Spatio-temporal analysis of yield variability for a corn-soybean field in Iowa

Citation
A. Bakhsh et al., Spatio-temporal analysis of yield variability for a corn-soybean field in Iowa, T ASAE, 43(1), 2000, pp. 31-38
Citations number
28
Categorie Soggetti
Agriculture/Agronomy
Journal title
TRANSACTIONS OF THE ASAE
ISSN journal
00012351 → ACNP
Volume
43
Issue
1
Year of publication
2000
Pages
31 - 38
Database
ISI
SICI code
0001-2351(200001/02)43:1<31:SAOYVF>2.0.ZU;2-2
Abstract
Spatio-temporal analyses of yield variability are required to delineate are as of stable yield patterns for application of precision farming techniques . Spatial structure and temporal stability patterns were studied using 1995 -1997 yield data for a 25-ha field located near Story City, Iowa. Corn was grown during 1995-1996, and soybean in 1997. The yield data were collected on nine east-west transects, consisting of 25 yield blocks per transect. Th e two components of yield variability, i.e., large-scale variation (trend) and small-scale variation, were studied using median polishing technique an d variography, respectively. The trend surface, obtained from median polish ing, accounted for the large-scale deterministic structure induced by treat ments and landscape effects. After removal of trend from yield data, the re sulting yield residuals were used to analyze the small-scale stochastic var iability using variography. The variogram analysis showed strong spatial st ructure for the yield residuals. The spatial correlation lengths were found to vary from about 40 m for corn to about 90 m for soybean. The range para meter of the variograms showed a significant correlation coefficient of -0. 95 with the cumulative growing season rainfall. The total variance of 1995 corn yield was partitioned as 56% trend, 37% small-scale stochastic structu re, and 7% as an interaction of both. Yield variance of 1996 corn was about 80% trend and 20% small-scale stochastic structure. Contrary to corn years , the total yield variance for soybean in 1997 was partitioned as about 25% trend and about 75% small-scale stochastic structure. The significant nega tive correlation of range with rainfall shows that small-scale variability may be controlled by factors induced directly or indirectly by rainfall. Mo re years of data are required to substantiate these relationships. The lack of temporal stability in large-scale and small-scale variation suggest tha t longer duration yield data analyses are required to understand and quanti fy the impact of various climatic, and management factors and their interac tion with soil properties on delineation of areas under consistent yield pa tterns before applying variable rate technology.