THE DISTRIBUTION OF WATER AND NITROGEN IN THE SOIL-CROP SYSTEM - A SIMULATION STUDY WITH VALIDATION FROM A WINTER-WHEAT FIELD TRIAL

被引:38
作者
GRANT, RF
机构
[1] Department of Soil Science, University of Alberta, Edmonton, T6G 2E3, Alberta
来源
FERTILIZER RESEARCH | 1991年 / 27卷 / 2-3期
关键词
WATER UPTAKE; NITROGEN UPTAKE; MASS FLOW; DIFFUSION; ROOTING DISTRIBUTION; CROP GROWTH; NITROGEN PARTITIONING;
D O I
10.1007/BF01051128
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The realistic simulation of uptake processes for water and nitrogen, and of partitioning processes for nitrogen, are necessary to the accurate reproduction of water and nitrogen deficit effects on crop growth and yield. Mathematical descriptions of these processes, based on the findings of detailed studies, were used as part of a larger simulation model to calculate the extraction and uptake of water and nitrogen, and the distribution of nitrogen, by a winter wheat crop from a multi-layered soil profile over a growing season. Descriptions of water uptake processes allowed the model to reproduce the hourly dynamics of water uptake and redistribution through the root system, and to estimate the yearly dynamics of water depletion from the soil profile consistent with field data. Descriptions of nitrogen uptake processes allowed the model to reproduce the hourly dynamics of mass flow, diffusion and active uptake, but estimates of the yearly dynamics of mineral nitrogen depletion did not closely follow field data. This inconsistency arose largely from the partial disappearance of fertilizer nitrogen in the field plots shortly after application. This disappearance was not reproduced in the model. The model was able to reproduce the seasonal accumulation and redistribution of dry matter and nitrogen within the crop for fertilizer applications from 0 to 16 g m-2. These applications gave dry matter and nitrogen yields of phytomass from 1340 to 1600 and from 13.4 to 23.4 g m-2 respectively, and of grain from 673 to 810 and from 11.5 to 20.4 g m-2 respectively. However, the model tended to overestimate both dry matter and nitrogen yields under high rates of fertilizer application. This simulation study demonstrates that results from more detailed studies of water and nitrogen uptake may be used to understand the annual dynamics of water and nitrogen distribution in the soil-crop system.
引用
收藏
页码:199 / 213
页数:15
相关论文
共 36 条
[1]  
Baker J.M., van Bavel C.H.M., Water transfer through cotton plants connecting soil regions of differing water potentials, Agronomy Journal, 80, pp. 993-997, (1988)
[2]  
Barber S.A., A diffusion and mass-flow concept of soil nutrient availability, Soil Sci, 99, pp. 39-49, (1962)
[3]  
Barber S.A., Soil Nutrient Bioavailability: a Mechanistic Approach, (1984)
[4]  
Beek J., Frissel M.J., Simulation of nitrogen behavior in soils, (1973)
[5]  
Caassen N., Barber S.A., Simulation model for nutrient uptake from soil by a growing plant root system, Agronomy Journal, 68, pp. 961-964, (1976)
[6]  
Cushman J.H., An analytical solution to solute transport near root surfaces for low initial concentration, Soil Sci Soc Am J, 43, pp. 1087-1095, (1979)
[7]  
Fleisher Z., Kenig A., Ravina I., Hagin J., Model of ammonia volatilization from calcareous soils, Plant and Soil, 103, pp. 205-212, (1987)
[8]  
Gardner W.R., Dynamic aspects of water availability to plants, Soil Science, 89, pp. 63-73, (1960)
[9]  
Gilmour J.T., Clark M.D., Sigua G.C., Estimating net nitrogen mineralization from carbon dioxide evolution, Soil Sci Soc Am J, 49, pp. 1398-1402, (1985)
[10]  
Grant R.F., Simulation of carbon accumulation and partitioning in maize, Agronomy Journal, 81, pp. 563-571, (1989)