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lake bottom相关的网络例句

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Time series simulations are consistent with sediment records from lake bottom cores back to 100 years ago, and spatial distribution modeling of nutrient resources are agreement with changes in the geographical features. The work suggests that the simulations can catch basic characters of the basin nutrient changes, and provides a powerful tool to evaluate nutrient resources, sedimentations and distributions responding to historical changes in catchment environments.

模拟总氮和总磷浓度与太湖沉积钻孔沉积样推算的水体含量的数量级和变化范围相当,太湖流域的营养盐空间来源模拟也能够与流域自然地理变化吻合,表明模拟能够捕捉到流域营养盐历史变化特征,对湖泊营养物质来源、沉积和空间分布的流域环境历史变化响应具有良好模拟能力。

After past short while, there appear two giant monsters above the lake bottom, with two black and yellow groups light shading and fluctuating unceasingly in the water.

过不了多时,湖底上方出现了两只庞然大物,一黑一黄的两团光影不断在水中变幻。

Cooking casserole Tianmuhu head, use the natural water Tianmuhu head for raising a large bighead raw, pure natural water Tianmuhu soup base, coupled with unique cooking processing by the picturesque scenery of the day as head Green Lake is not only the surrounding mountain vegetation filters the water, and lake bottom is sandy rather than silt, this unique natural environment created Tianmuhu water clear and sweet, Qian Chen did not dye, so the growth of fish which have absolutely no off-flavor.

烹制天目湖砂锅鱼头,选用天目湖水体中天然生养的大花鲢鱼头作原料,纯天然天目湖水为汤基,加上特有的烹调工艺加工而成,由于山青水秀的天目湖不仅周围山体绿色植被过滤了湖水,而且湖底为沙质而非淤泥,这一独特的自然环境造就了天目湖水清澈甘甜,纤尘不染,故其中生长的鱼类也绝没有土腥味。

Some innovative results are listed below:1、According to the lithologic characters,lithofacies,genetic classification and the geomorphy,the Quaternary system is divided into piedmont-gully\'s and plain\'s. The piedmont-gully\'s Quaternary sediment,which is about 3~20 meters in thick,is in the western hills of the study area.The plain\'s Quaternary sediment is widely distributed in the study area,which is about 30~60meters thick and become thicker from southwest to northeast.2、The Quaternary sediments of plain can be divided into five sedimentary cycles.The Late Pleistocene series Quantan group,at the bottom of the Quaternary System,is constituted by a fluvial facies-river and lake facies sedimentary cycle. The Late Pleistocene series Jiashan group,at the middle of the Quaternary sediment, is constituted by two fluvial facies-neritic facies-river and lake facies sedimentary cycles.The Holocene series Binhai group,at the upper of the Quaternary sediment, is divided into three parts,the under layer and middle layer are constituted by two littoral facies-river and lake facies sedimentary cycles,the upper layer is constituted by paludal facies,which was deposited at the lower-lying land like West Lake, Jiangcun-Gu dang,Xianghu lake,and coastal-estuary facies in other area.3、Folding and fault activities were weak in Quaternary and the tectonic activity had little influence on the Quaternary sedimentation.The ancient landforms,the evolvement of the river system and transgression were the main elements which controlled the Quaternary sedimentation in Hangzhou.The ancient landforms formed the basis of the Quaternary sedimentation.The evolvement of the river system and transgression individually or jointly controlled the Quaternary sedimentation of this area.4、The alternation of the climate was the main reason for the evolvement of the river systems and transgression,and it\'s also the reason why the Quaternary system of Hangzhou has the special sedimentary structure which is called soft interbed with hard layers.

通过研究取得了以下成果:1、根据岩性、岩相、成因类型和地貌特点,将本区第四系划分为山麓沟谷区沉积和平原区沉积:山麓沟谷区第四系主要分布于西部丘陵地区,厚度较薄且变幅大,一般厚3~20m;平原区第四系广布分区,由南西向北东逐渐增厚,一般厚30~60m.2、平原区第四系自下而上大体由五个完整或不完整的沉积旋回构成:底部上更新统全塘组,由河流相—河湖相的沉积旋回构成;中部上更新统嘉善组,由河流相—浅海相—河湖相两个沉积旋回构成;上部全新统滨海组,其下中两段由滨海海湾相—河湖相的两个沉积旋回构成,上段由西湖、蒋村—古荡、湘湖等低洼处沉积的湖沼相和其他地区沉积的滨海河口相构成。3、第四纪以来,研究区内褶皱、断裂活动微弱,构造运动对第四系沉积的影响不大,古地形、古水系的发育、变迁和海侵是杭州市第四系沉积的主要控制因素:古地形构成了第四系沉积的基底,水系与海侵在其后的不同阶段或分别或联合的主导了区内的第四系沉积。4、水系的发育、变迁和海侵的共同原因是天气变化,正是由于第四纪以来"冷热交替"的天气特点形成了杭州市第四系"软硬互层"的特殊沉积结构。

The underwater enclosure was built along the boundary of target water body and the lake bottom sludge was filled into the enclosure by twisting-suction dredging ship according to designing elevation for the purpose of formation of slope riffle, which will improve natural condition of littoral zone of lake, and create favorable habitation condition for ecological restoration in littoral zone of lake.

文章介绍最新开发的湖滨陡坎沿岸水域基底修复技术,主要采用人工方法在需要进行大型水生植物群落恢复的湖滨陡坎沿岸的水域实施基底修复工程措施,在目标水域边界构筑水下围埝,采用绞吸式挖泥船将疏浚的湖泥按设计高程要求吹填至基底修复工程区内,形成缓坡浅滩,改善湖泊沿岸带自然条件,为湖泊沿岸带生态修复创造良好的生境条件。

He says that he would not expect to find much evidence in lake sites because magnetic material would rust away, while the tiny spheres float and would not collect on the lake bottom.

他表示,自己并不期望能够在湖中找到大量证据,因为磁矿物都会被锈蚀,悬浮在水中,不会集中在湖底。

Huangqihai Lake for the inland alkaline lake, Lake basin closed, evaporation, pH, 8-86, bottom of the lake is black-brown ooze.

黄旗海为内陆碱性湖,湖盆封闭,蒸发量大,pH值8—86,湖底为黑褐色软泥。

Refer to the research findings of CHengDu Research Institute of Geosciences and Minerals(1990) and Nanjing Research Institute of Geography and Lake of Chinese Academy of Sciences(1989), according to the Guidebook of China Stratum(2000), the chronostratigraphy of Kunming Basin is divided into 4 age: the bottom of the Quaternary corresponding to M/G Boundary, age is 2.6Ma;the Bottom of the Mid-Pleistocene corresponding to B/M Boundary, age is 0.78Ma;the Bottom of the Upper-Pleistocene corresponding to the Blake event, age is 0.128Ma;the Bottom of the Holocene corresponding to the Gothenburg event,age is 0.012Ma.

本次研究获得了大量的测年数据,参考成都地质矿产研究所(1990)及中科院南京地理与湖泊研究所(1989)等的研究成果,按照中国地层指南(2000)的方案,厘定了昆明盆地第四纪年代地层划分:第四系底界对应古地磁松山反向期与高斯正向期界线处,年龄为2.6Ma;更新统中部底界对应古地磁布容正向期与松山反向期界线,年龄为0.78Ma;更新统上部底界对应古地磁布莱克事件附近,年龄约0.128Ma:全新统底界对应古地磁哥德堡事件附近,年龄约0.012ma。

Into the lake by the fire surrounded conglomerate, oval-shaped like the bottom of the pan-shaped lake no significant intake, but Lake Circuit, outside the mountain, from the east, north, south are the three potential spring water spilled out, respectively, the flow of Linxia, Xunhua, water areas, waterhua hua sound could be heard far away, the lake to the high, dark, dangerous, known by God, inaccessible.

湖面由火成砾岩围成,呈椭圆形,似锅底状,湖无明显进水口,但湖围山体外侧,从东、北、南三个方向有三股泉水潜泻而出,分别流向临夏、循化、清水地区,哗哗水声,远处可闻,此湖以高、深、险、神所著称,人迹罕至。

In the National Natural Science Fund Project, supported by the Institute through 10 years in a row on the lake dried up Ebinur region of proliferation and the accumulation of observations and sampling analysis found that,Lop Nur, the Ebinur Lake, Xinjiang艾丁湖region is the main source of salt dust, from the bottom of the lake dried up Ebinur region of dust is an important source of salt dust material, Salt in the region of the frequency of dust storms has created extremely favorable conditions.

据中科院新疆生态与地理研究所吉力力阿不都外力研究员介绍,在国家自然科学基金项目支持下,该所通过连续10年对艾比湖地区干涸湖底的扩散和堆积进行观测和取样分析发现,罗布泊、艾比湖、艾丁湖地区是新疆盐尘暴的主要策源地,源自艾比湖地区干涸湖底的粉尘是重要的盐尘暴物质来源,为该地区盐尘暴的频发创造了极为有利的条件。

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