 6 mm of each soil were exposed to 80 mm of simulated rainfall with an intensity of 42 mm h-1. The final IR increased with increasing aggregate size from 4.2 to 5.2 mm h-1 in the low-OM soil, and from 5.8 to 10.8 mm h-1 in the high-OM soil. There was a significant interaction between OM content and aggregate size in seal formation and final IR. The low aggregate stability and the high dispersivity of the low-OM soil allowed the development of a dense and thick crust for all the aggregate sizes. Conversely, the high aggregate stability and the low dispersivity of the high-OM soil limited the seal formation. Consequently, the IR values were high and differences in IR among the three aggregate sizes in this soil were relatively high. The soil losses increased with increasing aggregate size, ranging from 4.5 × 10-3 to 6.6 × 10-3 kg m-2 mm-1 in the low-OM soil, and from 1.2 to 3.8 × 10-3 kg m-2 mm-1 in the high-OM soil. In this case, no significant interaction was found between soil OM content and aggregate size.
Scientific Publication
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