湖泥 的英文怎麼說

It can also restrain the decomposition of organic substances in the soil and the bind of nitrogen, and wash away the nutritious elements, such as magnesium, calcium, and potassium. the acid rain deprives the soil. it acidifies the rivers and lakes, and dissolves the heavy metal in the soil into water, therefore poisons the fish

它可以直接使大片森林死亡，農作物枯萎；也會抑制土壤中有機物的分解和氮的固定，淋洗與土壤粒子結合的鈣、鎂、鉀等營養元素，使土壤貧瘠化；還可使湖泊、河流酸化，並溶解土壤和水體底泥中的重金屬進入水中，毒害魚類；加速建築物和文物古跡的腐蝕和風化過程；可能危及人體健康。

The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems

五道梁群湖相碳酸鹽巖分為生物粘結灰巖（疊層石） 、泥晶灰巖、顆粒灰巖與泥晶白雲巖四大類，反映出沉積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。

Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock

摘要以現有資料為基礎，通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究，認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化，沉積了巨厚的新生代地層，自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。

( 2 ) based on indoor test, two typical soft rock of brecciated mudstone and siltstone in luohu jiancheng district is carried systemically though interior rheological testing ; moreover combining with preceding studying results of rock rheological constitutive model, rheological numerical constitutive model suited to rock mass mechanics characteristics and stratum structure of luohu fracture zone, and numerical parameters of the model are processed with studying of curve fitting

（ 2 ）立足於室內試驗，對羅湖建成區兩種典型的軟弱巖石?含角礫泥巖和粉砂巖進行系統的室內流變試驗研究，又結合前人對巖石流變本構模型的研究成果，分析並確定了適合羅湖破碎帶巖體力學特性及地層構造特徵的流變計算本構模型，並對該模型的計算參數進行了曲線擬合研究。

Can we control lake eutrophication by dredging

底泥疏浚能控制湖泊富營養化嗎

3. wetland preserve : mainly are fish ponds and swamps. sihcao lake is around 60 hectares and tourist can take raft to enjoy the estuary and the natural ecology to get a further knowledge of mongrove, waterbrids, fishes, fiddler crabs and plants

周邊有面積約60公頃四草湖自然景觀設施，旅客可搭乘管筏欣賞河口水域及自然生態進一步認識四草湖紅樹林、泥灘地等河口濕地之生態，包括水鳥、魚類、招潮蟹、紅樹林植物等，還有湖中湖與鷺鷥林景觀，體驗一場寓教於樂的生態之旅。

The paper is based on the construction of the express - highway between yiyang and changde in hunan province, aiming at enhancing the serviceability of cement concrete pavement, probing into the structural assemblage of the cement concrete pavement, the roadway drainage system, contraction joint with the dowel bar and precaution of bumping at the end of the abutment. it presents some achievements of the research, including more reasonable structural assemblage and roadway drainage system, the method of setting dowelled bar in contraction joint, putting forward the concept of stage - transition from rigid to flexile behind abutment

本文以湖南省益陽至常德高速公路項目為依託，以提高水泥混凝土路面使用性能為目標，就水泥混凝土路面結構組合、路面排水系統、縮縫設置傳力桿、橋頭跳車問題的防治等方面開展研究和工程實踐，取得了豐富的研究成果，如研究採用了更合理的路面結構組合，設置了較完善的路面排水系統，在國內高速公路上率先全面採用縮縫加傳力桿技術，對所有橋涵構造物臺背全部採用剛柔過渡技術處理橋頭跳車問題等。

Wetland habitats : intertidal mudflats, lagoons, mangrove, seashore rivers and canals

濕地生境：潮間帶泥灘鹹水湖紅樹林沿海河流與水道

Especially in shuanghu area and amdo 114 station, the sedimentary rocks is organic - rich, mostly consist of black shales, marls and mudstones

尤其是雙湖地區和安多114道班巖性特殊，為一套富含有機碳沉積，主要為黑色頁巖、泥灰巖和泥巖。

The microfacies characteristic of carbonate rock of suonahu formation in cuoqinin basin constitutes with the marl lithofacies, the intraclast ash lithofacies, biological detritus ash lithofacies

措勤盆地嗩吶湖組碳酸鹽巖微相由內碎屑灰巖相、生物碎屑灰巖相和泥灰巖相組成。

The northern qiangtang basin suonahu formation microfacies of carbonate rock is divided for the intraclast ash lithofacies, biological detritus ash lithofacies, oncolite limestone lithofacies, contain the calcium and alga ash lithofacies, marl lithofacies and pure microlite limestone lithofacies

羌北盆地嗩吶湖組碳酸鹽巖微相為內碎屑灰巖相、生物碎屑灰巖相、核形石灰巖相、含膏藻灰巖相、泥灰巖相和純微晶灰巖相等6種微相。

These geomorphic units of paleogeography constitute the basic model of paleocontinent, littoral - neritic sea and carbonate plateform at that stage, and this depositional model is similar to the pattern of the east china continent and ocean, which is the result of evolution during the past long geologic age

這些古地理地貌單元構成了湖北省泥盆紀時期古陸濱淺海和碳酸鹽巖臺地的基本沉積模式，這種沉積模式與現今中國東海大陸、海洋格局基本一致，亦是經過了漫長地質歷史時期演化，而形成現今這種格局的。

This is also borne out by the fact that the river and lake deposits contain peat.

這一點也被河湖沉積物中包含著泥炭這樣的事實所證明。

Cancelled nr808 manlai court - central nr809 pristine villa - tai wai kcr station nr810 parc royale - kowloon tong mtr station circular nr811 kwong yuen estate - causeway bay sai wan ho nr812 pictorial garden phase 3 - lucky plaza nr813 pictorial garden phase 3 - kowloon tong mtr station circular nr814 chevalier garden - university kcr station nr815 royal ascot - new town plaza circular nr816 kwong yuen estate - mei lam estate nr817 lakeview garden - tai wai kcr station nr818 golden time villas - tai wai kcr station nr819 granville garden - tai wai kcr station nr820 shatin heights - tai wai kcr station nr821 kwong yuen estate - ma on shan nr822 villa paradiso - university kcr station nr823 villa paradiso - diamond hill mtr station nr824 vista paradiso - bayshore towers nr825 lee on - tuen mun ho tin street nr826 villa athena - pai tau street nr827 kam ying court - cheung sha wan nr828 chung on - fo tan refer to gmb 801 nr829 castello - new town plaza phase 1 nr830 jubilee garden - wong tai sin cancelled nr831 monte vista - university kcr station nr832 baycrest - university kcr station nr833 julimount garden - tai wai kcr station nr91 fairview park - wan chai nr92 fairview park - tsuen wan nr93 fairview park - yuen long nr94 fairview park - sheung shui kcr station nr95 long ping estate - sheung shui kcr station nr96 long ping estate - hung hom kcr station nr97 long ping estate - wan chai nr98 long ping estate - hung hom kcr station nr99 long ping estate - kwun tong hung to road nr901 locwood court, kingswood villas - tsuen wan mtr station nr902 locwood court, kingswood villas - sheung shui kcr station nr903 kingswood villas - wan chai nr904 kingswood villas - china hong kong city nr905 maywood court, kingswood villas - tsuen wan mtr station nr906 maywood court, kingswood villas - tsui ping road kwun tong nr907 maywood court, kingswood villas - sheung shui kcr station nr908 tin shing court - causeway bay nr909 tin yiu estate - kwun tong nr913 palm springs - sheung shui kcr station nr914 palm springs - fung yau street north nr915 palm springs - wan chai nr917 fan kam road kam tin road - central wan chai nr918 lam kam road kam sheung road - central wan chai nr919 sai ching street yuen long - wan chai nr920 fung yau street north yuen long - granville square nr921 kingswood villas - tsuen wan mtr station nr922 fung kwan street yuen long - central wan chai nr923 royal palms, wo shang wai - sheung shui kcr station nr924 royal palms, wo shang wai - fung yau street north yuen long nr925 maywood court, kingswood villas - wan chai nr926 long ping estate - central quarry bay nr927 long ping estate - sha tin nr928 fung kwan street yuen long - kwun tong nr929 castle peak road - sha tin nr930 tin shui estate - sha tin nr931 tin shui estate - tsim sha tsui nr932 tin shui estate - cheung sha wan nr933 kin shing building, yuen long - sha tin nr934 tin yau court - kowloon city nr935 hung shui kiu - wan chai nr936 fairview park - hung hom kcr station nr939 kam tin - tuen mun nr940 san wai ha tsuen - sau fu street nr941 ha pak nai - on shun street refer to gmb 31 nr942 kam tin - tuen mun ferry pier nr943 beauty court bauhinia garden - wan chai nr944 beauty court bauhinia garden - tsim sha tsui nr945 yuen long yick fat tai hang mansions - north point nr946 the eldorado - tsim sha tsui nr947 palm springs - tsing yi mtr station nr948 fairview park - tsing yi mtr station nr949 parkside villa - on shun street nr950 park royale - on shun street circular nr951 scenic garden - on shun street

（已取消） nr831翠擁華庭- -大學火車站nr832觀瀾雅軒- -大學火車站nr833瑞峰花園- -大圍火車站nr91錦繡花園- -灣仔nr92錦繡花園- -荃灣nr93錦繡花園- -元朗nr94錦繡花園- -上水火車站nr95朗屏村- -上水火車站nr96朗屏村- -紅?車站nr97朗屏村- -灣仔nr98朗屏村- -紅?車站nr99朗屏村- -觀塘（鴻圖道） nr901嘉湖山莊樂湖居- -荃灣地鐵站nr902嘉湖山莊樂湖居- -上水火車站nr903嘉湖山莊- -灣仔nr904嘉湖山莊- -中港城nr905嘉湖山莊美湖居- -荃灣地鐵站nr906嘉湖山莊美湖居- -觀塘翠屏道nr907嘉湖山莊美湖居- -上水火車站nr908天盛苑- -銅鑼灣nr909天耀村- -觀塘nr913加州花園- -上水火車站nr914加州花園- -元朗（鳳攸街北） nr915加州花園- -灣仔nr917粉錦公路/錦田公路- -中環/灣仔nr918林錦公路/錦上路- -中環/灣仔nr919元朗（西菁街） - -灣仔nr920元朗（鳳攸街北） - -尖沙嘴（加連威老廣場） nr921嘉湖山莊- -荃灣地鐵站nr922元朗（鳳群街） - -中環/灣仔nr923加州豪園- -上水火車站nr924加州豪園- -元朗（鳳攸街北） nr925嘉湖山莊美湖居- -灣仔nr926朗屏村- -中環/鯽魚涌nr927朗屏村- -沙田nr928元朗（鳳群街） - -觀塘nr929青山公路- -沙田nr930天瑞村- -沙田nr931天瑞村- -尖沙嘴nr932天瑞村- -長沙灣nr933元朗（元發徑建成大廈） - -沙田nr934天佑苑- -九龍城nr935洪水橋- -灣仔nr936錦繡花園- -紅?車站nr939錦田- -屯門nr940廈村（新圍） - -元朗（壽富街） nr941下白泥- -元朗（安信街） [請參照專線小巴33 ] nr942錦田- -屯門碼頭nr943洪水橋（雅苑/紫翠花園） - -灣仔nr944洪水橋（雅苑/紫翠花園） - -尖沙嘴nr945元朗（益發/大興大廈） - -北角nr946金碧花園- -尖沙嘴nr947加州花園- -青衣地鐵站nr948錦繡花園- -青衣地鐵站nr949柏麗豪園- -安信街nr950御豪山莊- -安信街（循環線） nr951御景園- -安信街

Lab. and field test of hunan sepiolite drilling mud

湖南永和海泡石的石油鉆井泥漿試驗

Mud and silt have been continuously deposited in the lake.

泥沙不停地淤積在這湖裡。

The yanchang formation is divided, for the first time, into six third - order sequences, each with an average time duration of about 4. 5 ma. the single sequence is composed of deltaic and lacustrine sandstones, siltstones and mudstones. the subaerial and subaqueous distributary channel and channel - mouth bar sandstone reservoirs are well developed mainly in the lowstand and highland systems tracts

論文在富縣探區首次應用陸相層序地層學的觀點和方法，把延長組劃分為6個三級層序，平均時限4 . 5ma ，各層序由三角洲與湖泊相砂、泥巖沉積組成，主要在低位體系域和高位體系域發育水下（上）分流河道和河口砂壩砂巖儲層

Aiming at five kinds of targets from geneva lake which are rock, sand, pebble, grit and sullage, the features we extracted based on the cwt time - frequency matrix are singular values, some parameters of histogram and invariant moment

針對萊蒙湖底的巖石、沙、卵石、砂礫、淤泥等五類目標，文中所提取的特徵主要有時頻矩陣的奇異值、直方圖的有關參數以及不變矩等三類特徵。

The analyzed results are as follows : the late 1960 ' s cutoff of riverbends increased both the runoff amount and the sediment transport amount of the lower reach of jingjiang river, while the sediment deposition decreased in the lkngting lake area ; after the mid 1980 ' s, both the middle reach of yangtze river main stem and the dongting lake occurred a trend of decreasing annual sediment transport as a result of decreasing sediment releasing from the upper reach of yangtze river ; and in the recent 3 years ( 2003 - 2006 ), the three gorges reservoir first impoundment additionally reduced the sediment concentration in the middle reach of yangtze river flow with a long time, so a distance would be quite long for suspended sediment recovery, but the distance for bed - material load of suspended sediment recovery would be quite short

分析結果表明： 20世紀60年代下荊江裁彎后，三口（松滋口、太平口、藕池口）分流分沙減少，下荊江徑流量和輸沙量相應增加，洞庭湖泥沙淤積減少； 80年代中期以後，長江中游幹流及洞庭湖出口的年輸沙量呈減少趨勢，城陵磯至武漢河段河床由淤積轉為趨向沖淤平衡；三峽工程初期蓄水運用后，長江中游含沙量沿程恢復距離較長，但床沙質部分恢復距離相對較短。

Analysis and preventive strategy on main source of sediment in river and lake in jiangxi province

江西省河湖泥沙的主要來源及防治對策