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Effects of land reclamation on the physical, chemical, and microbial quantity and enzyme activity properties of degraded agricultural soils

机译:开垦对退化农业土壤理化,微生物量和酶活性特性的影响

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Purpose Land reclamation, as a measure of increasing cultivated land area, is being popularized in China in the past decades. However, the impact of land reclamation on soil carbon (C), nitrogen (N), and phosphorus (P) stoichiometry, microbial quantity, and enzyme activities has been rarely studied. The objective of this study was to know how land reclamation affected soil properties in agricultural soils. Materials and methods Soil samples were collected at 0-20, 20-40, and 40-60 cm depths before and after land reclamation of degraded soils in a village of southwest China. The samples were used to determine soil bulk density, porosity, moisture content, texture, pH, soil C, N, and P nutrient properties, microbial quantity, and enzyme activities in agricultural soils. Results and discussion The soil clay content was increased by 59.7%, while the soil organic matter (SOM), available phosphorus (AP), total potassium, microbial biomass carbon (MBC), microbial biomass nitrogen (MBN), and activities of catalase and urease enzymes were decreased by 49.9, 83.4, 32.8, 20.3, and 47.9%, respectively, at 0-20 cm of the soil. The decrease of SOM contributed to the decrease of MBC and MBN at 0-20 cm after the land reclamation. The soil texture had better capacity of water and fertilizer retention. Medium sand (> 0.25 mm) content, AP, the ratio of C to N, and activities of catalase were decreased, but pH and the ratio of N to P were increased at 20-40 and 40-60 cm. The clay content, medium silt (0.006-0.01 mm), total N, and quantity of fungi and actinomycetes were increased at 40-60 cm after the land reclamation. Conclusions Soil nutrient and enzyme activities at 0-20 cm were decreased but soil total microbial biomass was not disturbed at 0-20, 20-40, and 40-60 cm depths, after the land reclamation. The decrease of soil organic matter at 0-20 cm contributed to the decrease of MBC and MBN affected by land reclamation activities. Therefore, topsoil requires better management to preserve soil nutrients and enzyme activities after land reclamation.
机译:目的在过去的几十年中,作为增加耕地面积的一种手段,开垦土地正在中国普及。但是,很少研究土地开垦对土壤碳(C),氮(N)和磷(P)的化学计量,微生物数量和酶活性的影响。这项研究的目的是了解土地开垦如何影响农业土壤的土壤特性。材料和方法在中国西南一个村庄的土地复垦之前和之后,分别在0-20、20-40和40-60 cm深度采集土壤样品。样品用于确定土壤的容重,孔隙率,水分含量,质地,pH,土壤碳,氮和磷的养分特性,微生物数量以及农业土壤中的酶活性。结果与讨论土壤黏土含量增加了59.7%,而土壤有机质(SOM),有效磷(AP),总钾,微生物生物量碳(MBC),微生物生物量氮(MBN)以及过氧化氢酶和在土壤0-20厘米处,尿素酶减少了49.9%,83.4%,32.8%,20.3和47.9%。 SOM的降低有助于开垦后0-20 cm处MBC和MBN的降低。土壤质地具有更好的保水保肥能力。在20-40和40-60 cm处,中砂(> 0.25 mm)含量,AP,碳氮比和过氧化氢酶活性降低,但pH和氮磷比增加。土地开垦后,粘土含量,中等淤泥(0.006-0.01 mm),总氮以及真菌和放线菌的数量增加。结论开垦后0-20 cm深度土壤养分和酶活性下降,但0-20、20-40和40-60 cm深度土壤总微生物量不受干扰。 0-20 cm土壤有机质的减少导致了开垦活动对MBC和MBN的减少。因此,表土需要更好的管理,以在土地开垦后保留土壤养分和酶活性。

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