全新世内蒙古自然环境演变及其特点

根据内蒙古东、中、西部沙地、内陆湖、冰缘现象的发育与演变，讨论了全新世以来内蒙古环境演变过程，提出了对全新世中期沙漠化的形成环境、全新世环境演变特点及对现代环境影响的认识。     

塔里木河流域城市化与水资源利用关系分析

比较分析塔里木河流域1990—2005年城市化水平、用水总量、产业结构、用水效益的变化过程,建立城市化水平与用水效益、用水总量之间的数学关系。结果表明,城市化水平与用水效益呈线性增长关系,随着城市化进程的推进和产业结构的升级,塔里木河流域及各市用水效益都在不断提高;水资源对城市化进程存在明显的约束作用,塔里木河流域的城市化水平与用水总量之间对数增长关系不明显;总结归纳了塔里木河流域城市发展与水资源利用之间初级矛盾、扩张矛盾、适应矛盾、适应协调4个发展阶段特征。今后需调整产业结构,建立集约的水资源利用体系,调整水资源利用与城市发展关系由矛盾状态为适应协调状态,缓解水资源对城市化进程的约束。     

虚拟合作实验室-利用Internet开展大气科学国际合作研究的可行之路

试图提出一个由中美双方大气科学家参与的虚拟合作实验室的解决方案,实验室包括虚拟资料／信息系统、虚拟模拟系统、虚拟应用分析系统、虚拟培训学校、虚拟图书馆、虚拟可视化实验室和虚拟出版系统等。     

Evolution and spatial characteristics of tourism field strength of cities linked by high-speed rail (HSR) network in China

Traffic is an indispensable prerequisite for a tourism system. The “four vertical and four horizontal” HSR network represents an important milestone of the “traffic revolution” in China. It will affect the spatial pattern of tourism accessibility in Chinese cities, thus substantially increasing their power to attract tourists and their radiation force. This paper examines the evolution and spatial characteristics of the power to attract tourism of cities linked by China’s HSR network by measuring the influence of accessibility of 338 HSR-linked cities using GIS analysis. The results show the following. (1) The accessibility of Chinese cities is optimized by the HSR network, whose spatial pattern of accessibility exhibits an obvious traffic direction and causes a high-speed rail-corridor effect. (2) The spatial pattern of tourism field strength in Chinese cities exhibits the dual characteristics of multi-center annular divergence and dendritic diffusion. Dendritic diffusion is particularly more obvious along the HSR line. The change rate of urban tourism field strength forms a high-value corridor along the HSR line and exhibits a spatial pattern of decreasing area from the center to the outer limit along the HSR line. (3) The influence of the higher and highest tourism field strength areas along the HSR line is most significant, and the number of cities that distribute into these two types of tourism field strengths significantly increases: their area expands by more than 100%. HSR enhances the tourism field strength value of regional central cities, and the radiation range of tourism attraction extends along the HSR line.     

我国荒漠植物的水分饱和亏

本文研究了我国荒漠植物的水分饱和亏, 结果以典型的荒漠旱生植物珍珠和红砂最大, 分别为43.4%和35.6%, 梭梭34.7%, 籽蒿37.1%。中生植物刺槐和钻天杨水分饱和亏最小, 分别为15.0%和14.3%。这就表明, 荒漠植物在干旱条件下, 免于伤害的能力与水分饱和亏的大小密切相关。     

沉积物记录的亚高山湖泊环境变化——以鄂东南云中湖为例

根据云中湖27 cm长沉积岩芯进行元素、粒度和硅藻多指标分析以及²¹⁰Pb测年,结合流域气候和人类活动等历史资料,反演1958年以来云中湖在气候变化和人类活动影响下的环境变化。冗余分析结果显示云中湖沉积硅藻组合变化与Al、Fe、Pb和温度四个变量显著相关。硅藻属种聚类分析的结果表明云中湖环境变化经历了两个阶段：1958-1993年间喜碱性水体的Achnanthes minutissima和Fragilaria nanana属种大量出现与较高CIA指数响应于气候调控下的流域侵蚀过程;1993年以来气候变暖与旅游发展引起入湖营养盐增加是Cyclotella pseudostelligera和Aulacoseira alpigena等中—富营养硅藻种增殖的主要诱因。重建亚高山湖泊在气候变化以及人类活动影响下湖泊生态系统的演化,为保护亚高山湖泊生态环境和改善流域水质提供参考。     

中西部地区承接产业转移的影响因素研究

将中西部地区划分为东北、中部、西北、西南4个区域,采用1995—2013年的相关数据,分析各区域在承接东部发达地区产业转移过程中的主要影响因素。选取的影响因素包括资本存量、经济规模、劳动力成本、人力资源和路径效应。结果发现:4个区域的路径效应、资本存量与产业转移承接地均存在显著正相关关系;人力资源与产业转移承接地存在正相关关系,但东北、西北地区不显著;劳动力成本与产业转移承接地存在负相关关系,但对东北地区不显著;除中部地区外,经济规模与产业转移承接地并不存在显著相关关系。中西部区域地方政府和企业家在促进产业转移进程中应充分发挥比较优势,根据不同影响要素制定宏观政策与微观引资策略。     

河南省老龄人口的空间分布及变动

根据人口普查数据资料,运用数理统计分析方法对河南省老龄人口的分布及其变动、人口密度及其变化趋势等进行分析。河南乡村老龄人口仍占多数,但其分布重心正逐步向城镇转移;各地区老龄人口规模相差较大且分异明显,同时,地区间老龄人口密度差异悬殊,增长变化差距很大;老龄人口分布虽存在地区差异,但发展变化总的趋势是人口老龄化、高龄化加速发展,养老服务需求增大。建立科学合理的社会养老服务体系是当前应对人口老龄化、保障和改善民生的必然要求。     

鄱阳湖流域史前人类遗址时空分布及其环境响应（英文）

The temporal-spatial geographic distribution of archaeological sites and its feature between 10.0–2.8 ka BP(ka BP= thousands of years before 0 BP, where "0 BP" is defined as the year AD 1950) were determined, based on GIS spatial analysis in the Poyang Lake Basin. The relationship between geographic distribution of sites of different periods under subsistence existence of ancient civilizations, climate and environmental change was investigated. The results revealed numerous archaeological sites of the Neolithic Age(10.0–3.6 ka BP). The sites were mainly located in the northern part of the Poyang Lake Basin, a hilly and mountainous area with many river terraces suitable for the development of human civilization. The number of archaeological sites rapidly increased during the Shang and Zhou dynasties(3.6–2.8 ka BP) and spread widely on the floodplains of the middle and lower reaches of Ganjiang River and onto the west, south, and southeast beach areas of the Poyang Lake. Holocene records of climate change suggested that it was possible that climate fluctuations had a great impact on human evolution in the study area. Before 3.6 ka BP, westward and northward expansion of Neolithic cultures in the Poyang Lake watershed occurred under the background of climate amelioration(becoming warmer and wetter). The ancient people lived in the hilly areas with high elevation. The simple mode of a fishing and gathering economy was mostly suited to this area in the early Neolithic Age. The scope of human activities was expanded and cultural diversity developed in the late Neolithic Age. However, with population growth and increasing survival pressure in a dry-cold climatic stage after 3.6 ka BP, this simple living mode had to be abandoned, and various forms of economy, the majority being agriculture, were developed on flood plains of the lower reaches of numerous rivers around Poyang Lake. This promoted flourishing of the Bronze culture of South China.     

Capacity of soil loss control in the Loess Plateau based on soil erosion control degree

The capacity of soil and water conservation measures, defined as the maximum quantity of suitable soil and water conservation measures contained in a region, were determined for the Loess Plateau based on zones suitable for establishing terraced fields, forestland and grassland with the support of geographic information system (GIS) software. The minimum possible soil erosion modulus and actual soil erosion modulus in 2010 were calculated using the revised universal soil loss equation (RUSLE), and the ratio of the minimum possible soil erosion modulus under the capacity of soil and water conservation measures to the actual soil erosion modulus was defined as the soil erosion control degree. The control potential of soil erosion and water loss in the Loess Plateau was studied using this concept. Results showed that the actual soil erosion modulus was 3355 t?km^-2?a^-1, the minimum possible soil erosion modulus was 1921 t?km^-2?a^-1, and the soil erosion control degree was 0.57 (medium level) in the Loess Plateau in 2010. In terms of zoning, the control degree was relatively high in the river valley-plain area, soil-rocky mountainous area, and windy-sandy area, but relatively low in the soil-rocky hilly-forested area, hilly-gully area and plateau-gully area. The rate of erosion areas with a soil erosion modulus of less than 1000 t?km^-2?a^-1 increased from 50.48% to 57.71%, forest and grass coverage rose from 56.74% to 69.15%, rate of terraced fields increased from 4.36% to 19.03%, and per capita grain available rose from 418 kg?a^-1 to 459 kg?a^-1 under the capacity of soil and water conservation measures compared with actual conditions. These research results are of some guiding significance for soil and water loss control in the Loess Plateau.