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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:土地回收对农业土壤物理,化学和微生物量和酶活性的影响

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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:目的土地填海层作为耕地面积增加的衡量标准,在过去几十年中正在中国普及。然而,已经很少研究土地回收对土壤碳(C),氮(N)和磷(P)化学计量,微生物量和酶活性的影响。本研究的目的是了解土地接入土壤中的土壤性质。在中国西南部村的降解土壤之前和之后,在0-20,20-40和40-60cm深度下收集物料和方法土壤样品。该样品用于确定土壤堆积密度,孔隙率,水分含量,质地,pH,土壤C,N和P营养性质,微生物量和酶活性。结果与讨论土壤粘土含量增加59.7%,而土壤有机物(SOM),可用磷(AP),总钾,微生物碳(MBC),微生物生物量氮(MBN)以及过氧化酯酶的活性和活性尿素酶分别在0-20cm的土壤中降低49.9,83.4,32.8,20.3和47.9%。 SOM的降低导致土地回收后0-20厘米的MBC和MBN减少。土壤质地具有更好的水和肥料保留能力。中砂(> 0.25mm)含量,AP,C至N的比率和过氧化氢酶的活性降低,但pH和N至P的比例在20-40和40-60cm增加。在土地回收后,粘土含量,中淤泥(0.006-0.01mm),总n和放线菌的数量在40-60厘米处增加。结论土壤营养素和酶活性在0-20厘米处减少,但在土地回收后,土壤总微生物生物量在0-20,20-40和40-60厘米的深度下没有受到干扰。在0-20cm下的土壤有机质减少有助于降低受土地填海活性的MBC和MBN。因此,表土需要更好的管理,以保护土壤营养后的土壤营养和酶活性。

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