红色旅游发展效率评价及影响因素研究——以黔北黔西红色旅游区为例

红色旅游发展效率表征旅游区红色旅游高质量发展水平。以黔北黔西红色旅游区为研究对象,借助DEA模型及Malmquist指数对2014—2019年该区域17个县（市、区）的红色旅游发展效率进行测度,同时利用核密度函数和多元线性回归模型分别剖析了其空间演化特征与关键影响因素。研究发现：（1）研究区域内红色旅游发展效率整体偏低,受技术进步的积极影响,多数县（市、区）红色旅游发展效率呈稳步提升状态;（2）红色旅游发展效率具备空间集聚性和异质性的特征,整体呈现“M”型双峰分布,区域分布差异较大;（3）技术创新、红色旅游资源优势度、交通便利性是影响该区域红色旅游发展效率的主要因素,政府对旅游经济干预程度、经济发展水平和人才规模对该区域红色旅游发展效率的影响较小,产业结构对改善该区域红色旅游发展效率的积极影响尚未凸显。     

不同地区经济增长与环境污染关系的VAR模型分析——基于广州、佛山、肇庆经济圈的实证研究

利用向量自回归(VAR)计量技术对广州.佛山一肇庆(简称"广佛肇")经济圈各城市表征环境污染的指标(工业废水排放量、工业废气排放量和工业固废产生量)和表征经济增长的指标(人均GDP)的时序数据进行脉冲响应函数及预测方差分解分析,研究处于工业化后期的广州、佛山市及工业化前期的肇庆市经济发展与环境污染在时序维度上的关系及其...     

Vertical and temporal distribution of nitrogen and phosphorus and relationship with their influencing factors in aquatic-terrestrial ecotone： a case study in Taihu Lake, China

Vertical and temporal distributions of N and P in soil solution in aquatic-terrestrial ecotone （ATE） of Taihu Lake were investigated, and the relations among N, P, ORP （oxidation reduction potential）, TOC, root system biomass and microorganism were studied. As a whole, significant declines in TN, NO3^--N, DON （dissolved organic nitrogen） and TP concentration in soil solution have occurred with increase of the depth, and reached their minima at 60 cm depth, except for NH4^＋-N, which increased with depth. The concentration of TP increased gradually from spring to winter in the topsoil, the maximum 0.08 mg/L presented in the winter while the minimum 0.03 mg/L in spring. In the deeper layer, the concentration value of TP fluctuated little. As for the NO3^--N, its seasonal variation was significant at 20 cm depth, its concentration increased gradually from spring to autumn, and decreased markedly in winter. Vertical and temporal distribution of DON is contrary to that of NO3^--N. The results also show that the variation of N and P in the percolate between adjacent layers is obviously different. The vertical variation ofTN, TP, NO3^--N, NH4^＋-N and DON is significant, of which the variation coefficient of NO3^--N along the depth reaches 100.23%, the highest; while the variation coefficient of DON is 41.14%, the smallest. The results of correlation analysis show that the concentration of nitrogen and phosphorus correlate significantly with TOC, ORP, root biomass and counts of nitrifying bacteria. Most nutrients altered much from 20 to 40 cm along the depth. However, DON changed more between 60 and 80 cm. Results show that soil of 0-60 cm depth is active rhizoplane, with strong capability to remove the nitrogen and phosphorus in ATE. It may suggest that there exists the optimum ecological efficiency in the depth of above 60 cm in reed wetland. This will be very significant for ecological restoration and reestablishment.