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Available K and Total Organic C Accumulation in Soil with the Utilization Ages of the Vegetable Greenhouses in the Suburb of Shenyang

机译:沉阳郊区蔬菜温室利用年龄的土壤中可用K和土壤中的总积累

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The amount of available potassium, total organic C and pH in different utilization age (0, 1, 5, 13-year) vegetable greenhouses soil was examined in Damintun Town of Shenyang. The results showed that the amount of soil available K in all utilization ages vegetable greenhouses decreased with the soil depth. For all the samples, the amount of available potassium (AK) and total organic C (TOC) in the 0-40 cm layer was higher than that in the 40-120 cm. In the 0-20cm layer, the amount of available K in 13-year vegetable greenhouse soil is 3.4 times higher than that in the bare land, while the amount of available K in 1-year vegetable greenhouse is only 1.26 times the than the bare land. The amount of soil total organic C was the biggest in the surface soil (0-20cm) and was in the deep soil (80-120 cm) in the 5-year and 13-year vegetable greenhouse, respectively. It implied that long-term continuous organic carbon input from chemical fertilizer and organic manure could cause total organic C translocation into deep soil layers. Soil pH in the greenhouse has little changed, which indicated that continuous addition of fertilizer has little effect on it.
机译:在沉阳达顿镇检验了不同利用年龄(0,1,5,13岁)植物温室土壤中可用钾,总有机C和pH值。结果表明,所有利用率K中的土壤钾量随着土壤深度降低蔬菜温室。对于所有样品,0-40cm层中的可用钾(AK)和总有机C(TOC)的量高于40-120cm。在0-20cm层中,13年蔬菜温室土壤中可用的量高出3.4倍,裸机含量高3.4倍,而1年蔬菜温室的可用金额仅为1.26倍的裸露土地。土壤总有机C的数量分别是表面土壤(0-20cm)中最大,分别在5年和13年蔬菜温室中深土(80-120厘米)。它暗示化肥和有机粪肥的长期连续有机碳投入可能导致整个有机C易位进入深层土壤层。温室中的土壤pH值几乎没有变化,这表明连续添加肥料对其影响不大。

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