TY - JOUR
T1 - Variability of soil physical quality in uneroded, eroded, and depositional cropland sites
AU - Stavi, I.
AU - Lal, R.
N1 - Funding Information:
We are very grateful to Mr. Glenn Mills for his efficient assistance in the field, and Mr. Sandy Jones for his helpful guidance in the laboratory. We thank the Midwest Regional Carbon Sequestration Partnership (MRCSP) for funding the study.
PY - 2011/1/1
Y1 - 2011/1/1
N2 - Erosion and deposition processes affect the physical quality of the soil. Thus, the objective of this study was to assess the effects of these processes on a long-term no-till corn agroecosystem in a humid-temperate region of the Midwest U.S. The study was conducted under on-farm conditions, in a field which experiences erosional and depositional processes. At the end of the dormant season, soil characteristics were tested for two depths (0-5 and 5-10cm) in uneroded (UN), eroded (ER), and depositional (DP) sites. The data showed that UN and ER were characterized by the highest and lowest soil shear strength (137.3 and 78.1KPa, respectively) and organic carbon concentration (35.6 and 30.3g kg-1, respectively). The highest and lowest aggregate stability (85.4% and 73.6%, respectively) and mean weight diameter (2.9 and 1.6mm, respectively) were observed in UN and DP. The highest and lowest penetration resistance (4.82 and 4.57MPa, respectively) and bulk density (1.49 and 1.33Mg m-3, respectively) were measured in ER and DP. An opposite trend was observed for the C:N ratio (8.2 and 9.6, respectively), and the value's color variable (4.6 and 4.9, respectively). No significant differences among the erosional phases were measured in the soil's total nitrogen concentration, hue and chroma color variables, texture, hydraulic conductivity, and intrinsic permeability. The erodibility factor was the lowest and highest in DP and ER (0.00326 and 0.00397Mg ha h ha-1 MJ-1 mm-1, respectively), and the effect of erosional phase on this factor was close to significant. In general, the effect of erosion and deposition on soil characteristics decreased with an increase in soil depth. This study suggests that the occurrence of positive feedbacks in ER and DP have led to accelerated erosional and depositional processes and the continuous degradation of the soil quality. A range of management practices should be considered in order to mitigate these processes and reduce negative impact on crop yields in such agroecosystems.
AB - Erosion and deposition processes affect the physical quality of the soil. Thus, the objective of this study was to assess the effects of these processes on a long-term no-till corn agroecosystem in a humid-temperate region of the Midwest U.S. The study was conducted under on-farm conditions, in a field which experiences erosional and depositional processes. At the end of the dormant season, soil characteristics were tested for two depths (0-5 and 5-10cm) in uneroded (UN), eroded (ER), and depositional (DP) sites. The data showed that UN and ER were characterized by the highest and lowest soil shear strength (137.3 and 78.1KPa, respectively) and organic carbon concentration (35.6 and 30.3g kg-1, respectively). The highest and lowest aggregate stability (85.4% and 73.6%, respectively) and mean weight diameter (2.9 and 1.6mm, respectively) were observed in UN and DP. The highest and lowest penetration resistance (4.82 and 4.57MPa, respectively) and bulk density (1.49 and 1.33Mg m-3, respectively) were measured in ER and DP. An opposite trend was observed for the C:N ratio (8.2 and 9.6, respectively), and the value's color variable (4.6 and 4.9, respectively). No significant differences among the erosional phases were measured in the soil's total nitrogen concentration, hue and chroma color variables, texture, hydraulic conductivity, and intrinsic permeability. The erodibility factor was the lowest and highest in DP and ER (0.00326 and 0.00397Mg ha h ha-1 MJ-1 mm-1, respectively), and the effect of erosional phase on this factor was close to significant. In general, the effect of erosion and deposition on soil characteristics decreased with an increase in soil depth. This study suggests that the occurrence of positive feedbacks in ER and DP have led to accelerated erosional and depositional processes and the continuous degradation of the soil quality. A range of management practices should be considered in order to mitigate these processes and reduce negative impact on crop yields in such agroecosystems.
KW - Carbon cycle
KW - Conservation agriculture
KW - Geomorphic processes
KW - Landscape functionality
KW - Soil erodibility
KW - Soil structure
UR - http://www.scopus.com/inward/record.url?scp=78349311900&partnerID=8YFLogxK
U2 - 10.1016/j.geomorph.2010.09.006
DO - 10.1016/j.geomorph.2010.09.006
M3 - Article
AN - SCOPUS:78349311900
SN - 0169-555X
VL - 125
SP - 85
EP - 91
JO - Geomorphology
JF - Geomorphology
IS - 1
ER -