国内外旅游系统模型研究综述

从系统论角度来考虑。人类的旅游活动是一个系统。旅游系统是备种旅游事象的集合体。是通过旅游者的旅游活动使备组成要素相互联系、相互作用构成的一个有机整体．它具有实现旅游价值的整体功能。在分析和阐释旅游系统特征的基础上，以时间为序列对国内外学者提出的旅游系统模型进行了介绍评述和总结．指出系统论的观点不仅为旅游资源的开发提供了认识论基础；同时又为旅游规划和开发提供了方法论基础，并提出，对具有环境观和复杂性特点的旅游地理系统的研究将成为未来旅游科学的重要研究方向。旅游系统模型的建立将为旅游（业）的研究提供现实的理论基础。     

长江三峡花岗岩地区土壤流失时间分布特性

长江三峡花岗岩地区坡面土壤流失以耕地砂砾化面蚀和有部分植物覆盖坡面的鳞片状面蚀为主，该地土壤流失研究结果表明，由以上两类面蚀导致的土壤流失量月分布与月降雨量的分布基本趋势一致，二者呈现较为明显的线性相关关系。地面坡度＞３０°的裸地土壤流失量达５０００ｔ／ｋｍ３·ａ以上，覆盖度≥０．７０的林地土壤流失量＜５００ｔ／ｋｍ２·ａ，该流域土壤流失量为１５４４．１４ｔ／ｋｍ２·ａ，产沙量为６９４．８６ｔ／ｋｍ２·ａ     

Environmental disasters,migration and displacement. Insights and developments from L’Aquila's case

This paper analyses the environmentally-induced migration and displacement resulting from L’Aquila's earthquake of 2009. After a general critical overview of the social science literature on this topic, the main changes in the migration system are analysed looking at the roots and trajectories of the forced human displacement that followed the earthquake, and reflecting on the challenges related to post-earthquake demographic movements and post-disaster resettlement. Through the analysis of the pre disaster (2002–2008) and recovery period (2009–2013) data, this paper offers a general model of how environmental disaster might affect migration and displacement and suggests the main challenges related to the post-disaster governance. Relying on ISTAT data on internal migration in Italy this paper argues that the post-seismic recovery period is characterized by a strong increase of out-flows from L’Aquila to other provinces, within the Abruzzo region and outside it, in particular toward the closest regions (Latium, Campania).     

贫困地区可持续发展指标体系及其综合评估--以湖南湘西贫困地区为例

本文依据贫困地区可持续发展固有的制约因素，特殊的内涵与目标，首次利用压力（Pressure)——状态（State)——响应（Respons)模型，构建了贫困地区可持续发展指标体系，并采用专家咨询与定量模型相结合的方法，对湖南湘西贫困地区可持续发展水平作了实证评估与分析。     

关于区域可持续发展的系统分析

本文从更高、更新、更综合的高度和角度,对区域社会可持续发展系统进行了单元要素分析、结构层次分析。提出了三单元要素、三结构层次、三种发展类型的设想。这种分析尽管还是初步的、定性的、不很深刻的,但是为研究可持续发展系统提供了一种新的思路。     

19世纪是我国特大暴雨洪水发生期

本文用大量资料,论述了我国七个江河历史首位洪水均发生在19世纪。而且,洪水泛滥使得平原地区的水系迁移、湖泊淤缩极为严重。同时,存洪水年前后,伴随着一系列寒冷、干旱的气候异常现象。     

TREE RING RECONSTRUCTIONS OF STREAMFLOW FOR THREE CANADIAN PRAIRIE RIVERS1

ABSTRACT: Information regarding long term hydrological variability is critical for the effective management of surface water resources. In the Canadian Prairie region, growing dependence on major river systems for irrigation and other consumptive uses has resulted in an increasing vulnerability to hydrological drought and growing interprovincial tension. This study presents the first dendrochronological records of streamflow for Canadian Prairie rivers. We present 1,113‐year, 522‐year, and 325‐year reconstructions of total water year (October to September) streamflow for the North Saskatchewan, South Saskatchewan, and Saskatchewan Rivers, respectively. The reconstructions indicate relatively high flows during the 20th Century and provide evidence of past prolonged droughts. Low flows during the 1840s correspond with aridity that extended over much of the western United States. Similarly, an exceptional period of prolonged low flow conditions, approximately 900 A.D. to 1300 A.D., is coincident with evidence of sustained drought across central and western North America. The 16th Century megadrought of the western United States and Mexico, however, does not appear to have had a major impact on the Canadian rivers. The dendrohydrological records illustrate the risks involved if future water policy and infrastructure development in the Canadian Prairies are based solely on records of streamflow variability over the historical record.     

土地资源利用保护与农业生态建设

本文阐述了国内外土地后备资源现状及存在问题,解剖了土壤肥力演化机制和土壤资源保护的关系,介绍了我国生态农业建设的研究进展,指出了今后的主攻方向。     

多层次模糊综合评判在林业土壤评价中的应用

本文以四川部分林业土壤为例,应用多层次模糊综合评判法进行土壤资源的质量评价。采取聘请众多专家分级、打分的办法制定评价标准和确定评价因素权数。实施了专家系统与综合评判的联合运用技术,并探讨了提高土壤质量评级精度的“加细”评判问题。最后,通过比较多层次模糊综合评判法与传统法(评分法)的评价结果,指出前者具有更强的客观性和全面性。