旅游景区游客满意度的测评指标体系研究——以连云港花果山风景区为例

旅游景区的竞争力来自于游客的满意度,游客满意度的高低深刻影响着旅游景区的发展潜力与能力.旅游景区游客满意度评价是当前旅游景区管理的研究重点和难点之一.在文献综述的基础上,从旅游景观、价格感知、餐饮服务、交通状况、住宿、娱乐、购物、游览、经营管理9个方面构建了旅游景区游客满意度测评指标体系,运用因素重要性推导模型对连云港花果山风景区进行了实证研究,得出连云港花果山风景区的急需改进因素、次要改进因素、锦上添花因素和竞争优势因素,针对急需改进因素提出了连云港花果山风景区的发展建议.     

南京钟山风景区对主城环境空气质量的影响

详细监测了钟山风景区环境空气质量现状,利用大气污染扩散模型的扩散模拟,从地形方面研究了钟山风景区对主城大气污染物输送扩散的影响。结果表明,钟山风景区使得主城大气污染物不易扩散,易在主城区附近积累,加重主城区的大气污染。     

Work-related injury and ill-health among mountain instructors in the UK

In most industrialised countries, work-related injury and ill-health presents a major burden to society. Musculoskeletal disorders and stress are the most common reported illness types with those working in some industries more at risk than others. This study aimed to understand the occupational health issues of those working as mountain instructors in the outdoor sector within the UK and to identify the cultural norms and behaviours among this unique occupational group which influence health. Semi-structured, telephone interviews were conducted with 20 qualified mountaineers to gain information on work-related injury and ill-health. The majority of interviewees reported a current work-related musculoskeletal problem. Key factors were identified which prevented effective rehabilitation, including; a ‘macho’ attitude among young instructors, self-imposed extended working hours/days and mismanagement of injuries. Self-employed instructors reported that sick leave after a minor injury or illness was not financially viable. Work-related issues leading to stress were also reported.     

贡嘎山冷杉林带草海子小流域土壤及湖泊沉积物中磷的形态及迁移特征

磷（P）是控制水体生态系统生产力的重要元素,了解陆地与水体间P的迁移特征,是了解控制水体生态系统中P有效供给的重要途径。本研究选择青藏高原东缘贡嘎山海拔2800 m左右峨眉冷杉林带中一小湖泊——草海子及其流域,通过对流域内土壤、湖泊沉积物中P的形态组成分析,探讨流域内P的形态组成及其迁移特征。结果表明,草海子流域内土壤成土母质中的磷以Ca-P为主,表层土壤中的磷以Al、Fe结合态为主,占总磷的49%~80%,而湖泊沉积物中Al、Fe结合态P下降到46%左右。在成土作用及植物吸收的过程中P由土壤剖面下部向上迁移,迁移的主要形态为树脂提取态（或称可交换态,R-P）,而R-P还是由陆地向水体迁移的主要形态P。土壤的Al、Fe结合态P难以释放转化,因此少有随地表径流迁移向湖泊。     

泰山野生植物资源研究

泰山植物资源丰富,共有野生种子植物１０７科４０１属７６２种。本文按经济用途将泰山的资源植物主要分为１１类,提出了对它们进行合理开发利用的措施     

大巴山区早古生代地层和石煤中硒的化学活动性的初步研究

通过对大巴山区主要分布的早古生代地层中的碎屑岩，碳酸盐岩和石煤的原岩，风化岩，原生土壤的硒含量及其相关关系分析，及对南秦岭早古生代地层和石煤中硒的化学活动性进行了研究。结果表明：其岩石和石煤中的硒在地层环境下有较大的活动性，不同类型岩石中硒淋失率和硒的淋失量不同，富硒而淋失率低但淋失量高的下寒武统鲁家坪组和早志留世大贵坪组的炭质板岩和石煤的分布区土壤（主要为当地岩石的风化残积物）的含硒量可达10mg/kg，甚至更高，是大巴山的富硒带和硒中毒带，含硒低而且淋失率高的志留系砂岩和粉砂岩以及寒武系统砾屑灰岩分布区是大巴山区的低硒带。     

山地灾害防治工程经济效益评价刍议

阐述了山地灾害防治工程经济软益评价的必要性和作用，分析并指出现有评价方法和指标存在的问题，提出了规范和改进评价方法和指标的具体作法．     

五台山亚高山草甸小格局分析

用种毗连法和种小区法对五台山２４００２８００ｍ的亚高山草甸的小格局分析．结果表明：在小格局中,大部分种与优势种苔草呈正关联;小格局规模都较小,各个种趋于交错分布;不同规模的格局应用不同的分析方法,小格局不能用中格局分析方法进行研究;种小区法和种毗连法都是有效的小格局分析方法,从本文结果看前者优于后者．     

South-Siberian mountain mires: Perspectives on a potentially vulnerable remote source of biodiversity

Changes in climate, land-use and pollution are having disproportionate impacts on ecosystems and biodiversity of arctic and mountain ecosystems. While these impacts are well-documented for many areas of the Arctic and alpine regions, some isolated and inaccessible mountain areas are poorly studied. Furthermore, even in well-studied regions, assessments of biodiversity and species responses to environmental change are biased towards vascular plants and cryptogams, particularly bryophytes are far less represented. This paper aims to document the environments of the remote and inaccessible Altai-Sayan mountain mires and particularly their bryofloras where threatened species exist and species new to the regional flora are still being found. As these mountain mires are relatively inaccessible, changes in drivers of change and their ecosystem and biodiversity impacts have not been monitored. However, the remoteness of the mires has so far protected them and their species. In this study, we describe the mires, their bryophyte species and the expected impacts of environmental stressors to bring attention to the urgency of documenting change and conserving these pristine ecosystems.Supplementary InformationThe online version contains supplementary material available at 10.1007/s13280-021-01596-w.     

长白山高山冻原氮素生物循环及与北极冻原的对比

利用分室模型对长白山高山冻原系统氮素生物循环进行了研究;利用植物属种共有率对长白山高山冻原与北极冻原进行了对比研究.结果表明,长白山高山冻原植物区系中有89.3%的属和58.6%的种与北极冻原共有,其中地衣、苔藓和维管束植物与北极冻原相似类群属和种的共有率分别为95.5%和58.7%、82.1%和76.3%、93.1%和40.5%.这种高度的共有率决定了长白山高山冻原和北极冻原的植物区系和植被外貌具有高度相似性.长白山高山冻原植被-土壤系统总氮净储存为 65 220.6 t,其中土壤库占99.3%.长白山高山冻原系统中氮在各个分室的储存量分别是:植被库237.4 t;凋落物库145.3 t;土壤库64 837.9 t.地上植物活体、地下根系、凋落物中氮素年转移量分别为: 131.7 t·a^-1, 58 t·a^-1和73.7 t·a^-1.