tufa
- n.凝灰岩;钙华;石灰岩
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The floristic characteristics of tufa bryophytes and the main Travertine Deposition types in UK
英国钙华苔藓植物区系特征及其主要钙华沉积类型
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Bio - effect on Tufa Deposition
钙华沉积的生物效应
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The study of aeration effect on Mechanism of fluvial tufa deposit
河成石灰华成因&掺气效应研究
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Accordingly , the development process model of calcareous tufa is proposed preliminarily .
文中还初步提出研究区微生物(蓝藻等)起控制作用的石灰华发生和形成过程模式。
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Characteristics of ancient tufa and its prospecting signifcance in Northwest Hunan
湘西北地区的古硅华特征及其找矿意义
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The odd shapes that tufa take can sometimes resemble coral .
凝灰岩有时可以具有像珊瑚那样的奇怪形状。
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A special tufa fabric-stratified-algae-support fabric and the cause of its formation
一种特殊的石灰华组构&层状藻支架组构及其成因
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The uncanny tufa formations take on a golden appearance at sunset .
离奇的凝灰岩地层在日落时所呈现出的金黄色外观。
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Age Measurement and Significance of Calcareous Tufa of Lunan Stone Forest , Yunnan , Chian
中国路南石林地区钙华年代测定及其意义
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Made of limestone , tufa forms as a byproduct of the precipitation of carbonate minerals from surrounding water .
LimestoneBuildup石灰岩的构成凝灰岩是由石灰岩所组成,它是在其周围湖水里的碳酸盐矿物沉淀的副产品。
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The tufa towers rise like giant sand castles , peeking above Mono Lake 's surface .
BytheShore在岸边钙华塔升高得像巨型的沙堡,它正在窥视着莫诺湖的表面。TufaTowers钙华塔
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So , the appropriate geochemical condition and the advantaged water dynamic condition compose the growth of the tufa of Wang 4 well .
王4井的地热流体正是具备了合适的水化学条件,同时伴随着有利的水动力条件才生成了我们所看到的钙华。
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Mono Lake 's tall grasses and shrubbery are shown growing along the bottom of this tufa formation .
GrownOver长高了莫诺湖的高茎草和灌木林沿着凝灰岩地层的底部生长起来。
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The formation of tufa in huanglong , Sichuan
四川黄龙钙华的形成
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Fossil plants from calcareous tufa and palaeoenvironments in ruoqiang , Xinjiang
新疆若羌石灰华中的植物化石及古环境
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Another strangely beautiful early morning shot of the tufa formations , with the Sierra Nevada Mountains in the background .
这是另一张在清晨所拍摄形态奇怪而又美丽的凝灰岩照片,背景是内华达山脉。
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The delicate white tufa towers formed where freshwater springs percolate up from the bottom of the lake .
柔和、白色的钙华塔形成于淡水泉从湖底渗透出来的地方。
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Deep-source co_2 in natural waters and its role in extensive tufa deposition in the Huanglong ravines , sichuan , China
四川黄龙沟天然水中的深源CO2与大规模的钙华沉积
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A sunset casts a warm glow over the tufa formations as seagulls forage for dinner .
当海鸥在寻找晚餐时,夕阳在凝灰岩地层上面投射了温暖的光辉。AlabasterandAzure光洁雪白和天蓝色
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Tufa , as a product of karstification , is a carbonate sediment in pools , rivers , or springs .
钙华作为岩溶作用的产物,又称泉华或石灰华,是指湖泊、河流或泉水所形成的以碳酸钙为主的碳酸盐沉积物。
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The more recent calcareous , or calcium carbonate , deposits that make up the tufa formations are closer to the bottom and lighter in color .
钙质或碳酸钙越近现代,所构成凝灰岩地层的沉积物越靠近底部,颜色也比较浅。
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The torrent flowed along the surface of the hardened tufa , and destroyed the few meager skeletons of trees which had withstood the first eruption .
洪流沿着凝固了的凝灰岩表面流去,把第一次火山爆发以后残存下来的几棵干枯的树干都摧毁了。
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Tufa , the unusual rock formations that jut out of Mono Lake in California 's Eastern Sierra , are famous for their otherworldly beauty .
MoonlitMonoLake洒满月光的莫诺湖凝灰岩,是突出在加利福尼亚州的东部雪乐山的莫诺湖面的不同寻常的岩层,以其超凡脱俗的美丽而闻名于世。
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Tufa is a good carrier which records the information of palaeoclimate-environment , and has the unique superiority : ( 1 ) The resolution is high , may achieve the resolution of season or month .
钙华是记录古气候环境信息的良好载体,并有独特的优势:①分辨率高,可达到季-月的高分辨率。
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A STUDY ON BIOGENETIC OF CALCAREOUS TUFA & Examplified by the tufa in Jiuzhaigou , Sichuan , and Huangguoshu , Guizhou
石灰华的生物成因研究&以四川九寨沟和贵州黄果树等地石灰华为例
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These pale gray and ivory " tufa towers ," located in California 's Mono Lake , may look like eerie art instillations , but they occur naturally and are made of limestone .
这些浅灰色和象牙形的“钙华塔”,位于美国加州的莫诺湖,它们可能看起来像是令人毛骨悚然的艺术灌注物,然而它们是在自然界里由石灰岩所构成的。
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These pale gray and ivory " tufa towers , " located in California 's Mono Lake , may look like eerie art instillations , but they occur naturally and are made of limestone .
WhimsicalTowers稀奇古怪的钙华塔这些浅灰色和象牙形的“钙华塔”,位于美国加州的莫诺湖,它们可能看起来像是令人毛骨悚然的艺术灌注物,然而它们是在自然界里由石灰岩所构成的。
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According to previous researches , tufa results from the supersaturation of calcium carbonate , as the partial pressure of CO_2 in the spring water is higher than that in the atmosphere and CO_2 outgases from the water .
根据研究,钙华的形成是由于泉水中的CO2分压高于周围空气的CO2分压,CO2从水中逸出,因而导致碳酸钙发生过饱和并产生沉淀的结果。
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It was found by in-situ monitoring that the Xiangshui River has a very low concentration of calcium and bicarbonate , which does not match with the huge tufa deposits in the riverbed and the dense vegetation cover in surrounding area .
文章报道了响水河河水的现场监测结果,得到响水河河水的Ca2+和HCO-3非常低,这明显与河床中大规模钙华的存在和景区内发育的茂密植被不匹配;
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By 1982 , the lake had lost 51 percent of the surface area it had before the diversions began in 1941 , revealing once-submerged tufa ( limestone ) , which now forms scenic , jutting towers across the water 's surface .
自从1941年开始改道,一直到1982年,这片湖已经流失了51%的表面面积,露出了曾一度淹埋在水下的凝灰岩(石灰石),像塔一样耸立在水面,形成了一道独特的风景。