首页|期刊导航|林业科学|毛乌素沙地地下水埋深驱动樟子松水分利用趋深适应与效率提升

毛乌素沙地地下水埋深驱动樟子松水分利用趋深适应与效率提升OA

Water Table Depth Drives Deepening Adaptation and Efficiency Enhancement in Water Use of Pinus sylvestris var.mongolica in the Mu Us Sandy Land

中文摘要英文摘要

[目的]探究毛乌素沙地樟子松人工林的水分利用策略,分析地下水埋深梯度与降水年型交互作用下樟子松水分来源和水分利用效率的动态变化规律及差异,为旱区人工林的林分结构优化和可持续经营提供科学依据.[方法]以毛乌素沙地初始地下水埋深分别为 4 m(WTD4)、9 m(WTD9)和 13 m(WTD13)的樟子松人工林为研究对象,采用稳定同位素(δ2H、δ18O和δ13C)技术结合MixSIAR模型,分析欠水年和平水年樟子松水分利用策略对地下水埋深的响应.[结果]1)随着地下水埋深增加和土壤含水量显著降低(从WTD4 的 0.029 g·g-1 降至WTD13的0.022 g·g-1),樟子松 60~200 cm土层的根质量密度占其 0~200 cm土层总根质量密度的比例增加(从WTD4 的17.3%增至WTD13 的 24.0%);2)不同地下水埋深下的樟子松在相同时期的水分来源存在差异,同一地下水埋深下的樟子松在不同降水年型的水分来源也有差别,欠水年对浅层土壤水的利用比例较平水年降低;3)整个观测期内,樟子松主要依赖深层(WTD4 为 60~360 cm,WTD9 和WTD13 为 60~400 cm)土壤水,其贡献率随地下水埋深增加逐渐上升(从WTD4 的 34.6%增至WTD13 的 52.6%),水分利用效率同步提升(从WTD4 的 102.7 μmol·mol-1 增至WTD13 的106.9 μmol·mol-1);4)樟子松的株高、胸径、冠幅和林分密度在地下水深埋区(WTD13)均显著低于浅埋区(WTD4).[结论]地下水埋深和降水年型通过影响土壤水分状况,驱动樟子松形成"根系深扎-水源深取-效率提升"的协同适应策略,但深埋区的樟子松生长受限.植被恢复过程中,需依据地下水埋深变化,实施差异化的植被配置和密度调控措施,有效减少植被建设对深层土壤水的过度消耗,促进生态建设的可持续发展.

[Objective]This study aims to explore the water use strategies of Pinus sylvestris var.mongolica plantations in the Mu Us Sandy Land,and analyze the dynamic variation patterns and differences in water sources and water use efficiency of P.sylvestris var.mongolica under the interaction of water table depth gradients and hydrologic year types,so as to provide a scientific basis for the stand structure optimization and sustainable management of artificial forests in arid areas.[Method]This study targeted P.sylvestris var.mongolica plantations with initial water table depth(WTD)of 4 m(WTD4),9 m(WTD9)and 13 m(WTD13).Stable isotope techniques(δ2H,δ18O,and δ13C)combined with the MixSIAR model were employed to analyze the response of P.sylvestris var.mongolica water-use strategies to WTD during both dry years and normal precipitation years in the Mu Us Sandy Land.[Result]1)With the increase in WTD and the significant decrease in soil water content(decreasing from 0.029 g·g-1 in WTD4 to 0.022 g·g-1 in WTD13),the proportion of the root mass density of P.sylvestris var.mongolica in the 60-200 cm soil layer to the total root mass density in the 0-200 cm soil profile increased(increasing from 17.3%in WTD4 to 24.0%in WTD13).2)Water sources of P.sylvestris var.mongolica differed under different WTD during the same period,and varied across different hydrologic years within the same WTD.The proportion of shallow soil water utilized by P.sylvestris var.mongolica in dry years was lower than that in normal years.3)Throughout the observation period,P.sylvestris var.mongolica primarily relied on deep soil water(WTD4:60-360 cm;WTD9 and WTD13:60-400 cm),and its contribution rate gradually increased with the deepening of the WTD(increasing from 34.6%in WTD4 to 52.6%in WTD13).Concurrently,the water use efficiency also increased(increasing from 102.7 μmol·mol-1 in WTD4 to 106.9 μmol·mol-1 in WTD13).4)The height,diameter at breast height(DBH),crown width,and stand density of P.sylvestris var.mongolica in areas with deep water table depth(WTD13)were significantly lower than those in areas with shallow water table depth(WTD4).[Conclusion]WTD and hydrologic year type drive P.sylvestris var.mongolica to develop a synergistic adaptation strategy of"root deepening-deeper water sourcing-enhanced water-use efficiency"by influencing soil water conditions,but growth becomes constrained in areas with deeper WTD.Based on this,during the vegetation restoration process,it is necessary to implement different vegetation allocation and density regulation measures according to the changes in water table depth,so as to effectively reduce the excessive consumption of deep soil water by vegetation construction and promote the sustainable development of ecological construction.

梁璇;王力

西北农林科技大学资源环境学院 杨凌 712100西北农林科技大学资源环境学院 杨凌 712100||西北农林科技大学水土保持科学与工程学院 杨凌 712100||中国科学院水利部水土保持研究所水土保持与荒漠化整治全国重点实验室 杨凌 712100

农业科技

毛乌素沙地稳定同位素水分来源水分利用效率降水年型MixSIAR

Mu Us Sandy Landstable isotopewater use sourceswater use efficiencyhydrologic year typeMixSIAR

《林业科学》 2026 (2)

53-65,13

国家自然科学基金项目(42171043,42377318).

10.11707/j.1001-7488.LYKX20250426

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