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首页> 外文期刊>Biology and Fertility of Soils >Long-term yield trend and sustainability of rainfed soybean–wheat system through farmyard manure application in a sandy loam soil of the Indian Himalayas
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Long-term yield trend and sustainability of rainfed soybean–wheat system 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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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 on grain yield trends of rainfed soybean (Glycine max)–wheat (Triticum aestivum) system and nutrient status (soil C, N, P and 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. Maximum 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, whereas 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 might be 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 + FYM 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 study also 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)系统和小麦籽粒产量趋势的影响。砂质壤土(典型的Haplaquept)中的养分状况(土壤C,N,P和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 (平均30年)。大豆对无机氮磷钾肥的施用响应良好,氮磷钾肥的产量显着提高至0.87 Mg ha?1 。在NPK +农家肥(FYM)处理下,该地块的大豆(2.84 Mg ha?1 )和剩余小麦(1.88 Mg ha?1 )的最大产量均显着高于单产。在其他治疗下观察到。在未施肥和无机肥料处理下,该地块的大豆产量随时间下降,而在N + FYM和NPK + FYM处理下,该地块的大豆产量显着增加。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处理的地块土壤在0–45 cm土层中的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中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。然而,所有处理下的土壤剖面都有不可交换的钾素净损失,范围从NK处理下的172 kg ha?1 到NPK + FYM处理下的最大960 kg ha?1 。多年的种植。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。该研究还表明,尽管氮磷钾和风云素的组合施用可以维持大豆-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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