《山东大学学报(理学版)》 ›› 2026, Vol. 61 ›› Issue (10): 201-212.doi: 10.6040/j.issn.1671-9352.0.2026.109
• 水文过程与生态响应 • 上一篇
张学涵,韩美*
ZHANG Xuehan, HAN Mei*
摘要: 济南市是黄河流域中心城市,是驰名中外的“泉城”,全面评估其地表水连通性的时空变化,识别关键影响因素,提出科学可行的优化路径,对提升其水资源流动性、改善水质、促进以泉水为核心的生态系统修复具有重要意义。本研究立足南山北水地貌格局,构建“结构连通-过程连通-功能连通”三维评价体系,综合利用遥感解译、地理空间分析等多源数据,系统揭示1985—2022年济南市地表水连通性的时空演变特征与驱动机制,并提出多尺度优化策略。实践上,将海绵城市建设理念融入路径设计,提出适用于北方岩溶型城市的保泉供水协同优化策略,为破解水资源供需矛盾提供技术范式。结果表明:近40年来,济南市的地表水连通性呈现波动上升的趋势;在空间上呈现出南部山区优于北部城区的格局,过渡带受农田水利工程影响,整体形成结构优化-功能提升的良性循环。生态修复工程缓解了城市连通性退化,但城市化扩张对水系格局的切割效应仍然存在。地理探测器定量归因表明,GDP和年降水量是解释连通性空间分异的主导因子,人类活动已成为影响连通性演变的主导因素。基于上述结论,本文针对性提出南部岩溶区封山育林与阶梯渗滤池修复地下水、北部平原疏浚河道与建设生态堰重构廊道、建成区推广海绵工程与智慧管理,促进蓝绿协同的差异化修复策略。
中图分类号:
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