• ISSN 1008-505X
  • CN 11-3996/S
岳龙凯, 蔡泽江, 徐明岗, 王伯仁, 李冬初, 黄晶, 张会民. 长期施肥红壤钾有效性研究[J]. 植物营养与肥料学报, 2015, 21(6): 1543-1550. DOI: 10.11674/zwyf.2015.0621
引用本文: 岳龙凯, 蔡泽江, 徐明岗, 王伯仁, 李冬初, 黄晶, 张会民. 长期施肥红壤钾有效性研究[J]. 植物营养与肥料学报, 2015, 21(6): 1543-1550. DOI: 10.11674/zwyf.2015.0621
YUE Long-kai, CAI Ze-jiang, XU Ming-gang, WANG Bo-ren, LI Dong-chu, HUANG Jing, ZHANG Hui-min. Potassium availability in red soil under long-term fertilization[J]. Journal of Plant Nutrition and Fertilizers, 2015, 21(6): 1543-1550. DOI: 10.11674/zwyf.2015.0621
Citation: YUE Long-kai, CAI Ze-jiang, XU Ming-gang, WANG Bo-ren, LI Dong-chu, HUANG Jing, ZHANG Hui-min. Potassium availability in red soil under long-term fertilization[J]. Journal of Plant Nutrition and Fertilizers, 2015, 21(6): 1543-1550. DOI: 10.11674/zwyf.2015.0621

长期施肥红壤钾有效性研究

Potassium availability in red soil under long-term fertilization

  • 摘要: 目的 长期不同施肥可改变土壤速效钾、 缓效钾含量及土壤pH,进而影响土壤钾素有效性。本研究利用始于1990年的祁阳旱地红壤长期定位试验,研究不同施肥条件下土壤钾素有效性的变化情况,为指导合理施肥提高土壤肥力提供依据。方法 选择不施肥(CK)、 施氮磷化肥(NP)、 施氮磷钾化肥(NPK)、 氮磷钾肥与有机肥配施(NPKM)4个处理。采用生物耗竭方法,以玉米苗为供试作物,在施用氮磷肥不施钾肥的条件下连续种植5次,测定每次种植20 d后玉米钾素含量及土壤速效钾、 缓效钾含量。结果 1)土壤速效钾含量随耗竭种植次数的增加而逐渐降低。22年不同施肥土壤速效钾含量存在差异,耗竭种植后土壤速效钾含量的变化表现为: CK处理在第二次种植后土壤速效钾含量降至最低值,NP处理在5次耗竭种植后土壤速效钾含量接近最低值。5次耗竭种植后CK和NP处理土壤速效钾含量分别降低了45.2和41.7 mg/kg,降低幅度分别为65.9%和60.4%; NPK和NPKM处理分别降低了171.0和390.3 mg/kg,降低幅度为73.4%和81.3%。2)22年后不同施肥处理土壤缓效钾含量高低顺序为NPKM NPK NP CK,5次耗竭种植后土壤缓效钾含量顺序未发生变化。5次耗竭种植后CK和NP处理土壤缓效钾含量分别降低了54.0和77.0 mg/kg,降低幅度分别为46.0%和53.8%; NPK和NPKM处理分别降低了41.0和55.0 mg/kg,降低幅度分别为27.2%和22.5%。3)玉米钾素带出总量的大小顺序为NPKM NPK CK NP,NPKM处理玉米钾素带出总量是NPK处理的3.1倍,NPK处理是NP处理的1.9倍。4)采用Elovich方程对土壤钾素供应能力进行模拟得出土壤供钾能力的大小顺序与实际顺序一致,从方程决定系数和标准误差角度判断一级动力学方程对CK和NPKM处理的拟合效果较好,Elovich方程对NP和NPK处理的拟合结果较好。5)土壤速效钾(X1)、 缓效钾(X2)、 全钾(X3)含量和土壤pH(X4)与玉米钾素带出量(y)的多元回归方程为y=-438.90+0.33X1+0.22X2+22.14X3+18.44X4 (R2=0.995),X1(土壤速效钾含量)与y达到显著正相关水平(P0.05); 逐步回归方程为y=-107.36+0.38X1+25.16X4 (R2=0.985),X1(土壤速效钾含量),X4(土壤pH)分别与y达到极显著(P0.01)和显著(P0.05)正相关水平。结论 基于耗竭种植条件下玉米钾素带出量,旱地红壤长期不同施肥后氮磷钾肥与有机肥配施(NPKM)处理的土壤钾素有效性高于氮磷钾化肥(NPK)处理,不施肥(CK)和施氮磷肥(NP)处理。土壤钾素供应能力及累积供应量的大小顺序表现为NPKM NPK CK NP。旱地红壤速效钾含量和土壤pH与玉米钾素累积带出量呈显著正相关关系(P0.05)。

     

    Abstract: 【Objectives】 Long-term fertilization has changed contents of soil readily available and slowly-available potassium (K) and soil pH, while all these changes affect availability of soil K to plants. In order to instruct the optimum fertilization to improve soil fertility, a long-term fertilization experiment started from 1990 (Qiyang experimental station located in Hunan province) was involved to explore soil K availability to plants. 【Methods】 Treatments of no fertilization (CK), mixed application of chemical nitrogen and phosphorus fertilizer (NP), application of NP combined with chemical potassium fertilizer (NPK), and application of NPK combined with manure (NPKM) were selected. The bio-exhausting method was used to exhaust soil K for five periods, twenty days for each period after the planting of maize. After each harvest, the contents of plant K and the soil readily available K and slowly-available K were determined. For each period the N and P but K nutrients were applied to soil. 【Results】 1) The contents of soil readily available K were decreased with the planting periods. The long-term different K fertilization changed the contents of soil readily available K. The contents of soil readily available K arrived at the lowest level?? after the second planting period with CK, while the NP nearly arrived at this level after the fifth planting period. However, after the fifth period, the contents of soil readily available K were decreased by 45.2 and 41.7 mg/kg under CK and NP, and the decreased ratios were 65.9% and 60.4% respectively, while the contents under NPK and NPKM were decreased by 171.0 and 390.3 mg/kg with the decreases ratios of 73.4% and 81.3% respectively. 2) After the 22 years?? fertilization the contents of soil slowly-available K were in the order of NPKM NPK NP CK. The contents of soil slowly-available K with CK and NP were decreased by 54.0 and 77.0 mg/kg with the decreased ratios of 46.0% and 53.8% respectively, while the contents under NPK and NPKM were decreased by 41.0 and 55.0 mg/kg with the decreased ratios of 27.2% and 22.5% respectively after the fifth planting period. 3) The amounts of K uptake by maize were in the order of NPKM NPK CK NP. The amount of K uptake by maize with NPKM was 3.1 times as high as that with NPK. Furthermore the amount under NPK was 1.9 times as high as that under NP. 4) The Elovich equation showed that the soil K availability to plant well matched the real value. The first order kinetic equation can simulate the treatments of CK and NPKM better than the Elovich equation. The Elovich equation can simulate the treatments of NP and NPK better than first order kinetic equation, judging from R2 and standard error (SE). 5) There was a multiple linear regression between the content of soil readily available K (X1), slowly-available K (X2), total K (X3) and soil pH (X4) and the amount of K uptake by maize (y). The equation was y=-438.90+0.33X1+0.22X2+22.14X3+18.44X4 (R2=0.995). There was a significant positive correlation between X1 and y (P0.05). The stepwise multiple regression equation was y=-107.36+0.38X1+25.16X4 (R2=0.985). There was an extremely significant positive correlation between X1 and y (P0.01), and a significant positive correlation between X4 and y (P0.05) respectively. 【Conclusions】 The K supply capacity was in the order of NPKM NPK CK NP based on the amounts of K uptake by maize with planting periods. There was a significant positive correlation between the content of soil readily available K and soil pH and the amount of K uptake by maize respectively.

     

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