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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.
为做好超标洪水调度、保障流域防洪安全,开发建设了由基于水文水动力学耦合的超警超保风险区域预警模型与基于水文学法的洪水淹涝风险快速评估模型共同组成的超标特大洪水风险预警系统,该系统在太湖流域预报调度一体化系统中通过智能交互方式进行模型与系统的紧密集成,实现了预报调度成果的可视化。基于水利一张图的超警超保与淹涝动态展示,实现了预报产品从点到面、从常规预报到影响预测的突破,以及洪水风险由静态评估向实时快速动态分析的转变。应用结果表明:系统在2020年太湖流域性大洪水中累计发布超警超保风险提示39期、洪水淹涝风险评估4期,预测结果与实际基本一致,为科学调度防御超标洪水提供了技术支撑,避免了江苏省苏州市3万多的人员转移,有力保障了太湖流域防洪安全。 相似文献
5.
利用太湖常规监测点的监测资料,在黎曼近似解模型的基础上建立了太湖二维藻类生长模型,该模型采用有限体积法及黎曼近似解对二维水流水质方程组逐时段、逐单元进行求解,将每个时段各个单元ρ(TN)及ρ(TP)的模拟值传递到藻类的生长项,从而模拟出藻类的生长过程,率定验证结果表明,该模型能较好地模拟藻类的生长过程,并能对太湖水体富营养化进行预测。 相似文献
6.
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
7.
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
8.
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
9.
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
10.
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