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排序方式: 共有911条查询结果,搜索用时 15 毫秒
1.
青海湖旅游区生命周期问题探讨 总被引:2,自引:0,他引:2
肖景义 《青海师范大学学报(自然科学版)》2003,(1):88-90
本文立足青海实际,在分析影响青海湖旅游区生命周期的诸因素基础上,提出了延长该区旅游生命周期的具体措施。 相似文献
2.
本文用麦夸算法构造高原鼠兔体重生长的Logistic和Compertz曲线模型,其结果表明:Logistic曲线比Gompertz曲线更优化,Logistic模型比逻辑斯谛-指要饱和模型的精确度更高. 相似文献
3.
青海城镇体系经历了发韧期、奠基期、转型期3个发展历程.在这一过程中,湟水谷地最先拉开了城镇发展的历史帏幕,随后逐步向西扩展进入青海湖地区.宏观上,从农耕区向农牧交错区渗透,进而向游牧区拓展,反映了社会历史进程和地域开发进程的调控作用,因此城镇分布数量和密度呈现出农耕区—农牧交错区—游牧区逐级递减的趋势.中观上,以河流为脉络,城镇发展或溯源而上伸入高原腹地,或向河谷两岸推进,进入山区,表现为从优势生存空间向劣势生存空间的时空转化,城镇数量与密度呈现出川水地区—浅山地区—脑山地区的递减趋势.微观上,河谷农耕区城镇选址多位于河流阶地上,土地肥沃,取水便利;而牧区城镇的选址却往往与水草丰美的牧场相关,映射出古代城镇对自然条件和自然物质基础的依赖性.总体而言,青海省城镇兴起和发展的动力,主要来自于外部中央行政建制和军事据点的设置,而非城镇内部社会经济自我发展.就单个城镇而言,民族文化、民族宗教与民族贸易的亲合关系和响应力,是城镇成长的主要推进剂. 相似文献
4.
Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau 总被引:3,自引:0,他引:3
Scientific evidence for the upper limit of farmland is proposed. Shallow gully erosion is one of erosion types distributed
extensively on sloping farmland in the hilly regions of the Loess Plateau. Field observation and aerial photos interpretation,
as well as laboratory experiments show that the shallow gully erosion occurring on the steeper farmland in the hilly regions
of the Loess Plateau is an important factor leading to intensive erosion on slope, because of its extensive distribution and
intensive runoff collection. The data on the formation, development and distribution of shallow gullies on sloping farmland
indicate that critical slope gradient for shallow gully initiation ranges from 15 to 20 degrees with an average of 18.2 degrees.
Therefore, it is suggested that critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau
should be kept within the critical slope gradient for shallow gully initiation to prevent shallow gully formation in order
to control soil loss more effectively. But as the first step, the cultivation on the slopes with slope larger than 25 degrees
where the maximum erosion occurs should be strictly forbidden. 相似文献
5.
Discovery of eclogite at northern margin of Qaidam Basin, NW China 总被引:19,自引:0,他引:19
Jingsui Yang Zhiqin Xu Haibing Li Cailai Wu Junwen Cui Jianxin Zhang Wen Chen 《科学通报(英文版)》1998,43(20):1755-1755
Eclogite was first discovered at the northern margin of the Qaidam Basin in this study. It occurs as pods in the gneiss sequence of Middle to Upper Proterozoic age and is mainly composed of garnet, omphacite, phengite and rutile. The garnets contain 44%-62% of almandine, 15%-33% of grossular and 12%-30% of pyrope molecules, and the omphacites contain 40%-46% of jadeite. Applying garnet_clinopyroxene thermometry and jadeite geobarometry, the peak conditions of eclogite facies metamorphism occurred at about (722±123)℃ and at the pressure of up to c. 22 ×10 8 Pa. 相似文献
6.
New evidence for the Qinghai-Xizang (Tibet) Plateau as a pilot region of climatic fluctuation in China 总被引:12,自引:1,他引:11
Over 40 a observed temperature data in 172 stations in China and historical proxy data were analyzed. Evidence suggested that
during 1980–1994, the warmest year appeared first in southeastern part of the Qinghai-Xizang (Tibet) Plateau (henceforth SETP)
and then gradually spread northwards and eastwards to eastern China. The climatic change on century time scale in recent 600
a shows 3 relatively warm and clod stages in China. Each warm and cold stage appeared first in Tibet Plateau (henceforth TP)
and then in the Qilian Mountains, then in the eastern parts of China. The warm and cold stages in TP were 10–60 a earlier
than in the eastern China. The facts show that TP is a pilot region of climatic fluctuation in China on the time scale shorter
than 103a. 相似文献
7.
青海省国外旅游客源市场时空结构研究 总被引:2,自引:0,他引:2
该文对青海省的国外客源市场从时间和空间结构上进行分析,期望对未来青海省开拓国际市场提供理论依据.从时间结构上看,青海省国外客源市场在上个世纪90年代发展比较缓慢,在21世纪初期出现了快速增长的趋势,年平均增长率达到10%左右.而从空间结构上看,客源市场国的数量虽然在逐步增加,但是大部分旅游人数仍然来自少数几个国家,旅游市场地理集中指数G值自20世纪90年代逐步下降,但在本世纪初又出现了上升的迹象.因此,本文提出了未来青海省在开拓国外客源市场方面,需要在因地制宜、联合开发、树立明确形象和迎接多方挑战的措施和局势下作好工作. 相似文献
8.
基于GIS的陇中黄土高原潜在生态环境评价研究 总被引:10,自引:0,他引:10
利用Arc/Info提供的主成分分析方法对陇中黄土高原潜在生态环境进行评价.首先选取对潜在生态环境影响较大的指标构建数字生态环境模型,然后对二级指标体系进行主成分分析,获得一级指标指数,最后对一级指标体系进行主成分分析,获得潜在生态环境评价指数.主要目的在于提供一种生态环境评价方法. 相似文献
9.
Lightning activity on the central Tibetan Plateau and its response to convective available potential energy 总被引:6,自引:0,他引:6
Lightning flash activities on the central Tibetan Plateau have been studied by using the satellite-based Lightning Imaging Sensor(LIS)database from January 1998 to July 2002.The lightning activity shows a clear diurnal variation on the central Plateau.The peak lightning activity appears at about 17:00 which is 3 h earlier than that in Jingxhou,Hubei in the same latitude belt nearby,indicating that the lightning activity is a sensitive indicator of solar heating on the Plateau.The lightning discharge is weaker on the Plateau than Jingzhou.Hubei and other low-altitude continental regions because of the lower convective available potential energy(CAPE)on the Plateau.The CAPE on the Plateau is 12 times lower than that in Jingzhou,Hubei,and 20 times lower than that in the sea-level region,such as Guangzhou and Florida.However,the sensitivity of lightning activity to CAPE changes on the Plateau is up to 30 times more sensitive than other prominent low-altitude regions. 相似文献
10.
YANGBao A.Braeuning SHIYafeng ZHANGJiawu 《科学通报(英文版)》2003,48(14):1446-1450
The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e. 相似文献