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息地质的时空演变及其推动因素在汉河流域,中国
Jiefeng Kou1,2,3, Jun Liu4, Hongliang Wang5
1Changjiang Basin Ecology and Environment Monitoring and Scientific Research Center, Changjiang Basin Ecology and Environment Administration, Ministry of Ecology and Environment, Wuhan, 430010, China.
Scientific reports
|July 18, 2025
概括
汉河流域 (HRB) 的息地质量显示中等水平,最初下降,随后在20年内恢复. 土地使用强度和海拔高度是关键因素,导致低海拔地区的人为引发的压力和高海拔地区的自然调节.
科学领域:
- 生态评估和环境科学.
- 生物多样性和保护研究.
- 区域规划和可持续发展.
背景情况:
- 息地质量 (HQ) 对生态健康和生物多样性至关重要.
- 汉河流域 (HRB) 面临着严重的人类影响,需要HQ评估.
- 了解HQ进化对于生态安全和可持续发展至关重要.
研究的目的:
- 从2000年到2023年,分析HRB中总部的空间和时间演变.
- 量化影响HQ变化的主要驱动因素.
- 为HRB的生态保护和绿色发展提供科学支持.
主要方法:
- 使用InVEST模型来评估HQ.
- 采用地质探测器方法来确定驱动因素.
- 分析了23年时间内的空间和时间总部动态.
主要成果:
- 在HRB中的HQ保持中度 (0.446-0.461),显示整体略有下降.
- 空间总部模式显示"高在中间,低在两侧".
- 土地使用强度和高度是主要的驱动因素,人类活动和自然因素相互作用.
结论:
- 在HRB的总部经历了波动,与明显的空间模式的退化和改进.
- 土地使用强度,海拔,温度和GDP显著影响了HQ.
- 人类压力和自然调节的双模式驾驶模式塑造了HRB中的HQ演变.
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