SIMULATION OF WATER AND NITROGEN FLOWS AND PLANT-GROWTH FOR A WINTER-WHEAT STAND IN CENTRAL GERMANY

Citation
K. Blomback et al., SIMULATION OF WATER AND NITROGEN FLOWS AND PLANT-GROWTH FOR A WINTER-WHEAT STAND IN CENTRAL GERMANY, Ecological modelling, 81(1-3), 1995, pp. 157-167
Citations number
16
Categorie Soggetti
Ecology
Journal title
ISSN journal
03043800
Volume
81
Issue
1-3
Year of publication
1995
Pages
157 - 167
Database
ISI
SICI code
0304-3800(1995)81:1-3<157:SOWANF>2.0.ZU;2-T
Abstract
Two linked simulation models were applied to an experimental loam site at Neuenkirchen, Germany, for the years 1989 and 1991, using a data s et with soil and plant properties for winter wheat. Simulations of soi l water and heat dynamics were performed with the SOIL model. Both yea rs were rather dry. For the first year, soil water content and soil wa ter tension were calibrated by tuning the saturated hydraulic conducti vity. The simulations showed good correspondence with the measurements during the first six months down to 130 cm depth. However, the dynami cs of the simulated water tension in deeper layers was poor compared t o the measurements. Using the same parameterization for 1998, the mode l simulated soil moisture dynamics reasonably well in the upper 70 cm. Below this depth, the water content was underestimated. Soil and plan t nitrogen dynamics, litter decomposition and plant biomass production were simulated with the SOILN model. The model was tested against mea surements of leaf, stem and grain biomass and nitrogen, leaf area and soil nitrate and ammonium content. It was calibrated for the first yea r (1989) and validated in 1991. Parameters related to translocation of assimilates and nitrogen from different tissues to grain were estimat ed by calibration. The simulated plant properties in 1989 explained ab out 95% of the variations in measured values. A similar agreement was obtained for the validation year. The corresponding value for soil min eral nitrate in 1989 was only 38%, mainly due to problems in reproduci ng the dynamics in the upper 30 cm in connection to fertilization appl ications. In deeper layers up to 90% of the variation was explained. F or nitrate in 1991 and ammonium the agreement between simulated and me asured values was poor.