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Study on the Activation of Trace Nutrient Elements in Soil by Freeze-thaw Action

机译:冻融作用研究土壤中痕量营养素的激活研究

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In order to explore the mechanism of action that the freezing-thawing cycle times and freezing temperature to the nutrient forms and enzyme activity of zonal soil(Lou soil,feldspathic sandstone),using indoor freezer to simulate different freezing temperature(20 °C intense frozen and-10 °C weak frozen),with different freezing and thawing cycles(onece and twice).The results shows that the total nitrogen content of the two samples of the freeze-thaw cycle increases,and the increment trend of feldspathic sandstone is more pronounced than Lou soil’s;The increase of potassium content in Lou soil and feldspathic sandstone is 4.7% and 5.3% respectively compared with that before frozen.The effective phosphorus content of 2 kinds of soil in freezing-thawing cycle decreases,and the reducing trend of Lou soil is more pornounced than feldspathic sandstone’s.The peroxidase activity was enhanced by freezing-thawing cycle;however,the activity of urease was decreased.The effect of freezing temperature on the active nutrient and enzyme activity of tillage soil is not significant.
机译:为了探讨冻融循环时间和冻融温度与地狱土壤(娄土,长度砂岩)的营养形式和酶活性的作用机制,使用室内冰柜模拟不同的冷冻温度(20°C强烈冷冻和-10°C弱冷冻),具有不同的冷冻和解冻循环(ONECE和两次)。结果表明,冻融循环的两个样品的总氮含量增加,并且长度砂岩的增量趋势更多比娄土的发音;娄土壤和长期性砂岩的钾含量的增加分别为4.7%和5.3%,而冷冻之前分别为4.7%和5.3%。冻融循环中2种土壤的有效磷含量降低,降低趋势娄土比长期性的砂岩更为色情。通过冷冻解冻循环增强过氧化物酶活性;然而,脲酶的活性降低了。冷冻温度的效果关于耕作土壤的活性营养素和酶活性并不重要。

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