生成周期视角下旅游业内部绩效评价及其影响机制——以张家界为例     

麻学锋  刘雨婧 《地理研究》2016,35(10):1983-1998

在旅游业绩效内涵及相关理论研究基础上,界定旅游业内部绩效概念及其特征,从产业生成周期视角,评价和探讨旅游业内部绩效及其影响机制。采用1989-2013年张家界旅游相关数据,结合小波分析、耦合—协调模型和路径分析等研究方法,研究发现：① 出现期,张家界旅游处于投入阶段,产业结构极度失调,高度化上下波动,内部绩效均值为1.199;② 生成期,旅游经济快速增长,结构合理性中度失调,高度化周期波动,内部绩效均值为6.265,经济绩效表现较好;③ 发展期,旅游经济绩效经历了三次下降,产业结构优质协调,高度化在调整中稳步前进,内部绩效均值为47.885,结构绩效表现较好;④ 影响机制：总体来说,经济水平、交通、旅游总需求社会固定资产和政府支出是主要影响因子,但不同阶段作用机理有所差异。研究对张家界旅游业理性发展及可持续发展具有一定科学指导意义。  相似文献   

累积绝对速度CAV在中国三代核电站地震监测中的应用     

陈志高  黄俊 《大地测量与地球动力学》2016,36(5):467

介绍中国将要建成的三代核电站和目前已建成的二代核电站的地震监测原理。通过处理国内地震数据,分析可能影响三代核电站安全运行的地震的特点,并将三代核电站地震报警方式与二代核电站地震报警方式进行对比。结果表明,三代核电站OBE报警方式能有效减少二代核电站OBE报警中的误报和漏报,是一种更加稳健的核电站地震监测方法。  相似文献   

祁连山木里地区侏罗系窑街组烃源岩生烃潜力评价   总被引：1，自引：0，他引：1  

徐久晟  文志刚  胡道功  张耀玲  戚帮申 《地质力学学报》2015,21(3):446-452

祁连山木里坳陷侏罗系窑街组煤系泥岩和煤有机质丰度、有机质类型和有机质成熟度分析结果表明, 窑街组煤系泥岩为好的烃源岩, 有机质类型为Ⅱ₁型, 处于成熟阶段, 以生油为主, 生气为辅; 煤为差等烃源岩, 有机质类型为Ⅲ型, 处于成熟阶段, 富氢基质镜质体含量高, 具有一定的生烃潜力。综合其它层位烃源岩分析结果, 认为窑街组煤系泥岩和晚三叠世尕勒得寺组湖相泥岩为祁连山木里地区天然气水合物的主要气源岩。   相似文献   

Hydrological processes of glacier and snow melting and runoff in the Urumqi River source region,eastern Tianshan Mountains,China   总被引：1，自引：0，他引：1  

Meiping SUN  Xiaojun YAO  Zhongqin LI  Mingjun ZHANG 《地理学报(英文版)》2015,25(2):149-164

Hydrological processes were compared, with and without the influence of precipitation on discharge, to identify the differences between glacierized and non-glacierized catchments in the Urumqi River source region, on the northern slope of the eastern Tianshan Mountains, during the melting season (May-September) in 2011. The study was based on hydrological data observed at 10-min intervals, meteorological data observed at 15-min intervals, and glacier melting and snow observations from the Empty Cirque, Zongkong, and Urumqi Glacier No.1 gauging stations. The results indicated that the discharge differed markedly among the three gauging stations. The daily discharge was more than the nightly discharge at the Glacier No.1 gauging station, which contrasted with the patterns observed at the Zongkong and Empty Cirque gauging stations. There was a clear daily variation in the discharge at the three gauging stations, with differences in the magnitude and duration of the peak discharge. When precipitation was not considered, the time-lags between the maximum discharge and the highest temperature were 1-3 h, 10-16 h, and 5-11 h at the Glacier No.1, Empty Cirque, and Zongkong gauging stations, respectively. When precipitation was taken into consideration, the corresponding time-lags were 0-1 h, 13 h, and 6-7 h, respectively. Therefore, the duration from the generation of discharge to confluence was the shortest in the glacierized catchment and the longest in the catchment where was mainly covered by snow. It was also shown that the hydrological process from the generation of discharge to confluence shortened when precipitation was considered. The factors influencing changes in the discharge among the three gauging stations were different. For Glacier No.1 station, the discharge was mainly controlled by heat conditions in the glacierized region, and the discharge displayed an accelerated growth when the temperature exceeded 5°C in the melt season. It was found that the englacial and subglacial drainage channel of Glacier No.1 had become simpler during the past 20 years. Its weaker retardance and storage of glacier melting water resulted in rapid discharge confluence. It was also shown that the discharge curve and the time-lag between the maximum discharge and the highest temperature could be used to reveal the evolution of the drainage system and the process of glacier and snow melting at different levels of glacier coverage.  相似文献   

珠江口盆地花岗岩成因探讨及其对油气资源指示 意义   总被引：2，自引：0，他引：2       下载免费PDF全文

刘安  吴世敏 《地学前缘》2011,18(1):141-148

珠江口盆地燕山期花岗岩地球化学、地球物理等特征分析表明,其形成缘于中生代太平洋板块向华南大陆的俯冲,并引起华南大陆边缘岩石圈等温面上隆及上地壳硅铝质岩石的多次重熔。花岗岩层形成后的区域性剥蚀作用导致盆地隆起部位花岗岩穹窿和背斜的形成;此后,新生代沉积物覆盖在花岗岩背斜和穹窿之上并形成披覆背斜,该类构造为珠江口盆地重要的含油气构造类型。在中生代时,东沙隆起及其以北具有高地温场,花岗岩发育的特点;南部坳陷带则表现低地温场和中生代沉积等特点。中生代烃源岩演化程度相对较低,它在新生代时期具备二次生烃的可能性。  相似文献   

夏秋季南海北部陆坡区氧化亚氮的分布、产生及海-气交换通量     

任妍妍  郑文静  叶旺旺  张云燕  张桂玲 《海洋与湖沼》2017,48(1):29-39

分别于2014年10月和2015年6月对南海北部陆坡区进行了调查,研究了其溶存氧化亚氮(N_2O)的分布、产生并估算了其海-气交换通量。结果表明:秋季南海北部表层海水中溶解N_2O浓度为(8.19±0.79)nmol/L,饱和度为132.5%±13.4%;夏季表层海水中溶解N_2O浓度为(7.72±0.56)nmol/L,饱和度为135.5%±9.7%。夏季由于受到珠江冲淡水的影响,表层N_2O浓度随盐度升高呈降低趋势,秋季调查区域东北部受到穿过吕宋海峡的黑潮分支表层水的影响,N_2O浓度较低。结合文献资料,南海北部陆坡区表层N_2O浓度季节变化特征为春末秋季夏季,同一季节,南海陆坡区的N_2O浓度高于其他区域。温度是影响N_2O分布的重要因素,ΔN_2O与表观耗氧量(apparent oxygen utilization,AOU)和NO_3~ˉ的显著相关说明硝化作用是南海水体中N_2O产生的主要机制,由此估算硝化作用的N_2O产率分别为秋季0.033%,夏季0.035%。利用N2000和W2014公式分别估算了该区域秋季和夏季N_2O的海-气交换通量:秋季为1.81—23.81(11.11±6.52,平均值±SD,下同)(N2000)和1.73—24.38(11.30±6.81)(W2014),夏季为1.01—21.57(7.04±6.10)(N2000)和0.75—22.69(6.94±6.49)(W2014),单位均为μmol/(m~2·d)。初步估算出南海北部陆坡N_2O释放量为0.055Tg/a,约占全球海洋总释放量的0.39%,远高于其面积比,说明南海北部陆坡是N_2O释放的活跃海域,是大气N_2O的重要源。  相似文献   

华北北部凌源-宁城盆地蓟县系洪水庄组生烃潜力分析——以小庄户剖面为例     

宗文明  郜晓勇  孙求实  蒋兴超  吴桐  周铁锁 《地质与资源》2017,26(4):370-376

通过岩石热解、饱和烃色谱-质谱、镜质体反射率等分析测试方法,对凌源-宁城盆地小庄户剖面蓟县系洪水庄组烃源岩的有机质丰度、类型及成熟度进行了详细分析,综合评价了其生烃潜力.研究结果表明,蓟县系洪水庄组有机碳的含量分布在0.42%~2.65%,平均值为1.46%。应用Pr/n-C₁₇与Ph/n-C₁₈的相关关系及干酪根碳同位素分析,判断其有机质类型为Ⅰ型和Ⅱ₁型.镜质体反射率R_o主要分布于0.62%~0.81%之间,平均为0.73%;岩石热解参数T_max主要为429~447℃,平均值为440.44℃,指示洪水庄组烃源岩属于成熟演化阶段。综合评价认为,凌源-宁城盆地蓟县系洪水庄组具有良好的生油气潜力.  相似文献   

我国不同原油裂解成气动力学研究     

王民  黄靖轩  卢双舫  王永兴  薛海涛  李吉君  杨金秀  张亮  张宏 《海相油气地质》2017,22(2)

提供了我国海相、湖相原油的黄金管裂解成气热模拟实验数据和裂解成气的动力学参数。对比分析典型样品裂解生气特征、升温速率与温度对油裂解成气的影响表明:我国海相、湖相原油裂解成气门限温度、消亡温度差异不大,但与国外样品差异明显;源内和源外原油裂解成气过程差别明显,源内原油热稳定性弱于源外原油热稳定性,在油裂解气评价中应该考虑排烃效率的影响;温度是原油裂解的主要控制因素,温度高于180℃时,原油裂解过程主要在10 Ma内完成,且液态烃消亡温度要高于200℃。本次研究的实验结果、动力学参数及相关结论可供盆地模拟和油藏勘探工作采用和借鉴。  相似文献   

汶川M_S8.0级地震成因三“层次”分析——基于深部电性结构   总被引：2，自引：1，他引：1       下载免费PDF全文

赵国泽  陈小斌  肖骑彬  王立凤  汤吉  詹艳  王继军  张继红  H. Utada  M. Uyeshima 《地球物理学报》2009,52(2):553-563

2008年5月12日汶川M_S8级地震的发生不是局部地区孤立的构造事件,研究汶川地震的孕震机制,应该把局部分析和区域分析相结合,关注地壳上地幔直至地幔过渡带的深部结构.基于近年来在东北、华北和汶川地震附近地区进行的深部结构电磁探测结果,结合地震学等其他资料,从太平洋板块的俯冲、印度板块的碰撞和松潘甘孜地块的推挤三个“层次”探讨分析汶川特大地震的成因.太平洋板块向亚洲大陆的俯冲作用,导致中国大陆东部地幔过渡带深度较普遍地存在着停滞的板片,它对汶川地震的影响不可忽视.印度板块与青藏高原的碰撞,使组成高原的各地块发生向北和向东的运动,各地块向东的运动作用于南北地震带中南段,影响到该区域的地震活动.松潘甘孜地块向四川地块的推挤,使松潘甘孜地块运动方向和龙门山断裂带形成“丁”字形结构,龙门山断裂带显示为较陡直的电性边界,加剧了汶川地震前的应力积累,可能是汶川地震发生的最直接的诱因.  相似文献   

Slope runoff study in situ using rainfall simulator in mountainous area of North China     

XU Jing-Ji  YANG Cong  LIU Chang-Meng  SONG Xian-Fang  HU Shan-Shan  LI Fa-Dong  TANG Chang-Yuan 《地理学报》2009,30(4):461-470

Simulated rainfall is a valid tool to examine the runoff generation on the slope.13 simulated rainfall experiments with different rainfall intensities and durations are completed in a 5 m ×10 m experimental plot in mountainous area of North China.Simultaneously,rainfall,surface runoff,soil-layer flow,mantel-layer flow and soil moisture are monitored respectively.From the results,it is found that the hydrographs in all layers have the characteristics of rapid rise and fall.The recessions of surface flow and soil-layer flow are much faster than that of mantel-layer flow.Surface flow,the main contributor,makes up more than 60% of the total runoff in the study area.It even exceeds 90% in the cases of high intensity rainfall events.Runoff coefficient(ratio of total runoff to rainfall amount) is mainly influenced by rainfall amount,rainfall intensity and antecedent soil moisture,and the relationship can be well expressed by a multiple linear regression function α = 0.002P + 0.182i + 4.88Wa-0.821.The relation between the rainfall intensity and the lag time of three flows(surface runoff,soil-layer flow and mantel-layer flow) is shown to be exponential.Then,the result also shows that the recession constant is 0.75 for surface runoff,is 0.94 for soil-layer and mantel-layer flow in this area.In this study area,the dominant infiltration excess runoff is simulated by Horton model.About 0.10 mm/min percolation is observed under the condition of different rainfall intensities,therefore the value is regarded as the steady infiltration rate of the study area.  相似文献