[Characteristics of Stable Isotopes and Moisture Sources of Two Typical Precipitation Events in Lanzhou City].

To better understand the isotope variations on a short time scale, this study focused on a long-term rainfall event with light precipitation (June 26-27) and a short-term one with heavy precipitation (July 28) in Lanzhou City in the summer of 2019. Combined with HYSPLIT model, samples collected during a continuous precipitation event every 10 min and 30 min were analyzed to explore the characteristics and mechanism of stable hydrogen and oxygen isotopes in precipitation. The results indicate that the effect of sub-cloud secondary evaporation makes the slope of the sequential meteoric water line (SMWL) smaller at the beginning of the rainfall event. Most of the continuous sampling points are distributed above the global meteoric water line (GMWL) and local meteoric water line (LMWL). Moreover, the deuterium excess is larger than the local average annual deuterium (8.13), indicating that the samples have experienced moisture recycling to a certain extent. During two consecutive days (June 26-27) of rainfall, the variations in oxygen isotope δ18O did not follow the effect of precipitation amount; the precipitation δ18O of the first day was "L" shaped, and it fluctuated the next day. On July 28, δ18O steadily decreased, and the range of δ18O exceeded 9‰. On June 26, the moisture transport path was short at the height of 500 m and on June 27 local evaporation was the main pathway. On July 28, with a relatively stable air mass, the moisture source of the entire precipitation event did not change significantly, neither did the isotope value. Therefore, for a single precipitation event on a short time scale, the difference in moisture sources is one of the reasons for isotope variations.

[Environmental selection and dispersal limitation drive the assemblage of bacterial community in temperate forest soils]. / 环境选择和扩散限制驱动温带森林土壤细菌群落的构建.

Environmental selection and dispersal limitation are two basic processes underlying community assembly. The relative importance of those two processes differs across scales, community identities, and community types. The processes responsible for structuring microbial communities in soil of temperate subalpine forest are poorly understood. Here, we investigated the relationship between soil bacterial community structure and environmental factors, and quantified the relative role of edaphic factors, vegetation, and spatial variables in shaping the structure of six soil bacterial communities (LpMC1, LpMC2, PwMC, PmMC, PtMC, and BMC) in five forest types including Larix principis-rupprechtii, Picea wilsonii, Picea meyeri, Pinus tabulaeformis, and Betula platyphylla in Pangquangou Nature Reserve by using PCR-DGGE technology. Our results showed that the structure and biodiversity of bacterial communities were significantly different among six communities. The biodiversity of bacterial community were higher in LpMC2 and PtMC, lowest in PmMC, and highest in LpMC1. Soil environmental factors, such as pH, soil water content, total carbon, total nitrogen, soil organic matter, available phosphorous, and soil enzymes, were significantly correlated with biodiversity and structure of soil bacterial community. The beta diversity of bacterial communities were significantly correlated with geographic distance, indicating the influence of dispersal limitation on the structure of bacterial community. The order of driving force on the structure of bacterial community was edaphic factors (0.27), spatial factor (0.19) and vegetation (0.15) in six samples. Using regional soil microbes from 10 samples around reserve as source community, results from the microcosm experiments showed that the edaphic factors were the predominant driving factors (0.35) on structure of artificial dispersal bacterial community, while the high diversity of source microbial community affected the structure of microcosm soil. In summary, at local scale, environmental selection predominantly determined the structural and biodiversity of soil bacterial communities in temperate subalpine forest, while dispersal limitation played a significant role. Such a result indicated that deterministic processes and stochastic processes played important roles in shaping the structure of soil bacterial community at local scale, with the former having the leading role. The composition of dispersal soil bacteria community was source-dependent but also modulated by local environmental selection.