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生态学报  2011 

Responses of soil enzyme activities and microbial biomass N to simulated N deposition in Gurbantunggut Desert
古尔班通古特沙漠土壤酶活性和微生物量氮对模拟氮沉降的响应

Keywords: N deposition,soil enzyme,microbial biomass N,Gurbantunggut desert
氮沉降
,土壤酶,微生物量N,古尔班通古特沙漠

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Abstract:

Nitrogen (N) deposition influences microbial decomposition and nutrient transformation rates by affecting the activities of microbial properties, such as soil enzymes, microbial biomass and structure of the microbial community. In desert ecosystems, where water and N are two major limiting factors for biological activity, minimal nutrient dynamics are linked to comparatively large changes. In this paper, an in situ experiment was conducted in Gurbantunggut desert to explore the effects of N deposition on soil enzyme activities and microbial biomass N. Sixty 8 m 8 m plots were established in the inter-dune area, with each plot having similar vegetation and a biological soil crust cover. Six N fertilizer treatments (N0, N0.5, N1, N3, N6 and N24 denoting 0, 0.5, 1.0, 3.0, 6.0 and 24 g N m-2 a-1, respectively) were conducted, , with ten replicates for each treatment. Nitrogen was applied at the ratio of 2:1 for NH4 -N:NO3?-N (informed in NH4NO3 and NH4Cl), consisting with ratio of the main N components in deposition in Urumqi. Soil samples were collected in May 2009 from 24 of the 60 plots with 4 replicates for each treatment (6 N treatments 4 replicates). Soil samples were taken from two layers (0?5 cm and 5?10 cm) and transported to laboratory quickly. The results showed that original vertical distribution patterns of nutrient, soil enzyme and microbial biomass were not changed by N addition. Soil organic C, total N, total P, available P and available N pools were greater in the 0?5 cm soil layer than in the 5?10 cm layer, regardless of N addition rates. The polyphenol oxidase and peroxidase activities in 0?5 cm soil layer were 11.5% ? 29.1% and 1.4% ? 14.2% lower than those in 5?10 cm soil layer, respectively. However, the activities of invertase, urease, alkaline phosphatase (AlP) and microbial biomass N in the 0?5 cm soil layer were 4.3% ? 98.1%, 45.3% ? 119.0%, 76.1% ? 138.1% and 77.5% ? 162.4% higher compared with the 5?10 cm layer, respectively. The soil enzyme activities and microbial biomass N were more sensitive to N addition in the 0?5 cm layer than in the 5?10 cm layer. Although low and moderate N levels (N0.5, N1 and N3) have marginal effects on oxidative enzyme activities in the 0?5 cm layer, high N levels (N6 and N24) reduced the activities of oxidative enzyme. With respect to control (N0), the activities of polyphenol oxidase and peroxidase were 22.4% and 12.1% lower under N24. In contrast, the oxidative enzyme activities in the 5?10 cm layer were not sensitive to N addition. With the increase in N addition, both the invertase and AlP activities in the two layers increased at low N addition levels, then they decreased at high N levels. Compared with control, N1 and N3 increased invertase activities in the 0?5 cm layer by 49.6% and 72.3%, respectively; and by 8.6% and 11.4% in the 5?10 cm layer, respectively. AlP activities in the 0?5 cm layer tended to increase at the low N levels (i.e., N0.5, N1 and N3). Highest increasing rate of 4

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