LONG-TERM EFFECTS OF EROSION AND CLIMATE INTERACTIONS ON CORN YIELD

Citation
Mj. Shaffer et al., LONG-TERM EFFECTS OF EROSION AND CLIMATE INTERACTIONS ON CORN YIELD, Journal of soil and water conservation, 49(3), 1994, pp. 272-275
Citations number
14
Categorie Soggetti
Water Resources",Ecology,"Agriculture Soil Science
ISSN journal
00224561
Volume
49
Issue
3
Year of publication
1994
Pages
272 - 275
Database
ISI
SICI code
0022-4561(1994)49:3<272:LEOEAC>2.0.ZU;2-7
Abstract
An accurate assessment of the impacts of soil erosion on corn producti on ss needed for conservation and management programs. Climatic variab ility produces a range of crop yield responses on eroded and non-erode d soil profiles and often masks the long-term trends and differences. Short-term corn yield data from representative soils across the North Central region were supplemented with calculated yields from the NTRM model to develop long-term yield responses for the historical climate records at each of seven highly-managed rainfed sites across the regio n. Results showed that long-term average regional corn yields were red uced by 10% for severely eroded versus control plots. Till-derived soi ls showed yield reductions averaging 12%, while loess soils lost an av erage of 7%. Sensitivity runs with the NTRM model made after field val idation with 119 plot-years of data suggested that changes in soil phy sical properties, especially plant-available water bolding capacities, probably accounted for most of the yield differences. Mean growing se ason (May-September) precipitation across all sites for the short-term field study was 35.3 cm, compared with 36.3 cm for the long-term hist orical record. This resulted in a mean short-term corn yield reduction of 9% for severely eroded soils versus a reduction of 10% for the sam e soils based on long-term climate projections. However, the close agr eement between the short- and long-term studies with regard to mean gr owing season precipitation and corresponding corn yields should not be used to make the general conclusion that 3 to 6 years is an adequate time period for research on long-term crop response to eroded soil con ditions.