旅游者感知文化距离对民族文化遗产体验意愿影响机制

基于“认知－情感－意动”理论框架,引入旅行生涯模式理论,构建了包括旅游者感知文化距离、感知新奇、感知文化风险、文化体验意愿和旅游经验等构念在内的模型,以2个典型民族文化遗产旅游目的地——广西龙脊梯田和贵州肇兴侗寨为案例地,运用PLS-SEM工具检验结构模型,结果表明：1）认知阶段对情感阶段的影响显著,即TPCD正向影响感知新奇和感知文化风险,情感阶段对意动阶段的影响亦显著,即感知新奇正向影响文化体验意愿而感知文化风险负向影响文化体验意愿;2）感知新奇与感知文化风险在TPCD对文化体验意愿的影响过程中起中介作用,该结论验证了旅游者文化体验意愿产生的心理过程遵循CAC理论模型,这是一个认知影响情感进而影响行为意愿的递进过程;3）认知积累在认知阶段对情感阶段影响路径中的调节作用部分显著,即旅游经验负向调节TPCD对感知文化风险的正向影响,但在TPCD对感知新奇的正向影响过程中的调节效应不显著。结论表明,感知文化距离在特定的国内旅游情境下同样对旅游者行为意愿有显著影响,这在一定程度上拓展了旅游文化距离研究的对象范围。     

面向星群的遥感影像智能服务关键问题EI北大核心CSCD

全天时、全天候和全球的遥感信息实时智能服务是对地观测系统建设的目标。近几年来,随着我国高分专项和商业卫星的发展,在轨卫星数量急剧增加,对地观测能力得到极大增强,使得传统的单星和星座卫星系统的运控、接收、处理和应用服务模式面临严峻挑战,亟须统筹规划卫星应用各环节资源,充分发挥多星协同优势,构建统一的遥感影像实时智能服务体系和系统。本文针对遥感星群卫星体系特点和对地观测用户需求特征,开展面向星群的遥感影像智能服务关键问题研究。提出了面向任务的全球多尺度语义描述网格,统筹全球动静态的任务语义描述,在此基础上重点分析了面向星群的自主任务管理、精准动态规划和协同智能处理等关键技术问题,形成集任务描述、任务管控、任务规划、在轨处理、终端分发一体化的星群智能服务技术体系。通过充分发挥星群协同的优势,结合在轨处理和人工智能技术来降低各环节时间延迟,提高数据处理精度,从而实现完全自动化和智能化的近实时星群智能服务,为对地观测的全天时、全天候快速高效智能服务奠定基础。     

Accumulation and speciation of selenium in Cardamine sp. in Yutangba Se Mining Field,Enshi, China

A naturally selenium-accumulating Cardamine sp. is growing in Yutangba Selenium Mining Field, Enshi area, Hubei Province, China, where the geochemical environment is selenium-enriched and endemic selenosis ever occurred in humans. The present study investigated the characteristics of accumulation, speciation and quantity of selenium in Cardamine sp. with HPLC-ICP-MS. Results show that Cardamine sp. can accumulate Se at most 1427 mg/kg in seedling leaves. Even after the biomass incensement of growing up, the plant still could accumulate Se up to several hundred of mg/kg in concentration. Moreover, the biomass enrichment coefficient （BEC） of Se is exceedingly high, in the seedling leaves mostly, higher than 50 mg/kg; in the range of 43.7-68 mg/kg; and the lowest value is higher than 3 mg/kg in mature fronds. Se is present in the plant predominantly in form of SeCys2 with the highest concentration in seeds; up to 1081 mg/kg as Se. In contrast, SeCysz levels are low during early growth period; they are 136.1 mg/kg as Se in seedling fronds and 39.4 mg/kg as Se in mature fronds, respectively. SeMet concentration is comparatively low; 10.6 mg/kg as Se in seedling frond and 5.3 mg/kg as Se in half mature fronds, respectively. This indicates that Cardamine sp. is extremely efficient in extracting Se from soil and translocating it into its above-ground biomass. Therefore, Cardamine sp., found in Yutangba Se Mining Field may be a new Se hyperaccumulator. It is still uncertain whether the Se-accumulation or detoxification of Cardamine sp. happens through the pathway of SeCys methylated to form Se-methylselenoCys or through the formation of Se-carboxymethyl- selenohomocysteine. Indeed, further study should be carried out on the determination of more Se species to explain the high Se hyperaccumulation in Cardamine sp.     

Fluid inclusion and H–O–C isotope geochemistry of the Yaochong porphyry Mo deposit in Dabie Shan,China: a case study of porphyry systems in continental collision orogens

The Yaochong porphyry Mo deposit in Xinxian County, Henan Province, China, is located in the Hong’an terrane, that is, the western part of the Dabie orogen. The Dabie orogen is part of a >1,500 km long, Triassic continental collision belt between the North China Block and the South China Block. Four types of vein are present. Paragenetically, from early to late, they are as follows: stage 1 quartz + K-feldspar ± pyrite ± magnetite vein; stage 2 quartz + K-feldspar + molybdenite ± pyrite vein; stage 3 quartz + polymetallic sulfides ± K-feldspar vein; and stage 4 quartz ± carbonate ± fluorite vein. Four compositional types of fluid inclusion, pure CO₂, CO₂ bearing, aqueous, and solid bearing, are present in quartz from the first three stages; only low-salinity aqueous fluid inclusions occur in quartz from the last stage. All the estimated salinities are ≤13.1 wt% NaCl eq., and no halite crystals were identified. Homogenization temperatures for the fluid inclusions from stages 1 to 4 are in the ranges of 262–501, 202–380, 168–345, and 128–286 °C, respectively, and estimated depths decrease from 6.9 to 8.9 km, through 6.2–7.2, to ~4.7 km. Quartz separates from the veins yielded a δ¹⁸O value of 7.7–11.2 ‰, corresponding to δ¹⁸O_H2O values of ?1.3 to 6.9 ‰ using temperature estimates from fluid inclusion data; δD_H2O values of fluid inclusion vary from ?80 to ?55 ‰, and δ¹³C_CO2 from ?2.3 to 2.7 ‰, suggesting that the ore-fluids evolved from magmatic to meteoric sources. We conclude that the ore-forming fluid system at Yaochong was initially high temperature, high salinity, and CO₂-rich and then progressively evolved to CO₂-poor, lower salinity, and lower temperature, by mixing with meteoric water, which results in ore precipitation.     

Experimental study on bar formation in a scouring process

Bars are widely thought to be large sediment bodies formed under sediment supply. Nevertheless, little has been known on how they form in sediment scouring processes. In this study, we carried out a flume experiment to study the formation of bars without sediment supply. The experiment was divided into two stages. In the first stage, the discharge was successively increased; in each discharge step, the disturbance from upstream and downstream boundaries had little influence on the flow. We observed that no bars formed in this stage. In the second stage, we kept a small discharge at the flume inlet. In this stage, the bars emerged from the fluctuated bed topography with millimeter-scale bed forms by headcut initiated from the outlet. As the headcut migrated upstream, the accompanying undercut gradually forced the unconfined flow run into the low-elevation zone, lowering the water level and inducing the outcrop of regions free from the incision (i.e., bars). At the end of the experiment, a relatively stable topography formed under the joint effect of the upstream migrating headcut, the following undercut after the headcut and the lateral erosion on the emerged bars. The requirements for the formation of bars and the distinctive characteristics of the bars induced by headcut were investigated. This study shows that bars can form in a scouring process under appropriate conditions, and the headcut may be one of the precipitating factors for the formation of bars in natural rivers.     

Earth pressure evolution of the double-row long-short stabilizing pile system

Double-row stabilizing piles provide larger stabilizing force and lateral stiffness than the single ones. However, the loading shared by the front and rear pile is not the same with each other because of the shadow effects. A double-row long-short stabilizing pile system is verified in this paper. Physical model tests are used to investigate the influence of short rear pile on the earth pressures evolution in the stabilized soil. Numerical models are established and calibrated with the applied displacement–force curve and monitored earth pressure in the physical model test. The influence of the short rear stabilizing pile on the soil–pile interaction is further investigated based on the numerical model. The soil–pile relative displacement, total stabilizing force and bearing proportion of front and rear stabilizing pile are used to evaluate the soil–pile interaction. It is concluded that the total stabilizing force and bearing proportion of front and rear stabilizing pile are not significantly influence by the short rear stabilizing pile when the double-row piles are arranged in a line. When the double-row piles are arranged in a zigzag form, the total resistance provided by the double-row stabilizing piles decreases as the short rear piles are being used.     

基于时序InSAR的京津高铁北京段地面沉降监测

京津高铁是中国第一条高速运行的城际铁路,其安全运行对轨道的平顺性有着严格的要求。地面沉降,尤其是不均匀地面沉降会引起部分路基和桥梁变形,威胁着高速铁路的运营安全。合成孔径雷达干涉测量技术可以大范围监测地表形变,对高速铁路沿线地面沉降具有较好的监测能力。本文以45景高分辨率TerraSAR-X 数据为基础,采用 PS-InSAR技术监测京津高铁北京段沿线地面沉降,获取京津高铁北京段沿线地面沉降的分布信息,从动静载荷视角结合北京地区地下水、断裂带、地质条件和含水层系统介质等数据,综合分析高铁沿线不均匀地面沉降的原因,为京津高铁的安全运营提供技术支撑。研究结果表明：京津高铁北京段沿线地面沉降发展在空间上存在一定差异性,北京南站至十里河区间,年沉降速率小于10 mm/a; 至十八里店区间,年沉降速率在10~40 mm/a范围内浮动;过亦庄站至东石村以东区间,最大年沉降速率达到90 mm/a;至永隆村以西,年沉降有所缓解,往东至坨堤村,沉降较为稳定,年沉降速率小于10 mm/a。地下水超采是沿线区域地面沉降的主要因素,动静载荷共同作用下对地面沉降产生一定的影响,沿线地面沉降一定程度上受到南苑—通县断裂带和旧宫断裂带构造控制,沉降量较大的路段位于粘土层较厚的大兴迭隆起。