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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Potassium balance as influenced by farmyard manure application under continuous soybean-wheat cropping system in a Typic Haplaquept.
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Potassium balance as influenced by farmyard manure application under continuous soybean-wheat cropping system in a Typic Haplaquept.

机译:在典型的大豆斑节菜中,大豆-小麦连作制度下农田肥料施用对钾平衡的影响。

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摘要

The effect of 30 years of continuous cropping, fertilization and manuring on the potassium (K) balances, the soil K pools and the non-exchangeable K release in a Typic Haplaquept soil from Almora, India under a rainfed soybean-wheat cropping system were investigated. The apparent K balance was measured as the difference between the total K added and that removed by the crops. The results showed that the total removal of K by the crops exceeded the amount of total K applied to the soil in all the treatments showing a net negative K balance. This ranged from 3.7 in the plots under NK to 81.7 kg ha-1 year-1 in the N+FYM treated plots. Continuous annual application of recommended doses of NPK+10 t FYM (NPK+FYM) to soyabean resulted in an accumulation (+56 kg K ha-1) of exchangeable K (1 N NH4OAc extractable K) in the 0-45 cm soil depth over the study period, despite the highest average annual uptake of K by the system (150.8 kg ha-1 year-1). However, there was a net depletion of exchangeable K (-80 kg K ha-1) in that soil depth under the NPK treated plots. The results also revealed that the content of non-exchangeable K decreased substantially from 3482 kg ha-1 to 2677 and 2896 kg ha-1 in the 0-45 cm soil layer after 30 years of cropping in the plots under NPK+FYM and NPK treatments, respectively. There was a significant decline in total soil K with the removal of non-exchangeable soil K in the surface (0-15 cm) soil layer (R2=0.526, P0.001, n=36). Thus, long-term application of non-revised recommended fertilizer rates may threaten sustainability of the rainfed continuous soybean-wheat system..
机译:研究了连续30年的连作,施肥和施肥对印度Almora旱作大豆-小麦种植系统下典型Typla Haplaquept土壤中钾(K)平衡,土壤钾库和不可交换钾释放的影响。 。表观的钾平衡被测量为作物添加和去除的钾总量之差。结果表明,在所有处理中,钾的总清除量超过了土壤中施用的总钾量,显示出净负K平衡。介于NK地块的3.7至N + FYM处理地块的81.7 kg ha-1 year-1。每年在大豆上连续施用推荐剂量的NPK + 10t FYM(NPK + FYM)会在0-45厘米土壤深度中积累(+56 kg K ha-1)可交换钾素(1 N NH4OAc可提取钾素)在整个研究期间,尽管该系统的年度平均钾吸收量最高(150.8 kg ha-1 year-1)。但是,在氮磷钾处理的田间,该土壤深度中可交换钾(-80 kg K ha-1)有净消耗。结果还表明,在NPK + FYM和NPK下耕种30年后,0-45厘米土壤层中不可交换钾的含量从3482 kg ha-1降至2677和2896 kg ha-1。治疗,分别。随着土壤表层(0-15厘米)不可交换土壤K的去除,总土壤K显着下降(R2 = 0.526,P <0.001,n = 36)。因此,长期使用未修正的推荐肥料用量可能会威胁到雨养大豆/小麦连续系统的可持续性。

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