Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.
Key Laboratory of Forest Ecology and Environment of State Forestry and Grassland Administration, Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Beijing 100091, China.
Sci Total Environ. 2019 Mar 25;658:1514-1522. doi: 10.1016/j.scitotenv.2018.12.171. Epub 2018 Dec 12.
Changes in global precipitation patterns would make wet regions more humid and extreme precipitation events occur frequently, followed by widespread flooding. Riparian forests are more capable of withstanding floods than inland forests because they are frequently exposed to short-term flooding events. Although many previous studies have investigated the soil water dynamics of terrestrial forests, little is known about how the soil water of riparian forests responds to different amounts of rainfall and which factors mainly regulate the soil water-holding capacity. Here, we employed stable hydrogen isotope to explore the contribution of different magnitudes of rainfall (7.9, 18.6 and 34.1 mm) to the soil water in two types of riparian forests (pure vs. mixed stand of Populus deltoides) in the middle-lower reaches of the Yangtze River, China. We further used structure equation modelling to determine the relative importance of soil properties and vegetation biomass in affecting the contribution of different magnitudes of rainfall to soil water. Our results revealed that there was no significant difference between these two stand types in the contributions of light and moderate rainfall to soil water, while the contribution of heavy rainfall to soil water (CHRSW) in mixed stand was significantly higher than that in pure stand (74.3% vs. 62.9%), suggesting that mixed stand soil has higher water-holding capacity than pure stand soil. Furthermore, soil properties were the best predictor affecting CHRSW, which explained 68% and 59% of the variation in the CHRSW on the 1st and 8th days after rainfall, respectively. Moreover, the root biomass could indirectly affect the CHRSW. Overall, mixed stand soil had a greater capacity in intercepting and storing rainwater than pure stand soil, implying that the mixed stand plantation, rather than the pure stand, should be recommended in riparian forest restoration projects that aim to improve their capacity for alleviating floods.
全球降水格局的变化将使湿润地区更加潮湿,极端降水事件频繁发生,继而导致广泛的洪水泛滥。河岸林比内陆林更能承受洪水,因为它们经常受到短期洪水事件的影响。尽管许多先前的研究已经调查了陆地森林的土壤水分动态,但对于河岸林的土壤水分如何响应不同降雨量以及哪些因素主要调节土壤持水能力知之甚少。在这里,我们使用稳定的氢同位素来探索不同降雨量(7.9、18.6 和 34.1 mm)对中国长江中下游两种河岸林(纯白杨林与白杨混合林)土壤水分的贡献。我们进一步使用结构方程模型来确定土壤性质和植被生物量在影响不同降雨量对土壤水分的贡献方面的相对重要性。我们的结果表明,这两种林分类型在轻雨和中雨对土壤水分的贡献方面没有显著差异,而混合林分的大雨对土壤水分的贡献(CHRSW)明显高于纯林分(74.3%对 62.9%),表明混合林分土壤具有更高的持水能力比纯林分土壤。此外,土壤性质是影响 CHRSW 的最佳预测因子,分别解释了降雨后第 1 天和第 8 天 CHRSW 变化的 68%和 59%。此外,根生物量可以间接影响 CHRSW。总的来说,混合林分土壤具有更大的截留和储存雨水的能力,这意味着在河岸林恢复项目中,应该推荐混合林分种植,而不是纯林分种植,以提高其缓解洪水的能力。