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I want to make a detour of those lofty arid mountain ranges where one dies of thirst and cold, that "extratemporal" history, that absolute of time and space where there exists neither man, beast, nor vegetation, where one goes crazy with loneliness, with language that is mere words, where everything is unhooked, ungeared, out of joint with the times.

我想要一个河流能把人载到各地去的世界,不是成为古老传说的河流,而是能叫人同别的男女,同建筑、宗教、植物、动物接触的河流。

Jin Shajiang trunk stream can develop the fluvial drop that use to be rice of 2 1 80, trunk stream of river of elegant rice huller can develop drifting fluvial drop to be rice of 2 82 7, the big trunk stream that cross a river can develop the fluvial drop that use to be 2 636 rice.

金沙江干流可开发利用的河流落差为 2 1 80米,雅砻江干流可开发利用的河流落差为 2 82 7米,大渡河干流可开发利用的河流落差为 2 636米。

Fully utilizing river' s own energy to reaerate for river, increase the DO concentration of city river polluted water and improve the water quality by the riverway artificial structures, such as dams and weirs, this is a effective method which is of tremendous social and economic benefit.

通过河道人工建筑物,如坝、堰等,充分利用河流本身所蕴藏的能量为河流复氧、提高城市河流污染水体的DO含量、改善水质状况,是一条可以带来巨大社会效益和经济效益的有效途径。

In this paper organoleptic index, physico-chemical index for water body and sediment,composition of river ecological system, function of river ecological system to assess river pollution condition were introduced

论文全面介绍了感观指标、水质和底泥的理化指标、河流生态系统的结构和河流生态系统的功能等评价河流污染状况及治理效果的指标体系。

Results The damp fans, rivers and lakes are main sedimentary systems in Yanqi Basin. They are funned from T(subscript 2-3) to J2, including Xiaoquangou, Badaowan, Sangonghe, Xishanyao and Toutunhe age. The rivers and lakes sedimentary systems are good development. The rivers sedimentary systems are divided into braided stream and meandering stream.

结果 潮湿扇、河流和湖泊沉积体系是焉耆盆地的主要沉积体系类型,它们形成于中晚三叠世至中侏罗世的小泉沟、八道湾、三工河、西山窑和头屯河期;其中的河流沉积体系和湖泊沉积体系较为发育,河流沉积体系分为辫状河和曲流河两种类型。

Secondly, based on the abstract and assignment decomposition of the entities included in the URWE, the Agent model of the URWE entities such as pollutionenterprise、 governor and water body was built, and combined with the theory of drainage basin water pollution control and decision-making, the assignment allotment and frame design of the Agent included in the URWE was made in detail, the theory foundation was established to achieve the URWEIDSS based on Agent.

再次,分析了现有城市河流水质数值仿真所存在的不足,提出了基于Agent的城市河流水质数值仿真模型,并基于这种城市河流水质数值仿真模型,提出了采用模块化、拖拉式的方式进行城市河流水质仿真的方法。

Lithological characterized by pyroclastic rocks interbedded with sedimentary rocks, with a few volcanic rocks.(2) The sedimentary facies: include normal fluvial, swamp, littoral and shallow lakes, as well as fallout facies of pyroclastic sediments, volcanic lahar facies, pyroclastic alluvial facies and pyroclastic fluvial facies (different from normal alluvial and fluvial facies).

1岩性——以火山碎屑岩、火山碎屑沉积岩和陆源碎屑沉积岩互层为特征,亦夹有少量火山岩;(2)沉积相类型——包括陆源碎屑沉积的河流相、沼泽相、滨浅湖相和火山碎屑沉积的空落相、火山泥石流相、火山碎屑冲积扇相和火山碎屑河流相(与陆源碎屑的冲积扇相和河流相不同)。

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 change extent of the water level and the falling extent the imbedded water level is the biggest in Phragmites sustralis-Carex schmidtii community, The reason is likely to be it's near to the river, and have gutters in the peatland which is near the river, which makes the water enter the river easily, and so make the change extent bigger.

水位变化幅度在芦苇-苔草群落中最大,这可能是由于该区距离河流较近,而且人为的在泥炭地与河流相接处挖排水沟渠,使泥炭地中的水更容易的进入河流,使之变化速率较快,变化幅度较大。

Major peninsular rivers whose steeper gradients prevent their waters from flooding include the Godavari , the Mahanadi , the Kaveri , and the Krishna , which also drain into the Bay of Bengal;[76] and the Narmada and the Tapti , which drain into the Arabian Sea .

但印度境内的河流包括戈达瓦里河, Mahanadi 河, Kaveri 河和克利须那河,虽然也都同样经孟加拉湾流入大海,由于河流坡度较陡,所有不大容易形成洪水。纳尔默达河和 Tapti 河的河流坡度也较陡,但最后流入阿拉伯海。

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