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Long-term yield trend and sustainability of rainfed soybean–wheatsystem through farmyard manure application in a sandy loam soil of the Indian Himalayas

机译:在印度喜马拉雅山的沙质壤土上,通过施肥农用肥料,雨水大豆-小麦系统的长期产量趋势和可持续性

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摘要

A long-term (30 years) soybean–wheat experiment was conducted at Hawalbagh, Almora, India to study the effects of organic and inorganic sources of nutrients onudgrain yield trends of rainfed soybean (Glycine max)–wheat (Triticum aestivum) system and nutrient status (soil C, N, Pudand K) in a sandy loam soil (Typic Haplaquept). The unfertilized plot supported 0.56 Mg ha−1 of soybean yield and 0.71 Mg ha−1 of wheat yield (average yield of 30 years). Soybean responded to inorganic NPK application and the yield increased significantly to 0.87 Mg ha−1 with NPK.udMaximum yields of soybean (2.84 Mg ha−1) and residual wheat (1.88 Mg ha−1) were obtained in the plots under NPK + farmyard manure (FYM) treatment, which were significantly higher than yields observed under other treatments. Soybean yields in the plots under the unfertilized and the inorganic fertilizer treatments decreased with time,udwhereas yields increased significantly in the plots under N + FYM and NPK + FYM treatments. At the end of 30 years, total soil organic C (SOC) and total N concentrations increased in all the treatments. Soils under NPK + FYM-treated plots contained higher SOC and total N by 89 and 58% in the 0–45 cm soil layer, respectively, over that of the initial status. Hence, the decline in yields mightudbe due to decline in available P and K status of soil. Combined use of NPK and FYM increased SOC, oxidizable SOC, total N, total P, Olsen P, and ammonium acetate exchangeable K by 37.8, 42.0, 20.8, 30.2, 25.0, and 52.7%, respectively, at 0–45 cm soil layer compared to application of NPK through inorganic fertilizers. However,the soil profiles under all the treatments had a net loss of nonexchangeable K, ranging from 172 kg ha−1 under treatment NK to a maximum of 960 kg ha−1 under NPK +udFYM after 30 years of cropping. Depletion of available P and K might have contributed to the soybean yield decline in treatments where manure was not applied. The studyudalso showed that although the combined NPK and FYM application sustained long-term productivity of the soybean– wheat system, increased K input is required to maintain soil nonexchangeable K level.
机译:在印度阿尔莫拉的Hawalbagh进行了长期(30年)大豆-小麦试验,研究了有机和无机养分来源对雨养大豆(Glycine max)-小麦(Triticum aestivum)系统的 udgrain产量趋势的影响壤质壤土(典型的Haplaquept)中的养分和养分状况(土壤C,N,P udand K)。未施肥的地块支持大豆产量0.56 Mg ha-1和小麦产量0.71 Mg ha-1(30年平均产量)。大豆对无机氮磷钾肥的施用产生了响应,氮磷钾肥使产量显着增加至0.87 Mg ha-1。 ud在NPK +下,该地块的大豆最高产量(2.84 Mg ha-1)和残留小麦(1.88 Mg ha-1)。农家肥(FYM)处理,明显高于其他处理下的产量。未施肥和无机肥料处理下的地块大豆产量随时间下降,而在N + FYM和NPK + FYM处理下的地块大豆产量显着增加。在30年结束时,所有处理均增加了土壤有机碳(SOC)和总氮浓度。经过NPK + FYM处理的样地,在0–45 cm土层中,土壤的SOC和总氮分别比初始状态高89%和58%。因此,单产下降可能是由于土壤有效磷和钾素状况的下降。在0-45厘米土壤层上,NPK和FYM的组合使用可使SOC,可氧化SOC,总N,总P,Olsen P和乙酸铵可交换钾分别增加37.8、42.0、20.8、30.2、25.0和52.7%。与通过无机肥料施用NPK相比。但是,所有处理条件下的土壤剖面都有不可交换的钾素净损失,耕作30年后,在NK处理下为172 kg ha-1,在NPK + udFYM下最大为960 kg ha-1。在不施用肥料的处理中,可用磷和钾的消耗可能导致大豆单产下降。研究 ud还表明,尽管氮磷钾肥和烟粉病的联合施用维持了大豆-小麦系统的长期生产力,但仍需要增加钾素的投入来维持土壤不可交换的钾素水平。

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