黄土高原生态系统中土壤氮库的储量、流量及其消长趋势
THE PRESERVATION AND DISCHARGE OP SOIL NITROGEN POOL AND ITS GROWTH AND DECLINE TREND IN THE ECOLOGICAL SYSTEMS OF LOESS PLATEAU
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摘要: 本文以黄土高原生态系统中土壤氮库为中心,研究了土壤氮库的能量、流量以及消长趋势。研究结果表明,黄土高原表层(0—20cm)土壤氮库储氮量为1.5×10~8t,主要吸肥层(0—1m)为5.0×108t。高产农田土壤氮库储量为2—3t/ha,中产农田土壤为1.5—2.0t/ha,低产农田土壤仅1.0—1.5t/ha。黄土高原土壤氮库的流入量为235×104t,其中化学氮肥流入量占总流入量57.0%,有机肥占36.6%;流出量为250×104t,其中由作物收获流出氮量占69.6%,水土流失占12.8%,土壤氮库呈现负平衡,其中氮储量有缓慢下降趋势。为此,要大力增加化学氮肥与有机肥投入量。同时应采取多种措施,以提高有机氮流入量,还应大力降低非生产性氮流出量,使土壤氮库保持动态平衡与稳步增长。Abstract: The preservation and discharge of soil nitrogen pool and its growth and decline trend in the ecological systems of loess plateau were discussed with the following resulfs:1. The nitrogen preserved in the top soil ( 0-20cm ) was 1.5×108 tons, and 5.0×108 tons in the layer reached by the plant roots ( 0-1m). The nitrogen preserved in soils of high-yielding crop land was 2 - 3 t/ha; 1.5-2.0 t/ha in moderate yielding soils and 1.0-1.5 t/ha in low yielding soils.2. The total input to soil nitrogen pools was 235×104 tons, among which 57.0% came from chemical nitrogen fertilizer, 36.6% from organic manure. The total output ,of nitrogen was 250×104 t, among which 69.6% due to harvest of crops, 12.8% due to erosion.3. Great effort should be made to increase nitrogen content by applying chemical fertilizers and organic materials because negative balance of soil nitrogen pool usually occured. Non-production oulput of soil nitrogen should be decreased in order to keep a dynamic equilibrium of soil nitrogen.