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生态学杂志 ›› 2023, Vol. 42 ›› Issue (6): 1474-1483.doi: 10.13292/j.1000-4890.202306.004

• 研究报告 • 上一篇    下一篇

气候变化和人类活动对干旱区垂直自然带NPP的影响

陈炳铭1,2,3,赵善超4,孙丰华1,2,3,王玉刚1,2,3*


  

  1. 1中国科学院新疆生态与地理研究所, 荒漠与绿洲生态国家重点实验室, 乌鲁木齐 830011; 2中国科学院阜康荒漠生态系统国家站, 新疆阜康 831505; 3中国科学院大学, 北京 100049; 4新疆维吾尔自治区天然林保护中心, 乌鲁木齐 830001)

  • 出版日期:2023-06-10 发布日期:2023-06-05

Impacts of climate change and human activities on the NPP of vertical natural belts in arid zones.

CHEN Bingming1,2,3, ZHAO Shanchao4, SUN Fenghua1,2,3, WANG Yugang1,2,3*   

  1. (1State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2Fukang Station of Desert Ecology, Chinese Academy of Sciences, Fukang 831505, Xinjiang, China; 3University of Chinese Academy of Sciences, Beijing 100049, China; 4Natural Forest Protection Center of Xinjiang Uygur Autonomous Region, Urumqi 830001, China).

  • Online:2023-06-10 Published:2023-06-05

摘要: 厘清气候变化和人类活动对净初级生产力(NPP)的影响,对区域环境管理和可持续发展具有重要意义。本研究以阜康市为对象,基于NPP、土地利用和气象数据,分析阜康市2001—2019年实际NPP(NPPA)的时空变化,进一步区分气候变化和人类活动对垂直自然带NPPA的影响。结果表明:阜康市NPPA多年均值为100.56 g C·m-2·a-1,年际变化呈显著上升趋势(P<0.05)。NPPA的高值区域和快速上升区域均位于农田和林地。不同土地利用类型NPPA的多年均值差别显著(P<0.05),其中林地最高(335.77 g C·m-2·a-1),沙漠最低(19.27 g C·m-2·a-1)。林地、草地和建设用地的NPPA均呈显著上升趋势(P<0.05)。将NPPA细分为潜在NPP(NPPP)和人类活动导致的NPP(NPPH)后发现,阜康市的NPPP多年均值为284.06 g C·m-2·a-1,年际变化不显著(P>0.05)。而NPPH多年均值为183.50 g C·m-2·a-1,存在显著的下降(P<0.05)。气候变化和人类活动对不同自然带的影响存在差异,草原带内气候变化对NPPA的贡献最大(NPPP=353.05 g C·m-2·a-1),而荒漠带内的NPPA受人类活动的影响最大(NPPH=201.94 g C·m-2·a-1)。对于NPPA的影响因素来说,降水量和温度的增加使NPPP上升,并间接促进NPPA上升;而有利的人类活动强度的增加使NPPH下降,并间接促进NPPA上升。


关键词: 路径分析, CASA模型, 净初级生产力, 温度, 降水

Abstract: Clarifying the impacts of climate change and human activities on net primary productivity (NPP) is important for regional environmental management and sustainable development. Based on data of NPP, land use type and meteorology, we analyzed the spatial and temporal variations of actual NPP (NPPA) in Fukang from 2001 to 2019, and further distinguished the impacts of climate change and human activities on NPPA in altitudinal natural belts. The results showed that the multi-year average of NPPA in Fukang was 100.56 g C·m-2·a-1, with a significant increasing trend (P<0.05). The areas with high and rapidly rising NPPA were located in farmlands and forests. The multi-year average of NPPA of different land use types differed significantly (P<0.05), with the highest in forests (335.77 g C·m-2·a-1) and the lowest in deserts (19.27 g C·m-2·a-1). NPPA of forests, grasslands, and built-up lands showed a significant increasing trend (P<0.05). After subdividing NPPA into potential NPP (NPPP) and NPP caused by human activities (NPPH), we found that the multi-year average of NPPP in Fukang was 284.06 g C·m-2·a-1, with insignificant interannual variation (P>0.05). In contrast, the multi-year average of NPPH was 183.50 g C·m-2·a-1, with a trend of significant decline (P<0.05). There were differences in the impacts of climate change and human activities on different natural belts, with climate change contributing most to NPPA in the steppe belt (NPPP=353.05 g C·m-2·a-1) and NPPA in the desert belt being most influenced by human activities (NPPH=201.94 g C·m-2·a-1). For the impact factors of NPPA, precipitation and temperature can indirectly contribute to NPPA by enhancing NPPP, while beneficial human activities indirectly contribute to NPPA by reducing NPPH.


Key words: path analysis, CASA model, net primary productivity, temperature, precipitation.