1) subaqueous delta
水下三角洲
1.
Study of dynamic mechanism for the formation and growth of gullylandform on the subaqueous delta near old Huanghe River mouth;
黄河口水下三角洲海底冲蚀沟发育的动力机制探讨
2.
Based on the sediment supply from the Yangtze River and the analysis of the accretion/erosion of the subaqueous delta at the Yangtze Estuary in recent ten years,the accretion/erosion response of the subaqueous delta to the sharp decline of the sediment supply from the Yangtze River to the sea and the impoundment of the Three Gorges Reservoir was preliminarily discussed.
根据对近10年来长江入海泥沙量和河口冲淤的对比分析,探讨水下三角洲冲淤对长江入海泥沙锐减以及三峡工程运行的响应。
3.
In order to understand the characteristics of 137Cs geochemical distribution in the subaqueous delta of Changjiang Estuary,the sedimentary cores from thi.
文章通过对长江口水下三角洲采集的10个柱状样放射性核素137Cs的分析可以得知,长江口水下三角洲137Cs剖面中均存在清晰的最大蓄积峰,其峰值比活度介于5。
2) underwater delta
水下三角洲
1.
Sedimentary characteristics and environment of underwater delta in Minjiang Estuary Ⅱ.Sedimentary characteristics and environment since Late Pleistocene;
闽江口水下三角洲沉积特征及沉积环境Ⅱ.晚更新世—全新世沉积特征和沉积环境
2.
Sedimentary characteristics and environment of underwater delta in Minjiang Estuary Ⅰ. Modern sedimentary characteristics and environment;
闽江口水下三角洲沉积特征及沉积环境 Ⅰ.现代沉积特征及沉积环境
3.
Formation and evolution of underwater delta in Minjiang Estuary─I. Formative environment factors of underwater delta and its geomorphological development;
闽江口水下三角洲的形成与演变──Ⅰ.水下三角洲形成的环境因子与地貌发育
4) subaqueous Yellow River Delta
黄河水下三角洲
1.
The results show that a limit cyclic loading exists, which results in soil failure in the subaqueous Yellow River Delta.
利用室内周期循环加载试验 ,对黄河水下三角洲土体中孔隙水压力的变化加以测定 ,通过对波浪水槽试验和动三轴试验 2种方案所获数据分析认为黄河水下三角洲土体 (粉土、粘质粉土、粉质粘土 )存在一破坏的循环极限荷载。
5) Huanghe subaqueous delta
黄河水下三角洲
1.
Based on practical exploration and the laboratory test, the possibility of sandy soil liquefaction in the modern Huanghe subaqueous delta induced by earthquake and wave is analyzed by using the limit equilibrium and linear wave theory.
根据实际勘探资料及室内土工试验结果，按极限平衡理论和线性波动理论等，分析了现代黄河水下三角洲砂土在地震和波浪动力因素的作用下发生液化的可能性，并根据其液化过程实质是孔隙水压力产生、发展和消散的过程，总结出砂土液化模式应包括四个阶段；（１）压密阶段：孔隙水压力升高至砂土本身强度，使颗粒产生相对位移；（２）初始液化阶段：孔隙水压力升至土层所受侧向压力，产生较大应变；（３）完全液化阶段：孔隙水压力升至土层上覆有效应力，产生喷水冒沙现象；（４）塌陷形成阶段：孔隙水压力消散。
6) Underwater delta plain
水下三角洲平原
1.
Formation and evolution of underwater delta in Minjiang Estuary Ⅱ. Underwater delta plain;
闽江口水下三角洲的形成与演变 Ⅱ.水下三角洲平原
补充资料：“三角洲“反恐怖部队
该部队组建于20世纪70年代，其主要任务是对付全球范围内一切威胁美国利益的恐怖活动。该部队编有两个中队，中队下辖小队，每小队通常有16名特战队员。他们训练严格，组织严密，装备精良。
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