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郑洋程琳琳王义方王俊奇 《地理科学进展》2023,(2):275-286
科学诊断资源型城市空间冲突等级,厘清空间冲突变化与土地利用间的复杂关系,对城市转型发展、区域资源合理利用具有重要意义。论文基于山东省新泰市资源型城市特征,以生态系统服务价值和土地利用为视角,从空间压力、空间暴露性和空间风险响应维度构建空间冲突测度模型,并运用地理加权回归模型探讨了空间冲突的变化与土地利用调整间的关系。结果表明:(1)2009—2020年,新泰市空间冲突指数保持稳定,变化量仅为0.0018,且不同冲突等级的变化趋势不同;空间冲突格局呈圈层分布,由中心向四周等级逐渐减弱。(2)2009—2020年,新泰市平均土地利用动态度为23.14%,空间布局差异性显著,土地利用特征以耕地林化、土地整治、建设用地及生态用地扩张为主。(3)地理加权回归模型分析显示,土地利用动态度与空间冲突指数变化呈显著相关(P<0.01,R^(2)=0.8517),平均系数值为0.1381,且以正相关为主,表明新泰市土地利用调整对空间冲突的抑制产生了积极影响。研究可为区域土地合理利用、空间冲突治理及空间结构优化提供科学依据。 相似文献
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针对新泰市区及周边村镇的水资源调查、水文取样及地下水的系统分析,综合运用相关分析和因子分析方法,研究了新泰市地下水水化学特征并揭示了其成因,指出NO3-、Cl-及SO42-浓度升高预示人为因素对地下水已经产生了一定的污染。 相似文献
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Multiple sulfur isotope ratios (^34S/^33S/^32S) of Archean bedded sulfides deposits were measured in the Yanlingguan Formation of the Taishan Group in Xintai, Shandong Province, East of China; 633S = -0.7%o to 3.8‰,δ^34S = 0.1‰-8.8‰, △^33S = -2.3‰ to -0.7‰. The sulfur isotope compositions show obvious mass-independent fractionation (MIF) signatures. The presence of MIF of sulfur isotope in Archean sulfides indicates that the sulfur was from products of photochemical reactions of volcanic SO2 induced by solar UV radiation, implying that the ozone shield was not formed in atmosphere at that time, and the oxygen level was less than 10-5 PAL (the present atmosphere level). The sulfate produced by photolysis of SO2 with negative △^33S precipitated near the volcanic activity center; and the product of element S with positive △^33S precipitated far away from the volcanic activity center. The lower △^33S values of sulfide (-2.30‰ to --0.25‰) show that Shihezhuang was near the volcanic center, and sulfur was mostly from sulfate produced by photolysis. The higher △^33S values (-0.5‰ to -‰) indicate that Yanlingguan was far away from the volcanic center and that some of sulfur were from sulfate, another from element S produced by photolysis. The data points of sulfur isotope from Yanlingguan are in a line parallel to MFL (mass dependent fractionation line) on the plot of δ^34S--δ^33S, showing that the volcanic sulfur species went through the atmospheric cycle into the ocean, and then mass dependent fractionation occurred during deposition of sulfide. The data points of sulfur isotope from Shihezhuang represent a mix of different sulfur source. 相似文献