青海湖旅游区生命周期问题探讨

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。     

High precision topographic data on Lop Nor basin's Lake "Great Ear" ? and the timing of its becoming a dry salt lake

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.     

杨庄煤矿塌陷湖水资源勘查计算

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。     

西藏冰湖溃决频次与径流峰值流量相关性分析

冰湖溃决事件频繁发生,严重阻碍西藏自治区区域社会经济发展,影响社会稳定。随着气候变暖,冰川减薄后退,冰川径流量增大,冰湖溃决风险上升。基于西藏自治区东南地区的嘎隆拉冰川径流观测资料,分析了2017—2019年消融期间5—9月冰川径流变化特征,探讨了西藏1931—2020年冰湖溃决事件发生的频次与径流峰值流量的关系。结果表明：在1931—2020年,西藏地区共发生冰湖溃决事件32次,集中在5—9月发生;在旬变化上,极大值频次呈单峰结构,在7月上旬频次最高;冰湖溃决频次与径流峰值流量显著相关,相关系数为0.673,随着径流增大,冰湖溃决发生的频次逐渐增大。在气候变暖的背景下,冰川融化引发的冰湖溃决灾害应引起重视,要加强冰川消融径流观测及冰湖水位的监测,进行冰湖溃决洪水预报。     

南四湖流域环境地质问题及其治理对策

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。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

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.     

鄱阳湖流域综合规划与管理技术

从80年代开始实施的江西省山江湖工程是一项针对鄱阳湖流域可持续发展的流域综合管理工程。本文回顾了山江湖工程l0多年来实施流域管理战略的过程，分析了鄱阳湖流域生态系统恢复的发展阶段和新时期流域综合规划和管理的战略思想，同时提出了建立鄱阳湖综合流域管理信息共享平台和一种对流域生境进行制图以及对景观生态系统进行建模的综合评价方法。     

鄱阳湖湿地保护与区域可持续发展

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。     

A method of quantitatively calculating amount of allochthonous organic carbon in lake sediments

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. δ¹³c_org 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.     

应用主成份分析法评判湖泊营养类别

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。