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嘉峪关草湖湿地土壤水分含量与植被盖度的空间格局

段凯祥1,2,张松林1,2*,赵成章1,2,彭鑫波1,隽伟超1,杨鹏1,杨晔1,姜右锦1,骆艳1   

  1. (1西北师范大学地理与环境科学学院, 兰州 730070;2甘肃省湿地资源保护与产业发展工程研究中心, 兰州 730070)
  • 出版日期:2019-03-10 发布日期:2019-03-10

Spatial pattern of soil moisture and vegetation coverage in Cao Lake wetland.

DUAN Kai-xiang1,2, ZHANG Song-lin1,2*, ZHAO Cheng-zhang1,2, PENG Xin-bo1, JUAN Wei-chao1, YANG Peng1, YANG Ye1, JIANG You-jin1, LUO Yan1   

  1. (1Institute of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China; 2Research Center of Wetland Resources Protection and Industrial Development Engineering of Gansu Province, Lanzhou 730070, China).
  • Online:2019-03-10 Published:2019-03-10

摘要: 土壤水分含量是植被格局形成和演变的主要因素。探讨干旱区盐沼湿地土壤水分含量的空间异质性,有助于揭示湿地植物的环境适应机理和土壤水分与湿地植物的相互关系。本研究利用地统计学方法建立了嘉峪关草湖湿地3个不同长势(植被盖度高、中、低)假苇拂子茅(Calamagrostis pseudophragmites)单优种群斑块土壤(0~90 cm)水分含量与植被盖度的变异函数理论模型,以Kriging插值法绘制了土壤水分含量与植被盖度的空间格局分布图,采用Moran I系数确定了湿地土壤水分含量和植被盖度的空间自相关关系,分析了湿地土壤水分含量与植被盖度的空间异质性及其相互作用关系。结果表明:草湖湿地样地土壤的平均含水量为湖边>干湖>沙丘间平地;盐分平均含量为干湖>湖边>沙丘间平地;在斑块尺度上,土壤水分含量和植被盖度均符合正态分布;各层土壤水分含量和假苇拂子茅盖度的空间结构均具有明显的斑块状分布特点,且均存在高度的空间异质性;3个样地各层土壤的水分含量和植被盖度均具有空间正相关性和空间集聚特征,60~90 cm土壤水分含量的空间集聚强度较0~30和30~60 cm土层更大,湖边样地植被盖度空间集聚特征更明显。假苇拂子茅最大限度利用土壤水分资源,提高了其对干旱生境的适应力,且在一定程度上影响小尺度土壤水分的空间分布格局。

关键词: 土壤微生物, 土壤酶, 营养元素, 枯枝落叶, 自肥能力

Abstract: Soil moisture is a major factor driving the formation and evolution of vegetation patterns. The exploration of spatial heterogeneity of soil moisture in salt marsh wetland in arid area is helpful for revealing the environmental adaptation of wetland plants and the interaction mechanism between soil moisture and wetland plants. In this study, the variogram models of soil moisture content (0-90 cm) and vegetation coverage were established according to the vegetation cover conditions (high, medium, and low) of three Calamagrostis pseudophragmitesdominated population patches in the wetland of Cao Lake, Jiayuguan City, using the geostatistical method. The spatial distributions of soil moisture and vegetation coverage were mapped with the Kriging interpolation method, and the spatial autocorrelation properties of soil moisture and vegetation coverage in the wetland were determined by the Moran’s I coefficients. Finally, the spatial heterogeneity of soil moisture and vegetation cover in wetland and their interaction relationships was analyzed. Results showed that soil water contents in different sites of the Cao Lake wetland were in order of lakeside>dry lake>flat land between dunes, and salt content was in order of dry lake>lakeside>flat land between dunes. On the patch scale, soil moisture and vegetation cover were in line with the normal distribution model. The spatial structure of soil water content in each layer and vegetation cover of C. pseudophragmites in the three sites all had an obvious patch-like distribution and exhibited high degrees of spatial heterogeneity. The spatial distribution of soil moisture contents and vegetation coverage in all three plots had positive correlations and agglomeration characteristics. The spatial agglomeration intensity of soil moisture content for the 60-90 cm soil layer was larger than those of 0-30 and 30-60 cm soil layers, and the spatial clustering characteristics of vegetation cover was more obvious in the lakeside plot. Therefore, C. pseudophragmites maximized the use of soil water resources, and thus improved its adaptability to drought habitats, which, to a certain extent, affected the spatial distribution of soil moisture on small scale.