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Temporal variation in properties of an uncropped, ploughed Miamian soil in relation to seasonal erodibility
Author(s) -
Bajracharya R. M.,
Lal R.,
Hall G. F.
Publication year - 1998
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/(sici)1099-1085(19980615)12:7<1021::aid-hyp635>3.0.co;2-z
Subject(s) - loam , environmental science , tillage , erosion , plough , silt , sediment , hydrology (agriculture) , soil science , seasonality , soil water , agronomy , geology , ecology , geomorphology , geotechnical engineering , biology
Knowledge of seasonal variation in soil structural and related properties is important for the determination of critical periods during which soil is susceptible to accelerated erosion and other degradative processes. The purpose of this research was to evaluate the magnitude of seasonal variations in selected soil and deposited sediment properties in relation to soil erodibility for a Miamian silt‐loam soil (Typic Hapludalf) in central Ohio. Erosion plots (USLE‐type) were established on a 4·5% slope and maintained under bare, ploughed conditions from 1988 to 1991. Particle size distribution, bulk density(ρ b ), percentage water stable aggregates (WSA), soil organic carbon (SOC), and total soil nitrogen (TSN) of both soil and sediment samples were monitored between Autumn 1989 and Spring 1991. The soil and sediment particle size distributions followed no clear seasonal trends. Soil ρ b increased following tillage (1·20 Mg m −3 ) and was highest (1·45 Mg m −3 ) during the autumn owing to soil slumping and consolidation upon drying. Low winter and spring values of ρ b and %WSA (20–50% lower than in autumn) were attributed to excessive wetness and freeze–thaw effects. Both SOC and soil TSN contents progressively declined (from 2·18 to 1·79% and 1·97 to 1·75 g kg −1 , respectively) after ploughing owing to maintenance of plots under bare, fallow conditions. Spring highs and autumn lows of sediment SOC (3·12 vs. 2·44%) and TSN (2·70 vs. 1·96 g kg −1 ) contents were a result of the combined effects of soil microbial activity and rainfall erosivity. Soil properties such as bulk density, SOC and WSA, which vary seasonally, can potentially serve as predictors of seasonal soil erodibility, which, in turn, could improve the predictive capacity of soil erosion prediction models. © 1998 John Wiley & Sons, Ltd.