植物生态学报 ›› 2016, Vol. 40 ›› Issue (10): 1037-1048.DOI: 10.17521/cjpe.2016.0020

所属专题: 碳循环

• 研究论文 • 上一篇    下一篇

川西亚高山流域水碳平衡研究

孙鹏森1,,A;*, 刘宁2, 刘世荣1, 孙阁3   

  1. 1中国林业科学研究院森林环境与保护研究所, 国家林业局森林生态环境重点实验室, 北京 100091
    2School of Veterinary and Life Sciences, Murdoch University, South Street, Murdoch, WA 6150, Australia
    3Eastern Forest Environmental Threat Assessment Center, USDA Forest Service, Raleigh, NC 27606, USA
  • 出版日期:2016-10-10 发布日期:2016-11-02
  • 通讯作者: 孙鹏森

Trade-offs between water yield and carbon sequestration for sub-alpine catchments in western Sichuan, China

Peng-Sen SUN1,*, Ning LIU2, Shi-Rong LIU1, Ge SUN3   

  1. 1Institute of Forest Ecology, Environment and Protection, Chinese Academy of Forestry, Key Laboratory of Forest Ecology and Environment, State Forestry Administration, Beijing 100091, China

    2School of Veterinary and Life Sciences, Murdoch University, South Street, Murdoch, WA 6150, Australia

    3Eastern Forest Environmental Threat Assessment Center, USDA Forest Service, Raleigh, NC 27606, USA
  • Online:2016-10-10 Published:2016-11-02
  • Contact: Peng-Sen SUN

摘要:

森林生态系统的产水量与固碳效益之间存在着一种可交易的平衡关系。基于WaSSI-C水碳耦合模型和趋势分析, 研究了1982-2006年川西杂古脑河上游22个子流域内不同植被类型空间分布对水碳平衡的影响并分析了其水碳耦合关系, 发现: 1)针叶林主导的流域在生长季增加土壤水分入渗的功能明显高于其他植被类型, 但不足以补偿其高蒸散带来的水分消耗, 因而其年平均土壤含水量明显低于高山草甸和混交林类型; 且森林土壤含水量随着森林覆盖率的升高而降低。2) 25年的土壤水分蓄变量的平均值, 高山草甸流域为-44 mm, 混交林为-18 mm, 针叶林为-5 mm, 说明川西亚高山植被的整体维持稳定产水量及其潜力在下降, 其中高山草甸流域下降趋势尤为显著。3)流域产流量和净生态系统生产力具有显著负相关性, 且不同植被组成对固碳和产水效益的转化具有重要影响: 高山草甸主导的子流域具有较高的产水量和较低的固碳能力, 常绿针叶林主导的子流域具有较高固碳能力和较低产水量, 且森林覆盖率越高, 产水量越低。三种植被类型的净生态系统生产力在研究期间均呈现上升趋势, 且高山草甸的上升趋势显著。

关键词: 水碳平衡, 耦合, 水文响应单元, 土壤水分蓄变量, WaSSI-C水碳耦合模型

Abstract:

Aims There is increasing concern on the trade-off between carbon sequestration and water yield of forest ecosystems. Our objective was to explore the effects of vegetation composition on water and carbon trade-off in the sub-alpine watersheds of western Sichuan during 1982-2006.Methods The WaSSI-C, which is an eco-hydrological model with coupled water and carbon cycles, was employed to calculate the key components in water balance and carbon sequestration for the 22 sub-catchments in the upper reaches of Zagunao River. Spearman’s Rho trend analysis was used to examine the trends in runoff and net ecosystem productivity. Important findings Compared with either subalpine meadow or mixed forest dominated catchments, the conifer-dominated catchments had much higher water loss due to high evapotranspiration, and the loss was not offset by its higher soil water infiltration during the growing season. The change in soil water storage for subalpine meadow, mixed forest and coniferous forest are -44 mm, -18 mm and -5 mm, respectively, which indicated significant decline in soil water storage and thus water yield particularly in alpine meadow catchments. Significant negative relationship was found between runoff and net ecosystem productivity, the alpine meadow as the dominant vegetation type showed high water yield and low carbon sequestration, and the conifer-dominant and mixed forest vegetation showed low water yield and high carbon sequestration, moreover, the higher the forest coverage, the lower the water yield. Upward trends in net ecosystem productivity were observed in the three vegetation types during the study period and the alpine meadow type was significant.

Key words: water and carbon trade-off, coupling, hydrological response unit, change in soil water storage, WaSSI-C model