河冰的

The Yuquanyuan is about 27,000 square meters, limpid Piaobai River goes through the whole garden, and you can see campfire party free of charge and actions of Gaoligong people every evening. During summer days, put fresh fruits in the clear river, then enjoy yourself freely. There are many bars around our hostel, which serve wine, coffee, tea, syrup, and so on. You can also stay in the hostel, to surf on the internet, to see a movie, to have a drink, or to read some books, you will feel at home. The time in Tengchong is very easygoing; you can even feel the flow of time. Life here is simple, easy, and degage, you can look for old stories of the southern Silk Road. With the comfortable feeling, you can also search for the mystery view beyond Gaoligong mountain. We are looking forward to welcoming your arrival.

园面积四十余亩，清澈的漂白河穿园而过，每晚都有热闹的高黎贡山民族表演和免费的篝火晚会，出了旅舍门就可以买个西瓜放在清冽的河水里冰一冰，然后坐在大青树下水车旁，看着水中游鱼水草，尽情地发呆……晚上无聊了就到泳池旁边的酒吧街随便进一家，喝醉了也不用担心，我们会把你捡回来……实在不想出门，就待家里吧，上网、喝瓶腾越老烧，看部电影；在书吧安静的一角细细研读中国远征军英勇的抗日史，或者猜测下家里随处可见的明清古董家具背后的故事，那一幅幅精妙的腾越民间刺绣又如何沉淀了古腾越曾经的商贾云集；和朋友聊下是不是找个火山一样的傈僳族男朋友，或者泡个温泉一样的……在腾冲待着的日子，时间是停滞的，但总不会感觉无事可做……岁月，人，心情和故事都很从容，仿佛连光阴也早被茶马古道伸长了……休息够了就背上包，顺着马帮留在青石板上深深的蹄印，寻找高黎贡山深处的参天古树、大树杜鹃……不管多晚我们会为你亮一盏灯，等你回来把旅途的见闻与我们一一分享

The Yuquanyuan is about 27,000 square meters, limpid Piaobai River goes through the whole garden, and you can see needfire party free of charge and actions of Gaoligong people every evening. During summer days, put fresh fruits in the clear river, then enjoy yourself freely. There are many bars around our hostel, which serve wine, coffee, tea, syrup, and so on. You can also stay in the hostel, to surf on the internet, to see a movie, to have a drink, or to read some books, you will feel at home. The time in Tengchong is very easygoing; you can even feel the flow of time. Life here is simple, easy, and degage, you can look for old stories of the southern Silk Road. With the comfortable feeling, you can also search for the mystery view beyond Gaoligong mountain. We are looking forward to welcoming your arrival.

园面积四十余亩，清澈的漂白河穿园而过，每晚都有热闹的高黎贡山民族表演和免费的篝火晚会，出了旅舍门就可以买个西瓜放在清冽的河水里冰一冰，然后坐在大青树下水车旁，看着水中游鱼水草，尽情地发呆……晚上无聊了就到泳池旁边的酒吧街随便进一家，喝醉了也不用担心，我们会把你捡回来……实在不想出门，就待家里吧，上网、喝瓶腾越老烧，看部电影；在书吧安静的一角细细研读中国远征军英勇的抗日史，或者猜测下家里随处可见的明清古董家具背后的故事，那一幅幅精妙的腾越民间刺绣又如何沉淀了古腾越曾经的商贾云集；和朋友聊下是不是找个火山一样的傈僳族男朋友，或者泡个温泉一样的……在腾冲待着的日子，时间是停滞的，但总不会感觉无事可做……岁月，人，心情和故事都很从容，仿佛连光阴也早被茶马古道伸长了……休息够了就背上包，顺着马帮留在青石板上深深的蹄印，寻找高黎贡山深处的参天古树、大树杜鹃……不管多晚我们会为你亮一盏灯，等你回来把旅途的见闻与我们一一分享

A important conclusion is that fluvial-lacustrine, karst, diluvial, colluvial, glacial and outwash deposits, which formed between early Pleistocene and early middle-Pleistocene, have high cement degree, low permeability, high intensity, low deformation, and good engineering properties, but modern riverbed phase deposits, which formed in between late middle-Pleistocene and Holocene, are loose, highly permeable, weak, highly deformable and have bad engineer characteristics, so they are susceptive to differential settlement, piping, drafting, liquefaction problems.

得出早更新世—中更新世早期河湖相沉积、岩溶沉积、洪积、崩坡积、冰碛和冰水沉积密实度高，胶结较好，透水性差，强度高，变形小，工程性质较好，而中更新世晚期—全新世现代河床沉积较松散，渗透性高，强度较低，变形较大，易发生差异沉降、管涌、流土、地震液化等工程地质问题的重要结论。

So, it is very necessary to study the river ice evolution. Based on ice jam mechanism, hydraulics model and energetics model are introduced into this research and well simulate water level, freeze-up and break-up date of each spring in Wudinghe River.

根据冰塞形成发展的机理，利用水力学模型和热力学模型模拟研究了无定河流域下游段丁家沟至白家川的每年春季河流水位、封河日期和开河日期。

The Menyuan Basin is an intermontane basin in the central segment of the Qilian Mountains,bounded by boundary faults on the north and south.

门源盆地是祁连山中段的山间盆地，南北边缘均为断裂控制，发育古近系白杨河组、第四纪冰碛物和冰水堆积物。

The field geological research indicates that the permafrost type is mainly of much ice- more ice - most ice, and there are ice layers containing soil distributing in the swampland area.

野外地质调查表明，中俄原油管道工程沿线途经的河漫滩、阶地附近，多年冻土类型以多冰—富冰—饱冰冻土为主，在沼泽地段分布有含土冰层。

It seems likely that changes in snowfall amounts, with season or in storm intensities, will alter the timing, temperature relations, and extent of avalanching.

小胡姆丹冰川在19世纪也形成过大型冰坝，其边缘已经进入河流并且从河上横跨过去，现在河水是从冰下流过的。

Their blood is in me, their lusts my waves.

在冰封的利菲河上，我在他们当中活动[147]。

The mechanical breakup of ice covers during spring often lead to the serious ice-dam formation.

春季河道武开河可能导致冰坝形成，至今仍缺乏以力学机制为基础的开河预测方法。

The paleochannel-Ⅱ might form during the Holocene Optimal period.

古河道-Ⅴ形成于风沙-Ⅱ和Ⅲ期形成之前，可能是末次冰期之前，即中更新世或更早，这时河流能够进入古松辽大湖；古河道-Ⅳ形成于风沙-Ⅱ和Ⅲ期形成之时，可能是末次冰期时期，这时河流与松辽大湖萎缩，规模减小，河流已不能进入松辽大湖，而是消失在沙地之中；古河道-Ⅲ形成于风沙-Ⅱ和Ⅲ期形成之后，可能是末次冰期末期的冰消期，这时气温升高，大量的冰雪融水进入河流，促使河水漫流，流入沙垅垅间洼地，开始造成古西拉木伦河、古老哈河与教来河水文网之间的相互联系；古河道-Ⅱ形成于全新世适宜期时期，统一的西辽河形成，伴随气候变化，出现多次风沙进退，对应于风沙-Ⅰ期；河道-Ⅰ是现在，同属于风沙-Ⅰ期，活动沙地集中在翁牛特等地。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。