|国家预印本平台
首页|微地形对高寒固沙植物水分利用特征的影响

微地形对高寒固沙植物水分利用特征的影响

中文摘要英文摘要

水是植物生存最主要的限制因子,对沙区植物水分利用的研究已成为沙地生态保护和植被恢复的关键。本文以青海湖湖东沙地3种典型固沙植物——樟子松、小叶杨、沙棘为研究对象,基于氢氧稳定同位素技术(δ18O和δD),结合IsoSource模型,对微地形影响下的各潜在水源(不同层次的土壤水)及植物主要水分来源进行分析。研究结果表明:(1)土壤含水量具有微地形差异,表现在迎风坡低地土壤含水量高于沙丘顶部和迎风坡中部,且9月土壤含水量处在最高值。(2)木质部水的δ18O值在不同微地形条件下具有树种差异性,樟子松在迎风坡低地的δ18O值最小,而沙棘和小叶杨在迎风坡中部的δ18O值最小。(3)不同植物的主要水分来源具有较为明显的季节差异,6月樟子松和沙棘在不同微地形条件下均以深层土壤水为主要水分来源,而小叶杨在沙丘顶部主要利用深层土壤水,在迎风坡中部和低地对中层土壤水的利用较大,但随着降水量的增加,9月各树种转而主要利用浅层和中层土壤水。总而言之,高寒沙地固沙植物的水分利用模式受微地形条件的影响,且不同物种对降水表现出不同程度的响应。

Water is the most important limiting factor for plant survival, and the study of plant water utilization in desert has become the key to ecological protection and vegetation restoration program. In the sandy land at east shore of the Qinghai Lake, we focuses on three typical sand-fixing plants (Pinus syivestris var.mongolica, Populus simonii and Hippophae rhamnoides) as the research object. The potential water source (different levels of soil water) and the main water sources of plants under the influence of micro-topography were analyzed by hydrogen and oxygen stable isotope technology (18O and D) and IsoSource isotope mixing model. The results show that: (1)the soil water content has micro-topography differences, manifested in the lower soil water content on the windward slope being higher than that on the top of the sand dunes and the middle of the windward slope, and the soil water content is at its highest value in September. (2)the 18O value of xylem water is different in tree species under different micro-topographic conditions. The 18O values of P. syivestris in the lowland of windward slope are the lowest, while those of H. rhamnoides and P. simonii are the lowest in the middle of windward slope. (3)there are significant seasonal differences in the main sources of water for different plants. In June, both P. syivestris and H. rhamnoides used deep soil water as the main source of water under different micro-topographic conditions, while P. simonii mainly used deep soil water at the top of sand dunes. Middle-layer soil water is more utilized in the middle and lowland of windward slope, but with the increase of precipitation, various tree species turned to mainly use shallow and middle soil water in September. In summary, the water use patterns of sand-fixing plants in alpine sandy land are influenced by micro-topographic conditions, and different species showed different degrees of response to precipitation.

范明彦、周 海、田丽慧

10.12074/202403.00036V1

农业科学研究环境科学基础理论自然地理学

高寒沙地稳定同位素微地形植物水分来源IsoSource模型

alpine sandy landstable isotopemicro-topographyplant water sourceIsoSource model

范明彦,周 海,田丽慧.微地形对高寒固沙植物水分利用特征的影响[EB/OL].(2024-03-01)[2025-08-02].https://chinaxiv.org/abs/202403.00036.点此复制

评论