旅游产业集群形成和演进过程研究--以敦煌市为例

通过对敦煌旅游产业集群的存在性进行判断,论述了敦煌旅游产业集群的形成过程,在此基础上对敦煌旅游产业集群形成的各阶段的特征进行了阐述,最后利用空间分析工具GIS对敦煌旅游产业集群主要成员在空间上的分布进行了分析。     

家蚕、野桑蚕线粒体Cyt b基因片段序列分析及分子进化研究

以家蚕中系一化地理品种延吉、印度多化品种迈索尔、欧系一化品种法 4 0 8油和中国镇江地区野桑蚕为材料 ,采用PCR技术扩增了其线粒体 (mitochondrialDNA ,mtDNA)细胞色素b(cytochromeb ,Cytb)基因 ,测定其 5′端5 91bp的核苷酸序列 ,并从GenBank中调取中系家蚕品种C10 8、夏芳 ,日系家蚕品种青熟 ,韩国家蚕品种Backokjam和日本野桑蚕的相应序列 ,进行同源性比较 ,发现日系家蚕品种青熟 ,印度家蚕品种迈索尔 ,欧系家蚕品种法 4 0 8油 ,韩国家蚕品种Backokjam和中系家蚕品种C10 8、延吉序列间的同源性最高 ,相互间均为 10 0 % ;日本野桑蚕与各家蚕品种序列间的同源性约 94 %～ 95 % ;中国野桑蚕与各家蚕品种序列间同源性约 98%～ 99%。分子进化树分析显示日本野桑蚕和各家蚕品种相应序列的分歧时间远远早于中国野桑蚕与各家蚕品种序列的分歧时间 ,这是在分子水平上证实家蚕起源于中国野桑蚕的证据之一。     

黄河下游地区土地利用和生态系统服务价值的时空演变

基于黄河下游地区1990—2015年土地利用分类数据,运用土地利用变化动态度、土地利用转移矩阵,探究不同土地利用类型的变化程度及转移情况,运用当量因子法、热点分析、重心模型、地理探测器探究黄河下游地区县域尺度生态系统服务价值的时空演变及其空间分异。结果表明:1)耕地、草地、未利用地面积逐渐减少,建设用地面积增加,耕地是建设用地面积增加的主要贡献者,建设用地扩张存在侵占耕地的现象。2)从时间尺度看,地区生态系统服务价值逐年减少;从空间尺度看,县域尺度的高值区逐渐减少,低值区逐渐增加;从地均生态系统服务价值的变化率来看,大部分县区的地均生态系统服务价值呈现持续降低趋势。3)地均生态系统服务价值的高值区与低值区空间集聚程度明显,但有逐渐弱化的趋势;生态系统服务价值的重心始终分布在山东省郓城县,重心迁移与两地区之间生态系统服务价值变化差值有关。4)黄河下游地区县域尺度地均生态系统服务价值空间分异受自然因素和社会经济因素共同作用的影响,是不同驱动因子共同作用的结果,其中人为综合影响指数对区域生态系统服务空间分异的影响最大。     

广西红壤果园土壤肥力演化与评价

本文着重探讨广西红壤果园土壤肥力在不同种植年限的演化特征,并利用数理统计软件—SPSS对果园土壤肥力进行综合评价。结果表明,广西红壤果园土壤肥力综合指标值(IFI)在0.17～0.25之间,果园土壤肥力属中下水平。不同年限果园IFI的变化趋势为"N"形走势,即新开果园在10年内IFI略有上升,10年后下降,而在30年以后果园土壤IFI又有增加。造成这种走势的原因,主要是由于受广西高温多雨的气候、果园环境和施肥管理等方面共同影响的结果。在近15年开垦种植的果园中,由于水土流失严重,果园土壤砂化,11～15年树龄果园的砂粒含量比0～5年树龄果园增加近23个百分点,而团聚体(>1mm)和有效阳离子代换量(ECEC)却分别减少24个百分点和3.0cmol/kg,果园土壤环境恶化。防止新开果园水土流失,改善新开果园土壤环境,为广西水果生产的当务之急。     

Andosol to Luvisol evolution in Central Mexico: timing, mechanisms and environmental setting

Surface and buried Andosols and buried Luvisols of the Nevado de Toluca Late Quaternary tephra-paleosol sequence (Central Mexico) were studied to show whether these soils present an evolutionary sequence and to determine the pedogenic mechanisms and environmental factors involved in the evolutionary process. Micromorphological observations and mineralogical composition of fine sand and clay fractions were used to detect type and succession of soil-forming process. Some of the buried Andosols, defined as “intergrade” Andosols, have a predominantly blocky structure, humus-depleted areas, redoximorphic features and thin clay coatings in Ah horizons. Clay fractions of buried Andosols contain halloysite besides amorphous components, whereas in modern Andosols, allophane is dominant. Luvisols have micro-areas with granular structure and abundant phytoliths in the groundmass of Bt horizons assumed to be the relict Andosol features. Luvisol clay fractions are dominated by halloysite and kaolinite. Primary minerals show micromorphological weathering features in all studied soils being stronger in Luvisols; however, even in Luvisols, sand fractions consist mostly of unstable volcanic silicates. We hypothesise that the studied profiles form an evolutionary sequence: Andosols–“intergrade” Andosols–Luvisols; the soil transformation is supposed to be linked to progressive crystallisation of 1:1 clay minerals. Comparing the Nevado de Toluca paleosol properties with the existing data on volcanic soil climo- and chronesequences and assessing the regional paleopedological and lacustrine records of Quaternary paleoclimates, we concluded that wet/dry climatic oscillations took place during the formation of the studied paleosols. Rapid crystallisation of 1:1 minerals occurred during dry phases, which speeded up the Andosol to Luvisol transformation and made it independent from the primary mineral weathering status. The Andosol to Luvisol transformation accelerated by climatic fluctuations is thought to be a common soil evolutionary pathway in the subtropical and tropical regions of recent volcanism, which suffered contrasting precipitation oscillations in the Quaternary.     

Variation of enzyme activities, CO2 evolution and redox potential in an Eutric Histosol irrigated with wastewater and tap water

An Eutric Histosol soil was irrigated for 4 years with municipal wastewater to compare its characteristics with a soil under natural rainfall that had never received wastewater and a soil that was irrigated with normal tap water. Four years irrigation of the soil with wastewater caused significant (P<0.001) increase in dehydrogenase, urease, acid and alkaline phosphate activities and CO₂ evolution, and reduced the redox potential (P<0.05). The influence of treatments and plant cover on soil properties were significant (P<0.05) under both salix and grasses, except for few properties (redox potential and urease and alkaline phosphatase activities). It is suggested that, although different toxicants, e.g. heavy metals, may accumulate in wastewater-treated soils, enrichment of soil with organic substances and nutrients stimulated CO₂ evolution and enzyme activities in the irrigated soil.     

Short and medium-term evolution of a coastal sector in Cadiz,SW Spain

The present paper is a combined study on the medium and short-term evolution of the littoral between Chipiona and Rota (SW Spain). The analysis of coastal evolution over a period of 24 years (i.e. medium-term), was carried out using six, well temporally spaced, photogrammetric flights. Cliff top and dune toe were used as shoreline indicators to solve problems related to the use of watermark in tidal environments. Short-term littoral variations were monitored monthly by means of an electronic theodolite over a period of 2 years. The width variations of the dry beach were surveyed by always using a constant, average value for the mean sea level position derived from the numerous surveys carried out. The obtained data was representative of both seasonal and annual variations.     

重大线性工程建设下山区乡村聚落空间演变

区域重大线性工程建设对传统山区乡村聚落的发展带来深刻的影响，乡村聚落发展步伐被打断或加快，驱动乡村聚落发展演变与重构，对这一影响和演变过程研究，有助于进一步理解区域重大线性工程与社会经济对传统山区乡村发展产生的外部性，为山区乡村振兴政策制定与发展策略选择提供参考。该研究以河北省赤城县大海陀乡为研究对象，基于1999、2009、2019年3期遥感影像数据，结合空间分析、景观格局指数、Voronoi图及Logistic回归模型，科学识别重大线性工程驱动下乡村聚落空间格局演变规律。结果表明：1）大海陀乡的乡村聚落在高速公路建设前后两个阶段表现出散乱式的斑块数量增长型扩张、集聚式的斑块面积增大型扩张的空间格局演变特征，重大线性工程建设加快了乡村聚落的扩张速度，促进了村庄聚落的内部集聚。2）重大线性工程的建设为构建聚落环境提供社会经济支撑，具有瞬时性与外界强干扰性，驱使大海陀乡乡村聚落从自然资源依附到经济社会依附的演变，形成跨域式的影响效应。3）大海陀乡乡村聚落呈现出"要素-结构-功能"的循环演变机制，内外因素的作用下主体行为的多元模式、自然发展演变与外界力量冲击下三生系统的耦合关系是乡村聚落演变的主要驱动力。京津冀一体化背景下，重大线性工程建设是加强城乡要素流通与转变村民生产生活观念的基石，需统筹城乡资源，加强规划引导与整治措施，促进村镇体系重构。     

Isozyme studies of genetic diversity and evolution in Hippophae

Summary To provide information on the genetic variation, differentiation and evolution in Hippophae seed samples of 25 populations from China, Finland and Russia were electrophoretically analyzed. Of six loci investigated, four were good genetic markers for identifying species and subspecies. The percentages of polymorphic loci per population were 40.3% and 62.5% at 0.95 and 0.99 polymorphic criteria respectively. The mean number of alleles per locus per population was 2.1. Total genetic diversity in the material was 0.4614. Genetic diversity partitioning showed that there was a large amount of diversity residing within geographical populations (0.1354), between subspecies within species (0.1046) and between species (0.2566) but not between geographical populations (0.0114). There were nearly twice as many negative fixation indices as positive ones in Hippophae populations. The phylogenetic tree agreed very well with botanic classifications of the species and subspecies and their geographical distributions, and quantitatively presented the genetic relationships of 25 populations. A detailed view of the evolutionary stages in Hippophae showed clearly a general decline of similarity as evolutionary divergence continued, which further explained the evolution process in Hippophae.     

青海湖地区耕地演变过程与影响机制分析

通过对青海湖地区耕地总面积、内部结构的变化过程和区域差异的分析，探讨了耕地变化的驱动机制。结果发现该区耕地面积变化呈现出平稳增加、激增、螺旋式增加和锐减的演变趋势，内部结构先呈现水浇地面积的显著增加，浅山地、脑山地相对减少的趋势，然后有出现水浇地和其它类型的耕地此消彼张变化阶段趋势；而耕地变化的区域差异也呈现出全区增长，区域不同步和全区减少的变化趋势。影响研究区耕地变化的原因，除自然因子外，国家大政方针和重大农业政策是导致这种变化的主要原因。