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Soil Degradation due to Potassium Mining under Intensive Cropping in Uttaranchal Hills

机译:北大山丘陵集约耕作下钾肥开采造成的土壤退化

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An investigation was undertaken in the Long Term Fertilizer Experiment (LTFE) located on an inceptisol in VPKAS Farm at Hawalbagh, Almora district of Uttaranchal Hills, with a specific objective of monitoring the changes in total soil K reserve and K availability under continuously followed varying nutrient input systems in 25 crop cycles of an intensive soybean-wheat rainfed cropping system. Potassic fertilizer application for most of the rainfed crops are practically nil because of higher total potassium soil K reserve due to dominance of micacious soil minerals. Though the soils of this long-term experiment are high in total K (4500 mg kg~(-1)) but low in NH_4 OAC-K (53.3 mg kg~(-1)) and responds irregularly since monsoon controls the release of potassium from soil minerals. The depletion of K was found in treatments receiving no K fertilization and even with the optimum K fertilization dose which needs verification after 25 years of cropping. The N+FYM treatment which is called farmers treatment in the region, showed mining of soil K reserve. Possible reasons are discussed in this paper.
机译:在位于Uttaranchal Hills Almora区Hawalbagh Hawalbagh的VPKAS农场的Inceptisol上进行的长期肥料实验(LTFE)进行了一项调查,其特定目的是在不断变化的养分情况下监测土壤总钾储量和钾有效性的变化。密集的大豆-小麦雨育作物种植系统在25个作物周期中的输入系统。大部分雨养作物的钾肥施用量几乎为零,这是因为由于云母土壤矿物质占主导地位,钾肥总钾储量较高。尽管该长期实验的土壤中总K较高(4500 mg kg〜(-1)),但NH_4 OAC-K较低(53.3 mg kg〜(-1)),并且由于季风控制了土壤的释放,因此响应不规则。土壤矿物质中的钾。在没有钾肥施用的情况下,甚至在最佳钾肥施用量的情况下,都发现钾的消耗,这需要在种植25年后进行验证。 N + FYM处理在该地区被称为农民处理,表明了土壤钾储量的开采。本文讨论了可能的原因。

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