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散文英译汉佳作赏析:河之歌 The Song of the River_沪江英语学习网
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散文英译汉佳作赏析:河之歌 The Song of the River
The Song of the River河之歌
W.S Maugham毛姆
You hear it all along the river. You hear it, loud and strong, from the rowers as they urge the junk with its high stern, the mast lashed alongside, down the swift running stream. You hear it from the trackers, a more breathless , as they pull desperately against the current, half a dozen of them perhaps if they are taking up wupan, a couple of hundred if they are hauling a splendid junk, its square sail set, over a rapid.沿河上下都可以听见那歌声。它响亮而有力,那是船夫,他们划着木船顺流向下,船尾翘得很高,桅杆系在船边。它也可能是比较急促的号子,那是纤夫,他们拉纤逆流而上。如果拉的是小木船,也许就只五六个人;如果拉的是扬着横帆的大船过急滩,那就要200来人。
On the junk, a man stands amidships beating a drum incessantly to guide their efforts, and they pull with all their strength, like men possessed, and sometimes in the extremity of their travail they craw on the ground, on all fours, like the beasts of the field. They strain, strain fiercely, against the pitiless might of the stream.船中央站着一个汉子不停地击鼓助威,引导他们加劲。于是他们使出全部力量,像着了魔似的,腰弯成两折,有时力量用到极限就全身趴在地上匍匐前进,像田里的牲口。
The leader goes up and down the line and when he sees one who is not putting all his will into the task he brings down his split bamboo on the naked back. Each one must do his utmost or the labour of all is vain. And still they sing a , eager chant, the chant of the turbulent waters.领头的在纤绳前后跑来跑去,见到有人没有全力以赴,竹板就打在他光着的背上。每个人都必须竭尽全力,否则就要前功尽弃。就这样他们还是唱着激昂而热切的号子,那汹涌澎湃的河水号子。
I do not know words can describe what there is in it of effort. It serves to express the straining heart, the breaking muscles, and at the same time the
spirit of man which overcomes the pitiless force of nature. Though the rope may part and the great junk swing back, in the end the
and at the close of the weary day there is the hearty meal...我不知道词语怎样能描写出其中所包括的拼搏,它表现的是绷紧的心弦,几乎要断裂的筋肉,同时也表现了人类克服无情的自然力的顽强精神。他们使劲,拼命使劲,对抗着水流无情的威力。虽然绳子可能扯断,大船可能倒退,但最终险滩必将通过,在筋疲力尽的一天结束时可以痛快地吃上一顿饱饭&..
But the most agonizing song is the song of the coolies who bring the great bales from the junk up the steep steps to the town wall. Up and down they go, endlessly, and endless as their toil rises their rhythmic cry. He, aw --ah, oh. They are barefoot and naked to the waist. The sweat pours down their faces and their song is a groan of pain.然而最令人难受的却是苦力的歌,他们背负着船上卸下的大包,沿着陡坡爬上城墙。他们不停地上上下下,随着无尽的劳动响起有节奏的喊声:嗨,呦&&嗬,嗨。他们赤着脚,光着背,汗水不断地从脸上流下。
It is a sigh of despair. It is heart-rending. It is hardly human. It is the cry of souls in infinite distress, only just musical, and that last note is the ultimate sob of humanity. Life is too hard, too cruel, and this is the final despairing protest. That is the song of the river.他们的歌是痛苦的呻吟,失望的叹息,听来令人心碎,简直不像是人的声音。它是灵魂在无尽悲戚中的呼喊,只不过有着音乐的节奏而已。那终了的一声简直就是人性泯灭的低泣。生活太艰难、太残酷,这喊声正是最后绝望的抗议。这就是河之歌。
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研究揭示了河流为什么会蜿蜒流动 Dynamic Reorganization of River Basins
By Science
23 Sep 2016
论文摘要&研究人员设计了一个可预测河流网络如何演变的模型;他们说,该模型可对过去、现在及未来地形的动态物理特征做出某些阐释。Sean Willett及其同事对江河流域及排水系统划分或分水线随着时间的推移因应侵蚀及地壳构造隆升而致的改变方式进行了研究。他们用其得出的公式来测量目前世界上3个河流体系的状态;他们提出,渠道、流域及分水线常常会迁移以达到一种平衡的状态,在平衡状态时,地形会停止变迁。他们说,例如,汇入黄河的支流现在似乎已经变得相对稳定。但是据研究人员披露,在台湾中部的年轻的地貌以及美国东南部古老的河流网络仍然处在不断的变化之中。这一新的观察过去、现在及未来河流体系的方式或能给来自不同背景的科学家探索由河流系统连接的地质学、化学及生物学系统提供方法。对许多生物来说,河流网络所起的或是实体的通道或是屏障的作用,因此更好地了解它们相对的稳定性和长期性可能会产生某些有关演化的生物物理驱动因素的有价值的并具有对未来的生态学及环境保护有意义的见解。Abstract&River networks evolve as migrating drainage divides reshape river basins and change network topology by capture of river channels. We demonstrate that a characteristic metric of river network geometry gauges the horizontal motion of drainage divides. Assessing this metric throughout a landscape maps the dynamic states of entire river networks, revealing diverse conditions: Drainage divides in the Loess Plateau of Chi the young topography of Taiwan has migrating divides driving adjust and rivers draining the ancient landscape of the southeastern United States are reorganizing in response to escarpment retreat and coastal advance. The ability to measure the dynamic reorganization of river basins presents opportunities to examine landscape-scale interactions among tectonics, erosion, and ecology.Structured AbstractIntroductionRiver networks, the backbone of most landscapes on Earth, collect and transport water, sediment, organic matter, and nutrients from upland mountain regions to the oceans. Dynamic aspects of these networks include channels that shift laterally or expand upstream, ridges that migrate across Earth’s surface, and river capture events whereby flow from one branch of the network is rerouted in a new direction. These processes result in a constantly changing map of the network with implications for mass transport and the geographic connectivity between species or ecosystems. Ultimately, this dynamic system strives to establish equilibrium between tectonic uplift and river erosion. Determining whether or not a river network is in equilibrium, and, if not, what changes are required to bring it to equilibrium, will help us understand the processes underlying landscape evolution and the implications for river ecosystems.MethodsWe developed the use of a proxy, referred to as χ, for steady-state river channel elevation. This proxy is based on the current geometry of the river network and provides a snapshot of the dynamic state of river basins. Geometric equilibrium in planform requires that a network map of χ exhibit equal values across all water divides (the ridges separating river basins). Disequilibrium river networks adjust their drainage area through divide migration (geometric change) or river capture (topologic change) until this condition is met. We constructed a numerical model to demonstrate that this is a fundamental characteristic of a stable river network. We applied this principle to natural landscapes using digital elevation models to calculate χ for three, very different, systems: the Loess Plateau in China, the eastern Central Range of Taiwan, and the southeastern United States.ResultsThe Loess Plateau is close to geometric equilibrium, with χ exhibiting nearly equal values across water divides. By contrast, the young and tectonically active Taiwan mountain belt is not in equilibrium, with numerous examples of actively migrating water divides and river network reorganization. The southeastern United States also appears to be far from equilibrium, with the Blue Ridge escarpment migrating to the northwest and the coastal plain rivers reorganizing in response to this change in boundary geometry. Major reorganization events, such as the capture of the headwaters of the Apalachicola River by the Savannah River, are readily identifiable in our maps.DiscussionDisequilibrium conditions in a river network imply greater variation of weathering, soil production, and erosion rates. Disequilibrium also implies more frequent river capture with implications for exchange of aquatic species and genetic diversification. Transient conditions in river basins are often interpreted in terms of tectonic perturbation, but our results show that river basin reorganization can occur even in tectonically quiescent regions such as the southeastern United States.
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