## Abstract Increasing concern for problems of soil degradation and the offβsite impacts of accelerated erosion has generated a need for improved methods of estimating rates and patterns of soil erosion by water. The use of environmental radionuclides, particularly ^137^Cs, to estimate erosion rate
Estimation of soil erosion from caesium-137 measurements in a small, cultivated catchment in Australia
β Scribed by R.J. Loughran; G.L. Elliott; B.L. Campbell; D.J. Shelly
- Publisher
- Elsevier Science
- Year
- 1988
- Weight
- 441 KB
- Volume
- 39
- Category
- Article
- ISSN
- 0883-2889
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β¦ Synopsis
Measurements
are reported of the distribution of "'Cs within a 6.6 ha drainage basin on cultivated black earth soils located near Merriwa in New South Wales (N.S.W.). The results were used to estimate net loss as well as accumulation of soil. The losses of "'Cs from the catchment slopes were assessed relative to an estimated input of "'Cs of 1OOmBq cm-l.
A regression equation was developed which relates the net loss of soil by erosion of black earth soils (kg ha-' y-') as a function of the measured loss of '~'CS activity in the soil expressed as a percentage of the normal input value.
Each input datum of '~'CS activity into the regression equation was obtained under similar conditions. Rates of soil losses, estimated at 19 sites, ranged between 420 and 2970 kg ha-' y-' with an average of 1530 kg ha-' y-l. The results confirmed the usefulness of the "'Cs technique for estimating loss of soil by erosion
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## Abstract Floodplains comprise geomorphologically important sources and sinks for sediments and associated pollutants, yet the sedimentology of large dryland floodplains is not well understood. Processes occurring on such floodplains are often difficult to observe, and techniques used to investig
The contributions of sediment from different geomorpholigical units within a small basin in the Loess Plateau have been determined using caesium-137 as a tracer. The mean caesium-137 content of sediment originating from the hill area, where sheet and rill erosion are predominant, was 3.37Bq kg-I, wh