土地分离与共享框架的研究现状及应用拓展

“土地分离”与“土地共享”是2种不同的土地利用思维方式,反映人类土地利用的决策选择。中国有大量包含土地分离和共享思维的实践,但缺乏将这些实践案例纳入统一体系的研究范式。土地分离与共享框架最初用来探索粮食生产与生物多样性保护的权衡关系。经过10多年的发展,其理论内涵和研究内容不断丰富,是地理资源与环境领域重要的研究议题。论文在解析土地分离与共享框架内涵的基础上,综述土地分离与共享框架的相关研究成果,探讨土地分离与土地共享的策略选择。研究发现土地分离与共享相关研究存在从农业环境主题向城市管理主题转化的趋势,而且除了强调单一生物多样性保护和农业生产外,还有少数研究开始关注碳储存、土壤保持等其他生态系统服务类型;尽管土地分离与土地共享策略各有其优势和局限,但在目前的研究和实践中,土地分离比土地共享更受青睐。论文基于土地的多功能性进一步扩展该框架在城市用地管理中的应用,可为复杂社会—生态系统可持续发展提供路径指导。     

Wintertime meso-scale horizontal distribution of large tintinnids in the southern Yellow Sea

Spatial distribution of some large tintinnid species (nominally > 76 μm) is investigated on samples vertically towed in the southern Yellow Sea in winters of 2001 to 2004. Nine tintinnid species are recorded: Codonellopsis morchella, Stenosemella pacifica, S. steini, Tintinnopsis schotti, T. radix, T. karajacensis, Eutintinnus tenuis, Parafavella sp., Leprotintinnus neriticus, of which C. morchella and T. radix dominated in the warm tongue-shaped zone of the Yellow Sea Warm Current (YSWC), and S. pacifica i...     

延龙图地区城市生态用地生态重要性空间识别与保护

采用加权指数求和法,从生态服务功能、景观生态空间格局以及生态敏感性3方面建立生态重要性空间识别指标体系,通过专家咨询和层次分析法确定各评价指标分级赋值标准和权重,结合GIS空间分析功能对“延龙图”（延吉-龙井-图们）地区生态用地的生态重要性进行空间识别,将其划分为3个级别：极重要、重要和一般重要,以反映不同生态用地保护级别和建设管制要求。结果表明,延龙图地区极重要生态用地占生态用地面积的25.720%,主要为耕地、林地和水域;重要生态用地占生态用地面积的39.500%,主要为林地和耕地;一般重要生态用地占生态用地面积的34.780%,以林地为主。     

EFFECTS OF LOW MOLECULAR WEIGHT CHITOSAN (LMC-1) ON SHRIMP PRESERVATION

This study on the effects of low molecular weight chitosan (LMC- 1) and shrimp preserving agentssuch as phytic acid (PA), sodium bisulfite (SB), and crustacean preservative (CP) on the preservation ofshrimp (Trachypenaeus curvirostris) and the bacteriostasis of LMC-1 showed that: (1) Different LMC-1conontration has different bacteriostasis on E. coIi, B. subtilis and S. aureou: (2) LMC-1 and CP arebetter than PA and SB for preserving the freshness of shrimp stored at 4℃.     

On long-wave breaking I. Consideringnth power bottom friction

Longwave breaking is the agent for many important upper ocean layer processes including the transfer of horizontal momentum. In a previous study on the process of longwave breaking, only linear bottom friction was considered. In this paper, we discuss the longwave breaking phenomena in the more general case ofnth power bottom friction. Using the theory of blowup of solution, the criterion for the time and location of the longwave breaking can be obtained. Contribution No. 2559 from the Institute of Oceanology, Chinese Academy of Sciences. This project was supported by NSFC (No. 49376254).     

中国历史文化名村的时空分布特征及成因

古村落是具有文化遗产性质的乡村聚落,选取古村落发展中最具代表性的国家级历史文化名村来分析中国古村落的空间分布特征,探讨其影响因素和分布原因,从而进一步引导中国乡村地区的同步发展,促进城乡一体化进程。研究表明:① 我国历史文化名村主要沿河流分布、多是历史上的经济文化中心、交通要塞和文明的发祥地,并形成了3 大集中区、3 大相对集中区和4 大过渡扩散区,孕育了6 个文化区;② 中国历史文化名村建造时间跨度较大,但多集中在唐宋明清4 个朝代,明朝保留下来的古村落最多,分布范围最广;③ 造成中国历史文化名村分布不均衡的主要原因有资源禀赋特点、评定标准的局限、依托腹地的经济发达程度和区域政策导向。     

高精度磁测与四道γ能谱在金矿床上的应用—─以阿希金矿为例

对阿希金矿床高精度磁测结果分析，发现了环状磁异常，它是火山岩地区控矿构造—环状构造的反映。对该异常进行了延拓处理，得出其浅部为环状和放射状断裂，深部为南北向断裂。对该矿床又作了四道γ能谱测量，发现它可以清晰的划分矿化蚀变带与围岩的界线，其基本规律是：钾道和总道含量在矿化蚀变带上明显升高，而钍道则明显下降     

A high resolution lithospheric magnetic field model over China

CHAMP satellite data and ground-based magnetic observations are used and combined to map the lithospheric magnetic field over China by means of the revised spherical cap harmonic analysis(R-SHCA)modeling technique.The magnetic field is described to a spatial resolution of 150 km at the mean Earth’s radius,which represents a good compromise between the resolutions afforded by surface and satellite data.We compare the magnetic anomalies modeled at the regional scale with composite regions containing large-scale of tectonic structures.These regions,including the Tarim Basin and the Tibetan Plateau,are correlated with regional magnetic anomalies at satellite altitude but contain a significant number of small-scale and complex magnetic structures at the mean Earth’s radius.These magnetic anomalies are globally consistent with the known geological features in China but also offer a way to delineate the contours of the geological blocks and to discuss the connection between magnetic anomalies and the heat flow distribution in this region.