Spatial heterogeneity of soil chemical properties at fine scales induced by Haloxylon ammodendron (Chenopodiaceae) plants in a sandy desert

Ecological Research - Tập 26 - Trang 385-394 - 2010
Congjuan Li1,2, Yan Li1, Jian Ma1
1Fukang Station of Desert Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, People’s Republic of China
2Graduate University of Chinese Academy of Sciences, Beijing, People’s Republic of China

Tóm tắt

Spatial heterogeneity is considered a ubiquitous feature in natural ecosystems. Fertile islands represent a typical example for such heterogeneity in desert ecosystems. The soil pH and salinity also show significant heterogeneity in fertile islands. To investigate the distribution of soil salinity and nutrients around individual shrubs and the major factors influencing their distribution, an experiment was conducted at the scale of the rhizosphere, root system, and individual for Haloxylon ammodendron (C. A. Mey.) Bunge (Chenopodiaceae) shrub in the Gurbantünggüt Desert. Specifically, the heterogeneity of the following soil chemical parameters was evaluated: pH, electrical conductivity (EC), soil organic carbon (SOC), total nitrogen (TN), and available phosphorus (AP). The chemical properties of the shrub stemflow were also evaluated to determine its contribution to the formation of fertile islands and the distribution of soil salinity. The results revealed great variance in the soil pH and EC at the rhizosphere and root system scales, indicating that a single root or root system exerts a great effect on soil pH and salinity. At the individual scale, the content of SOC, TN, and AP was significantly enriched in the layers adhering to the taproot, and this enrichment extended 20–40 cm from the taproot. Conversely, the soil pH and EC were significantly lower from the taproot to 10–25 cm away from the root, indicating that the fertile island is also an island of low alkalinity/salinity. Comparison of the chemical properties of stemflow and bulk precipitation revealed a higher content of chemical elements (except pH and CO3 2−) in the stemflow, indicating that the fertile island and lower pH and EC in this island were likely formed by the effects of stemflow. Specifically, stemflow brings in water and nutrients, while reducing the salt levels. Overall, the high nutrients and low alkalinity/salinity island created around the taproot favor the growth of the plants.

Tài liệu tham khảo

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