CAJ | 학술논문

为探索不同肥力水平对渭北旱塬连作冬小麦田在长周期免耕/深松轮耕措施下土壤蓄水保墒和作物增产效应的影响,在模拟精度验证基础上,应用WinEPIC模型长周期定量模拟研究了1980–2009年渭北旱塬免耕/深松轮耕连作麦田5个不同施肥水平下(T1, N 75 kg hm–2+P2O560 kg hm–2； T2, N 120 kg hm–2+P2O590 kg hm–2； T3, N 150 kg hm–2+P2O5120 kg hm–2； T4, N 180 kg hm–2+P2O5150 kg hm–2； T5, N 255 kg hm–2+P2O590 kg hm–2)冬小麦产量和土壤水分效应。在30年模拟期间,各处理的冬小麦产量、年度耗水量和水分利用效率均呈波动下降趋势,下降幅度表现为T5>T4>T3>T2>T1。0~5 m土层土壤有效含水量呈季节性波动降低趋势,且随施肥水平的升高而降低,5个处理的麦田平均干燥化速率依次为每年13.5、17.1、17.4、20.1和23.9 mm。0~1.5 m土层土壤湿度随季节降水波动；各处理在不同深度形成稳定的土壤干层,其中T1在1.5~2.0 m, T2和T3在1.5~3.0 m, T4和T5在1.5~4.0 m。上述结果表明,随着肥力水平的增加,旱作冬小麦产量和耗水量也增加,土壤干层加厚。综合考虑认为,在渭北旱塬免耕/深松轮耕长期连作小麦田适宜的施肥量为纯氮150 kg hm–2+P2O5120 kg hm–2。
위탐색불동비력수평대위북한원련작동소맥전재장주기면경/심송륜경조시하토양축수보상화작물증산효응적영향,재모의정도험증기출상,응용WinEPIC모형장주기정량모의연구료1980–2009년위북한원면경/심송륜경련작맥전5개불동시비수평하(T1, N 75 kg hm–2+P2O560 kg hm–2； T2, N 120 kg hm–2+P2O590 kg hm–2； T3, N 150 kg hm–2+P2O5120 kg hm–2； T4, N 180 kg hm–2+P2O5150 kg hm–2； T5, N 255 kg hm–2+P2O590 kg hm–2)동소맥산량화토양수분효응。재30년모의기간,각처리적동소맥산량、년도모수량화수분이용효솔균정파동하강추세,하강폭도표현위T5>T4>T3>T2>T1。0~5 m토층토양유효함수량정계절성파동강저추세,차수시비수평적승고이강저,5개처리적맥전평균간조화속솔의차위매년13.5、17.1、17.4、20.1화23.9 mm。0~1.5 m토층토양습도수계절강수파동；각처리재불동심도형성은정적토양간층,기중T1재1.5~2.0 m, T2화T3재1.5~3.0 m, T4화T5재1.5~4.0 m。상술결과표명,수착비력수평적증가,한작동소맥산량화모수량야증가,토양간층가후。종합고필인위,재위북한원면경/심송륜경장기련작소맥전괄의적시비량위순담150 kg hm–2+P2O5120 kg hm–2。
This study aimed at understanding the responses of grain yield and soil moisture to fertilization level in dryland winter wheat under long-term alternative no-tillage and subsoil tillage. The WinEPIC model was employed on the basis of precision veri-fication with five fertilization levels (T1, N 75 kg ha–1+P2O5 60 kg ha–1; T2, N 120 kg ha–1+P2O5 90 kg ha–1; T3, N 150 kg ha–1+P2O5 120 kg ha–1; T4, N 180 kg ha–1+P2O5 150 kg ha–1; and T5, N 255 kg ha–1+P2O5 90 kg ha–1) and the simulation period was from 1980 to 2009. During the 30-year period, water consumption in the growing season and water use efficiency of winter wheat tended to decrease in a fluctuating manner at different fertilization levels with the ranking sequence of T5>T4>T3>T2>T1. In the 0–5 m soil depth, the monthly available soil moisture tended to decrease in a seasonally fluctuating manner and reduced with the increase of fertilization amount. The soil desiccation rates from T1 to T5 were 13.5, 17.1, 17.4, 20.1, and 23.9 mm per year, respectively. During the simulation period, the soil humidity in 0–1.5 m soil layer fluctuated with the seasonal rainfall. A stable dry soil layer was found under all fertilization levels which was 1.5–2.0 m under T1, 1.5–3.0 m under T2 and T3, and 1.5–4.0 m under T4 and T5. These results indicate that grain yield and water consumption of winter wheat may increase with more fertilizer input, however, the dried soil layer is thickened. In a comprehensive consideration, we suggest N 150 kg ha–1+P2O5 120 kg ha–1 to be the optimal fertilization rates in winter wheat under long-term alternative no-tillage and subsoil tillage in Weibei Highlands.