Arid Land Geography ›› 2025, Vol. 48 ›› Issue (11): 1926-1938.doi: 10.12118/j.issn.1000-6060.2024.703
• Hydrology and Water Resoures • Previous Articles Next Articles
TIAN Jinhua1(
), HUANG Xiao2, GAO Yayu2,3,4(
), HAO Jianbin2, WU Guanheng5, HE Wenbo2
Received:2024-11-14
Revised:2025-01-09
Online:2025-11-25
Published:2025-11-26
Contact:
GAO Yayu
E-mail:tjhgyy@yeah.net;gyy@lut.edu.cn
TIAN Jinhua, HUANG Xiao, GAO Yayu, HAO Jianbin, WU Guanheng, HE Wenbo. Ecological benefits of inter-basin water transfer in arid ecological migration regions of northwest China: A case of Huanghuatan ecological immigrant area[J].Arid Land Geography, 2025, 48(11): 1926-1938.
Tab. 1
Data sources and ecological significance of ecological benefit evaluation indices"
| 要素层 | 指标层 | 生态学意义 | 数据来源 |
|---|---|---|---|
| 自然气象 | 年降水量 | 直接影响土地植被的生长、水资源的运动和分布、土壤 侵蚀和养分流失等 | 中国科学院资源与环境科学数据中心( |
| 年蒸发量 | 反映土地利用和气候变化影响最有效的因素 | ||
| 气温 | 气温变化直接影响生态系统的结构 | ||
| 平均相对湿度 | 影响植被群落的结构和物种组成,进而影响生态系统 的稳定性 | ||
| 植被概况 | 归一化植被指数 | 对植被变化状况监测、植被资源合理利用和其他生态 环境相关领域的研究有十分重要的参考意义 | 国家地球系统科学数据中心( |
| 植被净初级生产力 | 评估生态系统的碳储存能力、生物量生产以及对气候变 化的响应,可以更好地理解生态系统的生产力和健康状况 | ||
| 人类活动 | 土地利用 | 人类活动作用于自然环境的主要途径之一,是土地覆被 变化的最直接和最主要的驱动因子 | 中国科学院资源与环境科学数据中心( |
| 土地转移 | 人类活动作用于自然环境的主要途径之一,是土地覆被 变化的最直接和最主要的驱动因子 | ||
| 跨流域调水量 | 反映生态系统中人类活动的影响 | ||
| 景观格局 | 斑块数量 | 分析生态系统类型在区域内的分布规模和破碎程度, 从而评估人类活动对景观格局的影响 | 基于土地利用数据利用FRAGSTATS 4.2软件 计算所得 |
| 斑块密度 | 分析生态系统类型在区域内的分布规模和破碎程度, 从而评估人类活动对景观格局的影响 | ||
| 分割度指数 | 评估景观破碎化对生态系统服务和生物多样性的影响, 以及人类活动对生态系统的潜在影响 | ||
| 辛普森多样性指数 | 有助于评估和理解生态系统的多样性和健康状态, 从而为生态环境保护规划提供科学依据 | ||
| 聚合度指数 | 考察每一种景观类型斑块间的连通性,有助于评估 景观的连通性和生态过程的连续性 | ||
| 分离度指数 | 衡量景观中斑块或区域的空间分散程度,其值越大,表示 景观中的斑块被更多的线性特征(如道路、河流等)所分隔 |
Tab. 2
Area and proportion of different land use types in Huanghuatan ecological immigrant area from 2005 to 2020"
| 土地利用类型 | 2005年 | 2010年 | 2015年 | 2020年 | |||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| 面积/km2 | 占比/% | 面积/km2 | 占比/% | 面积/km2 | 占比/% | 面积/km2 | 占比/% | ||||
| 旱地 | 144.63 | 31.64 | 138.18 | 30.23 | 138.70 | 30.35 | 152.81 | 33.43 | |||
| 有林地 | 0.12 | 0.03 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | |||
| 疏林地 | 3.58 | 0.78 | 3.58 | 0.78 | 3.58 | 0.78 | 3.60 | 0.79 | |||
| 中覆盖度草地 | 45.73 | 10.01 | 47.08 | 10.30 | 43.96 | 9.62 | 41.79 | 9.14 | |||
| 低覆盖度草地 | 155.66 | 34.06 | 154.45 | 33.79 | 151.89 | 33.23 | 153.15 | 33.50 | |||
| 农村居民点 | 1.95 | 0.43 | 2.05 | 0.45 | 4.12 | 0.90 | 1.84 | 0.40 | |||
| 建设用地 | 0.00 | 0.00 | 0.00 | 0.00 | 34.83 | 0.08 | 529.20 | 1.16 | |||
| 沙地 | 92.20 | 20.17 | 90.69 | 19.84 | 90.19 | 19.73 | 87.74 | 19.20 | |||
| 裸地 | 13.18 | 2.88 | 21.00 | 4.59 | 24.25 | 5.30 | 10.87 | 2.38 | |||
Tab. 3
Changes of landscape pattern indices in Huanghuatan ecological immigrant area from 2005 to 2020"
| 年份 | 斑块数量/个 | 斑块密度/个·km-2 | 分割度指数 | 分离度指数 | 辛普森多样性指数 | 聚合度指数 |
|---|---|---|---|---|---|---|
| 2005 | 450 | 0.9846 | 0.9408 | 16.8841 | 0.7322 | 93.5590 |
| 2010 | 466 | 1.0196 | 0.9459 | 18.4766 | 0.7422 | 93.5449 |
| 2015 | 485 | 1.0612 | 0.9486 | 19.4632 | 0.7463 | 93.5702 |
| 2020 | 452 | 0.9888 | 0.9470 | 18.8768 | 0.7300 | 93.4910 |
Tab. 4
Changes of NDVI and NPP in Huanghuatan ecological immigrant area in water supply stage"
| 年份 | NDVI | NPP/g C·m-2 | |||||||
|---|---|---|---|---|---|---|---|---|---|
| 最小值 | 最大值 | 年均值 | 标准差 | 最小值 | 最大值 | 年均值 | 标准差 | ||
| 2013 | 0.02 | 0.63 | 0.17 | 0.07 | 3.00 | 253.00 | 41.20 | 71.60 | |
| 2014 | -0.07 | 0.57 | 0.18 | 0.07 | 12.00 | 253.00 | 45.75 | 69.84 | |
| 2015 | -0.18 | 0.63 | 0.16 | 0.06 | 4.00 | 253.00 | 42.81 | 70.88 | |
| 2016 | -0.13 | 0.66 | 0.18 | 0.08 | 4.00 | 253.00 | 42.81 | 70.88 | |
| 2017 | -0.35 | 0.64 | 0.17 | 0.06 | 4.00 | 253.00 | 42.81 | 70.88 | |
| 2018 | -0.26 | 0.65 | 0.21 | 0.08 | 4.00 | 253.00 | 42.81 | 70.88 | |
| 2019 | -0.24 | 0.61 | 0.22 | 0.07 | 2.00 | 253.00 | 41.04 | 71.59 | |
| 2020 | -0.25 | 0.64 | 0.18 | 0.07 | 4.00 | 253.00 | 42.81 | 70.88 | |
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