1) Lishihe river
李石河
1.
The design for Lishihe river landscape is an important landscape construction project in Fushun City Economic Development Zone.
李石河景观设计是抚顺市经济开发区景观建设的重要内容之一,本设计以实现自然与城市、自然与社会和谐共生为中心,将李石河两岸建设成为具有亲切感和活力的公共空间。
2) Li Shi
李石
1.
Li Shi and the Relations which Studies with Shu Academic of Song Dynasty;
李石及其与宋代蜀学的关系
3) Licun Estuary
李村河口
1.
Simulation Study on Mercury Released from Sediment to Atmosphere in Summer and Winter at Licun Estuary of Jiaozhou Bay;
夏冬两季胶州湾李村河口沉积物/大气汞的释放模拟研究
2.
In this study, we examined the Total Organic Carbon (TOC), organic carbon to nitrogen ratio (C/N), Acid Volatile Sulfide (AVS), and heavy metal contents of four sediment cores collected from the Licun Estuary in the northeast of Jiaozhou Bay near Qingdao, China.
本论文以胶州湾李村河口区为研究对象,通过4个沉积柱样的分析测试,对港湾内河口区沉积物中的有机质(TOC)、酸可挥发硫化物(AVS)及重金属的环境响应进行了系统的探讨,发现由于湾内河流流量较小、水动力较弱,且港湾有机生产力较强,只有紧贴河口的细粒(泥质粉砂)区域的有机质才受陆源控制,有机碳含量较高(JZB-2柱平均为1。
3.
The reactive metals, AVS, and organic carbon, etc, were analyzed in 9 short column sediment cores from the Licun estuary in the Jiaozhou Bay.
对胶州湾李村河口9个短柱状样沉积物中活性金属、AVS和有机质含量等参数进行了分析。
4) Licun River
李村河
1.
Analysis of Main Pollutant Sources Affecting Seawater Quality in the Jiaozhou Bay Area——Assessment of Present Water Quality in the Licun River and Its Main Tributaries;
影响胶州湾海域海水水质的主要污染源分析——李村河及其主要支流流域水质现状评价
5) Lee H.Y
李河荣
1.
Discussion on Silurian in Sino-Korean Plateau:in commemoration of distinguished micropaleontologists AN T.X. of China and Lee H.Y. of Korea;
中朝地台的志留系—纪念中、韩两国杰出的微体古生物学者安太庠和李河荣
6) Li Yinhe
李银河
1.
The book entitled SM Subculture delivered by Li Yinhe,where some western theor.
李银河介绍西方虐恋理论和实践的《虐恋亚文化》是解读王小波小说的一把钥匙。
2.
There haven taken place a great disturbance in the press of our country after the famous scholar Li Yinhe put forward a requirement that charge for interview, which led to a great number of discussion about legitimacy of paying interview.
著名学者李银河提出收费才接受采访的言论在我国新闻界掀起了轩然大波,关于“付费采访”合法性的讨论风起云涌。
补充资料：石河
| 石河 rock river 山坡上寒冻风化产生的大量碎屑沿坡滚落到凹地、沟谷中，厚度逐渐加大，在重力作用下发生的整体运动。大型的石河又称石冰川。温度变动对石河的运动起着重要作用，会引起碎屑空隙中水分的反复冻结和融解，导致碎屑整体的膨胀和收缩，促使石河向下运动。中央部分比两侧流速快，湿润气候时比干燥气候时的流速快。石河中岩块长期运动至山麓停积下来，形成石流扇。石河停止运动是气候转暖的标志，此时角砾表面开始生长地衣苔藓，有时在石河上生长树木或堆积新沉积物。这些石河多分布在多年冻土的南界（北半球）或高山冻土的下界。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条