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排序方式: 共有602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.
《科学通报(英文版)》2008,(6)
High precision elevation measurements using DGPS were carried out along three representative tran- sects for the "Great Ear" area, a dry salt lake within the Lop Nor basin. Results indicate that the Lop Nor basin is only 5.2 m deep and its lowest point occurs at the center of the "Great Ear". In addition, the basin is asymmetric - steeper in the southwest (0.19‰) and gentler in the northeast (0.09‰). Points along the same "Great Ear" ring were found to have an identical elevation value, but different when from different ones (lower towards the center). The spacing of the "Great Ear" rings was found to be closely related with the surface steepness. The closer the "Great Ear" rings are spaced, the steeper the ground surface, and vice versa. These findings support the argument that the "Great Ear" rings are the former shoreline trails left behind by Lop Nor water during the last few episodes of recession towards its total dry up. A comprehensive analysis of the high precision elevation data, historical accounts, aerial and satellite photographs and imagery, and official topographic maps of the study area suggests that the "Great Ear" area in the Lop Nor basin was incorrectly mapped as being covered by a great body of water on the 1963 topographic maps. A re-interpretation of the 1958 aerial photographs and newer remote sensing imagery indicated that the "Great Ear" ring structure was already in place in 1958 and it continued to appear on the subsequent remote sensing data without any major changes. It is estimated that lake water in the "Great Ear" area of the Lop Nor basin disappeared between the late 1930s and early 1940s. 相似文献
3.
潘元伯 《合肥工业大学学报(自然科学版)》1993,(2)
通过对塌陷湖的实地勘查,运用水均衡原理,计算出该湖可供开采的水资源,认为该塌陷湖可作为淮北市供水后备水源地之一。 相似文献
4.
南四湖流域环境地质问题及其治理对策 总被引:7,自引:0,他引:7
南四湖流域的各种环境地质问题较突出,如水体污染、矿山环境地质灾害、地下水环境异常、南四湖淤积、地方病等。对流域环境地质问题的治理应综合考虑各种影响因素,建立完善的环境管理体制,增大环境治理投资比例,加强环境治理力度。 相似文献
5.
Holocene lake deposits of Bosten Lake, southern Xinjiang, China 总被引:9,自引:0,他引:9
B.Wünnemann 《科学通报(英文版)》2003,48(14):1429-1432
A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects. 相似文献
6.
鄱阳湖区有十分丰富的湿地资源,是我国重要的温地之一。有效保护和合理利用这一重要资源,对振兴湖区经济保护区域生态环境和实施可持续发展战略有十分重要的意义。本文通过分析鄱阳湖湿地资源特点,以生态经济战略为指导思想,着重探讨了保护和合理利用这一资源的发展思路和措施等,提出了鄱阳湖区实施可持续发展的几点建议。 相似文献
7.
A method of quantitatively calculating amount of allochthonous organic carbon in lake sediments 总被引:2,自引:0,他引:2
Conclusion The lake sediments have registered the information of palaeoclimate and palaeoenvironment in the lake itself and the regional
scale. This also leads to a complexity in study of the palaeolimnology by all kinds of proxies. How to purify these proxies
to indicate the palaeoclimate has become a problem to be solved. Most of the proxies can qualitively identify the percentage
of allochthonous and autochthonous organic components, e.g. δ13corg CD/TC. The model introduced in this note has provided a method of quantitatively calculating the amount of allochthonous
organic carbon. As for determination of regulating parameters, i.e. A1 and As, further work is still in need. 相似文献
8.
采用主成份分析法对18个湖泊的是总磷、总氮、耗氧量、生物量、透明度进行了分析,并对湖泊营养类别进行了评判。分析结果表明,湖泊营养状态是总磷、总氮,耗氧量、生物量、透明度综合作用的结果,其中总磷的作用最大,其次是总氮。 相似文献
9.
安燕 《青海师范大学学报(自然科学版)》2004,(3):60-63
采用最大方差正交旋转因子分析方法研究青海盐湖水化学特征,结果表明,青海盐湖水化学类型主要为硫酸镁盐型,盐湖卤水发育程度较深,没有碳酸盐型,K、Na、Mg//Cl、SO4-H2O是青海盐湖卤水的主要化学平衡体系等,这与青海盐湖的实际情况完全相符。 相似文献
10.
辽西地区义县组湖泊沉积层中产出著名的“热河生物群”化石,对于此时期古环境的研究一直是诸多学者关注的焦点.本文对大康堡层湖相纹泥展开研究,重建此时期古环境.通过野外及室内对纹泥组成、类型、厚度等方面的观测,对此时期古气候有了新的认识.纹泥厚度特征变化表明沉积期降水量和沉积速率逐渐减小,统计洪水沉积间纹层数量可指示沉积期洪水事件的频率和规模.结合近现代纹泥形成和保存条件,可知该地区沉积期湖泊水体较深,湖水分层,存在一个缺氧环境,具有较小的表面积/深度比,湖盆形态适合,未受到风的侵扰. 相似文献