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It is shown that soils under the CT system tended to stay saturated for longer periods of time after each rainfall event.
After each rainfall event, the moisture at 5 10 cm depths decreases exponentially, attributable to both evapotranspiration at the surface and soil water infiltration into the deeper layer.
Surface soil samples were taken immediately before and after each rainfall event and also in between the rainfall events in order to monitor surface aggregate stability and soil FSD.
Because the N inputs as urine and manure on a pen surface can be considered inexhaustible in an open-lot beef cattle feedlot, it might be suggested that large emission peaks of GHGs are emitted after each rainfall event on dry soil/manure surfaces.
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The isotopic composition of throughfall and open rainfall were analyzed and compared for each rainfall event.
For each rainfall event with landslides, we reconstructed the rainfall history that presumably caused the slope failure, and we determined the corresponding rainfall duration D (in hours) and cumulated event rainfall E (in mm).
Automatic records were complemented with direct field observations of surface runoff in the experimental catchment after each significant rainfall event.
Fine soil particles and rock fragments were also assessed after each natural rainfall event and tillage practice.
Leachate was collected 24 h after each simulated rainfall event, and pH, EC, and K were analyzed directly in the collected solution.
Two potential contamination events, one after each major rainfall event on February 27 and March 2, respectively, were then proposed.
Based on the concentration found in the March 17 sample, the most probable peak concentration that the Clitheroe population would have been exposed to was 40 times greater, approximately 30 oocysts per 10 L. These values are based on tests in which the pulse was introduced instantaneously; in practice, contamination likely took place over several hours or days after each major rainfall event.
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