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Dynamics of soil microbial biomass and enzyme activities along a chronosequence of desertified land revegetation

机译:荒漠化陆地植物植物季节性近代土壤微生物生物量和酶活性的动态

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Large-scale sand control and afforestation in the Mu Us Sandy land of China have greatly improved soil nutrients and physicochemical properties; however, little is known about their effects on soil biological properties. This study aimed to investigate the changes in soil microbial biomass and enzyme activities and their relationships with soil physicochemical properties during sand land rehabilitation. Soil samples were collected from the shrub and arbor plantations with an age sequence of 20, 30, and 51 years in Yulin at depths of 0-10 cm and 10-20 cm and with semi-fixed sand land selected as a control (0-year-old site). The soil physicochemical and biological properties in the 0-10 cm soil layer were significantly (P 0.001) higher than in the 10-20 cm soil layer for all stand lands. The soil microbial biomass (e.g., microbial carbon and nitrogen) in the 0-10 cm and 10-20 cm layers greatly increased, by 1.58-5.59 times and 2.27-6.07 times, respectively, during the revegetation of shrub and arbor from 20 to 30 years on the control land. During the same period, the activities of soil catalase, urease, alkaline phosphatase and invertase also greatly increased, by 1.27-2.18, 0.59-1.23, 0.48-3.66 and 0.57-2.72 times in shrub land, respectively, whereas they increased by 1.51-2.73, 0.46-2.09, 0.97-2.79 and 2.00-6.65 times in arbor land, respectively, compared with the control land. However, during the 30-51 years of revegetation on the control land, the soil microbial biomass and all enzyme activities remained relatively stable or slightly increased in the arbor land, whereas they were reduced in the shrub land. The soil organic carbon (SOC), dissolved organic carbon (DOC), total nitrogen (TN) and available nitrogen (AN) contents also greatly increased after revegetation in the control land. Principal component analysis (PCA) also confirmed that most of the chemical and biological properties were influenced by the afforestation and showed coordinated variation between the analyzed parameters. Moreover, redundancy analysis (RDA) showed that the soil microbial biomass and enzyme activities were correlated with the changes of SOC, DOC and TN, whereas they were negatively correlated with the bulk density, pH and total potassium. Therefore, we concluded that revegetation by the establishment of both shrub and arbor plantations significantly improved soil biological properties. Moreover, SOC, DOC and TN were regarded as the key factors in the enhancement of soil biological activity during desertified land revegetation in the Mu Us Sandy land of China.
机译:中国澳洲沙地的大型沙子控制和造林极大地改善了土壤养分和物理化学特性;然而,对它们对土壤生物学性质的影响很少。本研究旨在探讨土壤微生物化学生物量和酶活性的变化及其在沙地康复期间与土壤理化性质的关系。从灌木和树木植物中收集土壤样品,玉林为20,30和51岁,深度为0-10厘米和10-20厘米,并选择半固定沙地作为对照(0-岁月的网站)。在0-10cm的土壤层中的土壤物理化学和生物学性质显着(P <0.001)高于10-20cm的土地层。在0-10厘米和10-20cm层中,土壤微生物的土壤微生物生物量(例如微生物碳和氮气)分别在灌木和灌木的再灌注期间分别大大增加1.58-5.59倍和2.27-6.07倍对照土地30年。在同一时期,土壤过氧化氢酶,释放酶,碱性磷酸酶和转化酶的活性也大大增加,分别在灌木土地中分别大大增加,0.59-1.23,0.59-1.23,0.48-3.66和0.57-2.72次,而它们增加了1.51- 2.73,0.46-2.09,0.97-2.79和2.00-6.65次分别与控制土地相比。然而,在对照土地的30-51岁之间,土壤微生物生物量和所有酶活性在灌木陆地上保持相对稳定或略微增加,而它们在灌木土地上减少。土壤有机碳(SOC),溶解有机碳(DOC),总氮(TN)和可用氮(AN)含量在对照土地中的再灌注后也大大增加。主成分分析(PCA)还证实,大多数化学和生物学性质受到造林的影响,并在分析的参数之间显示了协调的变化。此外,冗余分析(RDA)显示土壤微生物量和酶活性与SoC,Doc和Tn的变化相关,而它们与堆积密度,pH和总钾负相关。因此,我们得出结论,通过建立灌木和Arbor种植园的重新植被显着改善了土壤生物学性质。此外,SOC,DOC和TN被认为是中国澳洲沙地泥土陆地植物园土壤生物活性增强的关键因素。

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