Hillslope runoff and erosion on duplex soils in grazing lands in semi-arid central Queensland. I. Influences of cover, slope, and soil

David Silburn, Chris Carroll, Cyril A A Ciesiolka, R. C. DeVoil, Patrick W Burger

Research output: Contribution to journalArticle

37 Citations (Scopus)

Abstract

Many soils in semi-arid grazing lands develop low pasture cover or bare areas (scalds) under heavy grazing and have a low tolerance to soil erosion, due to low total water-holding capacity and concentration of nutrients in the soil surface. Runoff and erosion was measured for 7 years on 12 hillslope plots with cover (pasture plus litter) ranging from 10 to 80%, slopes from 4 to 8%, with and without grazing, with and without tree canopy cover, on a variety of soils. Soils were grouped into those derived from sandstone (SS), mudstone (MS), and eroded mudstone (MSe). One plot with low cover had a grass filter at the outlet. Runoff was strongly influenced by surface cover and was high with low cover (200-300 mm/year or 30-50% of rainfall). Runoff averaged 35 mm/year or 5.9% of rainfall with >50% cover. All soils fitted the same runoff-cover relationship. The grass filter had no effect on runoff and suspended load, but did reduce bedload. Grass pasture cover and tree litter cover were equally effective in controlling runoff and erosion. Total, bedload, and suspended load sediment concentrations increased linearly with slope in the range 4-8% for plots with low cover, and decreased exponentially with greater cover. Total and bedload sediment-cover relationships were similar for SS, MS, and MSe. However, plots on MSe had higher suspended sediment losses and thus slightly higher total soil losses. For all soils, erosion resulted in low sediment concentrations due to the hard-set surface soil, but total soil losses were high due to the large volumes of runoff generated. Concentration-cover relationships were different for bedload and suspended sediment. Consequently, suspended sediment was 20-40% of total soil loss for bare soil, and increased with cover to about 80% with cover >80%. The proportion of suspended sediment for bare soil was similar to the proportion of dispersed silt plus clay in the surface soil. About 90% of suspended sediment was fine-sized (50% ground cover to avoid excessive runoff and soil erosion, and degradation of soil productivity, and to maintain good off-site water quality. © CSIRO 2011.
Original languageEnglish
Pages (from-to)105-117
Number of pages13
JournalSoil Research
Volume49
Issue number2
DOIs
Publication statusPublished - 2011
Externally publishedYes

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grazing lands
duplex
hillslope
Queensland
runoff
grazing
erosion
suspended sediment
mudstone
bedload
soil
soil erosion
pasture
soil surface
suspended load
grass
bare soil
filter strips
litter
pastures

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Silburn, David ; Carroll, Chris ; Ciesiolka, Cyril A A ; DeVoil, R. C. ; Burger, Patrick W. / Hillslope runoff and erosion on duplex soils in grazing lands in semi-arid central Queensland. I. Influences of cover, slope, and soil. In: Soil Research. 2011 ; Vol. 49, No. 2. pp. 105-117.
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title = "Hillslope runoff and erosion on duplex soils in grazing lands in semi-arid central Queensland. I. Influences of cover, slope, and soil",
abstract = "Many soils in semi-arid grazing lands develop low pasture cover or bare areas (scalds) under heavy grazing and have a low tolerance to soil erosion, due to low total water-holding capacity and concentration of nutrients in the soil surface. Runoff and erosion was measured for 7 years on 12 hillslope plots with cover (pasture plus litter) ranging from 10 to 80{\%}, slopes from 4 to 8{\%}, with and without grazing, with and without tree canopy cover, on a variety of soils. Soils were grouped into those derived from sandstone (SS), mudstone (MS), and eroded mudstone (MSe). One plot with low cover had a grass filter at the outlet. Runoff was strongly influenced by surface cover and was high with low cover (200-300 mm/year or 30-50{\%} of rainfall). Runoff averaged 35 mm/year or 5.9{\%} of rainfall with >50{\%} cover. All soils fitted the same runoff-cover relationship. The grass filter had no effect on runoff and suspended load, but did reduce bedload. Grass pasture cover and tree litter cover were equally effective in controlling runoff and erosion. Total, bedload, and suspended load sediment concentrations increased linearly with slope in the range 4-8{\%} for plots with low cover, and decreased exponentially with greater cover. Total and bedload sediment-cover relationships were similar for SS, MS, and MSe. However, plots on MSe had higher suspended sediment losses and thus slightly higher total soil losses. For all soils, erosion resulted in low sediment concentrations due to the hard-set surface soil, but total soil losses were high due to the large volumes of runoff generated. Concentration-cover relationships were different for bedload and suspended sediment. Consequently, suspended sediment was 20-40{\%} of total soil loss for bare soil, and increased with cover to about 80{\%} with cover >80{\%}. The proportion of suspended sediment for bare soil was similar to the proportion of dispersed silt plus clay in the surface soil. About 90{\%} of suspended sediment was fine-sized (50{\%} ground cover to avoid excessive runoff and soil erosion, and degradation of soil productivity, and to maintain good off-site water quality. {\circledC} CSIRO 2011.",
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Hillslope runoff and erosion on duplex soils in grazing lands in semi-arid central Queensland. I. Influences of cover, slope, and soil. / Silburn, David; Carroll, Chris; Ciesiolka, Cyril A A; DeVoil, R. C.; Burger, Patrick W.

In: Soil Research, Vol. 49, No. 2, 2011, p. 105-117.

Research output: Contribution to journalArticle

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T1 - Hillslope runoff and erosion on duplex soils in grazing lands in semi-arid central Queensland. I. Influences of cover, slope, and soil

AU - Silburn, David

AU - Carroll, Chris

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AU - Burger, Patrick W

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AB - Many soils in semi-arid grazing lands develop low pasture cover or bare areas (scalds) under heavy grazing and have a low tolerance to soil erosion, due to low total water-holding capacity and concentration of nutrients in the soil surface. Runoff and erosion was measured for 7 years on 12 hillslope plots with cover (pasture plus litter) ranging from 10 to 80%, slopes from 4 to 8%, with and without grazing, with and without tree canopy cover, on a variety of soils. Soils were grouped into those derived from sandstone (SS), mudstone (MS), and eroded mudstone (MSe). One plot with low cover had a grass filter at the outlet. Runoff was strongly influenced by surface cover and was high with low cover (200-300 mm/year or 30-50% of rainfall). Runoff averaged 35 mm/year or 5.9% of rainfall with >50% cover. All soils fitted the same runoff-cover relationship. The grass filter had no effect on runoff and suspended load, but did reduce bedload. Grass pasture cover and tree litter cover were equally effective in controlling runoff and erosion. Total, bedload, and suspended load sediment concentrations increased linearly with slope in the range 4-8% for plots with low cover, and decreased exponentially with greater cover. Total and bedload sediment-cover relationships were similar for SS, MS, and MSe. However, plots on MSe had higher suspended sediment losses and thus slightly higher total soil losses. For all soils, erosion resulted in low sediment concentrations due to the hard-set surface soil, but total soil losses were high due to the large volumes of runoff generated. Concentration-cover relationships were different for bedload and suspended sediment. Consequently, suspended sediment was 20-40% of total soil loss for bare soil, and increased with cover to about 80% with cover >80%. The proportion of suspended sediment for bare soil was similar to the proportion of dispersed silt plus clay in the surface soil. About 90% of suspended sediment was fine-sized (50% ground cover to avoid excessive runoff and soil erosion, and degradation of soil productivity, and to maintain good off-site water quality. © CSIRO 2011.

U2 - 10.1071/SR09068

DO - 10.1071/SR09068

M3 - Article

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SP - 105

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JO - Australian Journal of Soil Research

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ER -