Tillage, mineralization and leaching: phosphate

被引:85
作者
Addiscott, TM [1 ]
Thomas, D [1 ]
机构
[1] AFRC, Inst Arable Crops Res, Dept Soil Sci, Harpenden AL5 2JQ, Herts, England
基金
英国生物技术与生命科学研究理事会;
关键词
leaching; surface run-off; organic and inorganic phosphate; erosion; tillage; mineralization;
D O I
10.1016/S0167-1987(99)00110-5
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Phosphate is usually the limiting nutrient for the formation of algal blooms in freshwater bodies, so tillage practices must minimize phosphate losses by leaching and surface run-off from cultivated land. Mineral soils usually contain 30-70% of their phosphate in organic forms;and both organic and inorganic phosphate are found in the soil solution. Some organic phosphates, notably the inositol phosphates, are as strongly sorbed by soil as inorganic phosphates, and this decreases their susceptibility to mineralization. The strength with which both categories are sorbed lessens the risk of their being leached as solutes but makes it more likely that they will be carried from the soil on colloidal or particulate matter, and the greatest losses of phosphate from the soil usually occur by surface run-off and erosion. Recent studies at Rothamsted have, however, shown substantial concentrations of phosphate in drainage from plots that have long received more phosphate as fertilizer than is removed in crops. These losses probably occurred because preferential water flow carried the phosphate rapidly from the surface soil to the field drains. For lessening losses of phosphate by leaching and run-off, the prime requirement of tillage is that it should encourage hows of water through the soil that help it to retain phosphate. Primary and secondary tillage should ensure that the surface roughness and porosity of the top-soil encourage the flow of water into the soil matrix where it will move relatively slowly and allow phosphate to be sorbed, thereby avoiding problems from run-off and preferential how. Inversion tillage can be useful for lessening the loss of phosphate by run-off and erosion. Secondary tillage could be used to decrease the size of the aggregates and increase the surface area for sorption. Although tillage will increase the mineralization of organic phosphate, pulses of mineralization are unlikely to be so rapid or to lead to such large losses as with nitrate. The strength with which phosphate is sorbed also lessens the problem. As with nitrate, the key to managing phosphate is basically good husbandry. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:255 / 273
页数:19
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