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Since then, I often went to Yangcheng Lake, and visited my godfather godmother and grandparents At there I'M a small Prince Edward, and with Yang Cheng lake 's little partners were playing crazy everywhere, In Spring shores of grasping the frog in the fields and dug tree holes,and climbed the trees and caught the little birds. In winter of Yangcheng Lake ,We went to pick the frozen village chicken and ducks.

此后,我常常要到阳澄湖去看干爹干妈和爷爷奶奶又做起了小太子、小大王,和阳澄的小伙伴们到处疯狂的玩耍,春天在田岸边抓青蛙,爬树掏鸟窝;冬天到阳澄湖边去拾被湖水冰冻的庄鸡和野鸭。

Data collected by a satellite launched in 2003 - the Ice, Cloud and Land Elevation Satellite, or ICESat - revealed a complex network of subglacial plumbing in which water periodically cascades from one hidden reservoir to another.

美国宇航局2003年发射的"冰云和地面高度卫星"收集的数据显示,南极冰层下有一个复杂的湖泊排水网络,湖水会周期性地从一个隐秘的湖泊流向另一个湖泊。

Data collected by a satellite launched in 2003 - the Ice, Cloud Land Elevation Satellite, or ICESat - revealed a complex network of subglacial plumbing in which water periodically cascades from one hidden reservoir to another.

美国宇航局2003年发射的"冰云和地面高度卫星"收集的数据显示,南极冰层下有一个复杂 www.dDdtt.com 的湖泊排水网络,湖水会周期性地从一个隐秘的湖泊流向另一个湖泊。

Influenced by the exterior source input of the detrital matters, U-series dating using aragonite is not suitable to the study of Lake Sugan sediment and a further study is required.2. The isotopes study of precipitation-groundwater-lake water system in Lake Sugan drainage area indicates that in modern climate system, the precipitation in Lake Sugan drainage area is mainly supplied by the water vapor carried by Westerly.

沉积物文石的铀系测年受到外源碎屑输入的影响,在苏干湖并不适用,需做进一步的研究。2、苏干湖流域降水-地下水-地表径流-湖水同位素系统研究表明,现代气候条件下苏干湖流域大气降水主要来源于西风环流携带的水汽输入。

Summertime, oh summertime, pattern of life indelible, the fade proof lake, the woods unshatterable, the pasture with the sweet fern and the juniper forever and ever, summer without end; this was the background, and the life along the shore was the design, the cottages with their innocent and tranquil design, their tiny docks with the flagpole and the American flag floating against the white clouds in the blue sky, the little paths over the roots of the trees leading from camp to camp and the paths leading back to the outhouses and the can of lime for sprinkling, and at the souvenir counters at the store the miniature birch-bark canoes and the post cards that showed things looking a little better than they looked.

我一个劲儿地回忆着这往昔的一切。那些岁月,那些夏日,对于我是无限的珍贵,值得永远珍藏心底。那是充满欢乐、宁静和美好的时光。八月初的到达本身就是桩了不得的事儿。农场的马车在火车站刚停下,你就闻到了空气中厚重的松树味儿;你第一次瞥见了笑容满面的庄稼人。车上的行李箱是那么重要,是少不得的。父亲在所有这些事儿上有着绝对的权威。马车在你身底下颠颠晃晃十几英里的感受,是多么令人激动!在最后一座长长的山脊上,你一眼望见了离别十一个月的湖,望见了你梦牵魂绕的那泓湖水

The water at that depth is a constant 4°C, its temperature protected by a layer of water above it called a thermocline.

在这个深度上的湖水一直恒定在摄氏4摄氏度,在其之上的一层水被称为温跃层(较热的水面区与冷的深冷水区之间的水层),可以保持其的温度。

The analysis of TOC andδ13Corg benefits from Well Chao-73, indicating that they response well enough to the Cretaceous paleoenvironment and paleoclimate. During the sedimentary period of Quantou formation to Qingshankou formation in Songliao basin, the water tends to rise and becomes anoxic, and the deoxidized water leads to the organic matter massively preserved. The paleoclimate changes from torridity and aridity to warmth and humidity, with the temperature evidently descengded, then ascended in a litter range. The result is basically consistent with paleoclimate by the palynological analysis.

朝73井TOC、δ13Corg有机地球化学指标的分析结果表明,TOC、δ13Corg的变化对该沉积时期的古环境、古气候也有很好的响应,该沉积期湖水位不断上升,湖生生物逐渐发展并繁盛起来,水体含氧量减少,湖底有机质的保存环境逐渐变为强还原环境,大量有机质被埋藏并保存,而古气候在泉头组/青山口组界线上下由炎热干旱变得温暖湿润,气温有明显下降,但随后又有小幅的上升,与孢粉分析的古气候变化特征基本一致。

If I had time, I would choose the place away from the city and the crowd, climbing in high mountain, canoe on the lake, wander in flowers and trees, till sunset at dusk, the darkness, the beautiful sunset view towards the moon, enjoy cool colour elegant lasting appeal.

假如我有时间的话,我会选择远离城市和人群的地方,攀缘于高山之上,荡舟于湖水之中,信步于花木之间,直到日落黄昏,夜幕降临,观赏西天晚霞的绚丽色彩,领略清风明月的高雅韵味。

Tufa form when underwater springs rich in calcium meet lake water rich in carbonates, forming calcium carbonate, or limestone.

当富含钙质的地下水接触到富含碳酸盐的湖水时,就形成了碳酸钙或者花岗岩,进而形成石笋。

The lake water is now undrinkable despite several billion dollars having been spent trying to clean it up.

尽管当地政府已经投入了数十亿美元试图进行清理,但是现在湖水已经无法饮用了。

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