共查询到20条相似文献,搜索用时 93 毫秒
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我国茶具 ,种类繁多 ,造型优美 ,既有实用价值 ,又富艺术之美 ,所以驰名中外 ,为历代饮茶爱好者所青睐。人们在品饮茶的过程之中 ,茶具也相应地发生了一些变化。茶具 ,按狭义的范围 ,主要指茶杯、茶碗、茶壶、托盘等饮茶用具。芳香美味的茶叶配上质优、雅致的茶具 ,更能衬托茶叶的颜色 ,保持浓郁的茶香。通常茶具大概可分为陶土茶具、瓷器茶具、漆器茶具、玻璃茶具、金属茶具、竹木茶具等。一、竹木茶具 :因其易吸收茶味 ,且不便观察汤色 ,所以较少使用。二、金属茶具 :其中较常见的是以锡为储茶器具材料 ,因为锡罐多制成小口长颈 ,盖为筒状… 相似文献
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常言道:“水为茶之母,壶为茶之父”。这实在是茶人茗客对茶、水、壶三者互为依存、相映成辉关系的独到精辟之见。中国的品茶艺术,从唐代开始就注重韵味、追求高雅情趣和深远意境。香茶配佳壶,佳壶倍添品茶意趣,香茗频增壶艺价值,恰似红花映衬绿叶,相得益彰。因而,自明代以降,会“玩”茶品茗的,必定会“玩”壶把盏,这也可以说是一种珠联璧合吧! 一茶壶,源于何年何代,出于何人之手,现已不可深究。在唐代茶圣陆羽的《茶经》中,并没有茶壶的记载,《六之饮》中也只有“贮于瓶伍之中”。据考,壶是古代一种无柄、大口、无盖、短身、圆肚的盛水器或酒器。《周礼》在《夏官》、《秋官》两章中就分别注释为:“壶,盛水器也”“壶,酒器也”。《周礼》还提到一种祭祀用的玄 相似文献
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(一)白鹤沐浴(1)洁具涤尘当在先,谓如白鹤沐清泉。孟臣壶(2)上水经过,杯有若琛(3)浴后编注:(1)白鹤沐浴(洗杯):用开水洗净茶具。(2)孟臣壶:乌龙茶具,来自人名。史载明天启年间宜兴著名制陶师叫惠孟臣,他精制的紫砂茶壶落有“孟臣”款,茶人遂习惯称为“孟臣壶”。(3)若深杯:亦来自人名,史载“若深所制茶杯”形美质佳。(二)观音入宫(1)茶名雅号铁观音,品种优良环宇闻。问得入宫茶几许?常规容量五公分。注:(1)观音入宫(投茶):把铁观音茶放入茶具,放茶量约占茶具容量的五公分。(三)高山流水(… 相似文献
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羊年伊始,上海‘四海茶具馆’内鲜花争艳,水仙溢香,荡漾着一派盎然的新春气息。红木陈列橱内,一把把古朴典雅、款式优美的紫砂名壶,弥散出一种独特的文化情韵。难怪远道慕名而来的台湾著名画家李奇茂教授边欣赏边连连对‘四海茶具馆’王人许四海说:‘我今天太高兴了,太愉快了,这里真是集天下名壶之大成!’被称为‘江南壶怪’的许四海,近年来以精湛的构思、多变的造型、考究的做工,制作了不少紫砂艺术壶。同时,他更以丰富的名壶收藏而名扬海内外,在台湾紫砂界也有很大的影响。这次李奇茂教授来上海开画展,虽然时间短暂、活动日程表排得满满的,但自称是‘壶迷’的李教授感到 相似文献
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西汉王褒《僮约》中“烹荼尽具”一词,是关于我国文字中最早的茶具记载。到了唐代,在唐诗中随处可见。茶与壶称为一对孪生兄弟,品茗者必有壶,国人都讲紫砂壶,一来是为了保证茶叶冲泡出的效果,二来为了提高饮茶的档次,三来也是一种爱好和收藏的需要,有的爱茶人珍藏紫砂壶成癖……那么,一把茶壶的制作流程, 相似文献
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ICP-OES法同时测定果蔬中铅、砷、镉、铬、铜、锡含量 总被引:2,自引:0,他引:2
果蔬样品经混酸消化后,控制一定的酸度,定容后应用等离子体发射光谱法(ICP-OES)对果蔬中铅、砷、镉、铬、铜、锡六种有害重金属进行测定,研究了分析测定条件,方法简单快速。测定结果表明,五种元素的加标平均回收率在91.0%~107%之间。其RSD均小于3.5%。按该方法进行处理及测定铅、砷、镉、铬、铜、锡,在选择的测定条件下最低检出限分别为0.0006 mg/kg、0.0003 mg/kg、0.00003 mg/kg、0.00005 mg/kg、0.00003 mg/kg、0.0006 mg/kg。 相似文献
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通过野外调查、标本采集、分类学研究及资料考证,基本摸清了贵州樟科、莲叶桐科、景天科、堇菜科、柳叶菜科、鹿蹄草科、柿科、山矾科、木犀科等9个科药用植物资源的种类与地理分布.结果发现贵州现有樟科药用植物49种4变种,莲叶桐科药用植物5种,景天科药用植物21种,堇菜科药用植物19种1变种,柳叶菜科药用植物20种4变种,鹿蹄草科药用植物7种1变种,柿科药用植物9种1变种,山矾科药用植物12种,木犀科药用植物30种3变种.其中,4种为贵州特有药用植物,40种5变种为贵州药用新资源. 相似文献
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Segregation of form, color, movement, and depth: anatomy, physiology, and perception 总被引:63,自引:0,他引:63
Anatomical and physiological observations in monkeys indicate that the primate visual system consists of several separate and independent subdivisions that analyze different aspects of the same retinal image: cells in cortical visual areas 1 and 2 and higher visual areas are segregated into three interdigitating subdivisions that differ in their selectivity for color, stereopsis, movement, and orientation. The pathways selective for form and color seem to be derived mainly from the parvocellular geniculate subdivisions, the depth- and movement-selective components from the magnocellular. At lower levels, in the retina and in the geniculate, cells in these two subdivisions differ in their color selectivity, contrast sensitivity, temporal properties, and spatial resolution. These major differences in the properties of cells at lower levels in each of the subdivisions led to the prediction that different visual functions, such as color, depth, movement, and form perception, should exhibit corresponding differences. Human perceptual experiments are remarkably consistent with these predictions. Moreover, perceptual experiments can be designed to ask which subdivisions of the system are responsible for particular visual abilities, such as figure/ground discrimination or perception of depth from perspective or relative movement--functions that might be difficult to deduce from single-cell response properties. 相似文献
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重金属稀土元素污染在水生物体内的生物富集 总被引:2,自引:0,他引:2
对铅、镉、汞以及镧、铈在鲤鱼体内的生物富集作用进行了室内试验和讨论。结果表明,重金属及稀土元素在鱼体各部位均有较强的富集作用,其中肌肉部分富集能力较弱,内脏富集能力最强;鱼体各部位对重金属及稀土元素的富集作用随时间的增加而增加,在一定的时间后趋于平衡;并且,鱼体中各部位对重金属及稀土元素的生物富集作用存在较大差异。 相似文献
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The finding of appreciable quantities of p,p'-DDT after feeding o,p'-DDT to rats led to the proposal of a theory, that an isomeric metabolic conversion occurs. The presence of p,p'-DDT as an impurity in supposedly pure samples of o,p'-DDT is the correct explanation for the appearance of p,p'-DDT. Purified o,p'-DDT and (14)C-labeled o,p'-DDT yielded no data to support the idea that o,p'-DDT is converted to the p,p'-DDT isomer. 相似文献
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The primary rocks are a sequence of titanium-rich basic volcanics, composed of clinopyroxene, plagioclase, and ilmenite with minor olivine, troilite, and native iron. The soil and microbreccias are respectively loose and compacted mixtures of fragments and aggregates of similar rocks, minerals, and glassy fragments and spheres. Impact events are reflected by the presence of shock metamorphosed rock fragments, breccias, and glasses and their resulting compaction to form complex breccias, glass-spattered surfaces, and numerous glass-lined craters. Chemistry of the glasses formed by the impact events is highly variable, and the high iron and nickel content of a few moundlike features suggests that at least some of the projectiles are iron and nickel-rich meteorites. 相似文献
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Macklis RM 《Science (New York, N.Y.)》2002,295(5560):1647-1648
Although Marie Curie is known primarily for her discovery of radium, her true gift to science was her realization that radioactivity is an intrinsic atomic property of matter rather than the result of chemical processes. She was one of the few Nobel laureates to win the prize twice (physics and chemistry). During her career and as one of the first prominent women scientists, she became increasingly aware of the need for funding for research and of the scientific freedom that money can bring. By nature shy and reserved, Marie's fame, as both a scientist and as an exemplar of a liberated professional woman of the roaring twenties, grew to superstar proportions. 相似文献
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Friedman I O'neil JR Adami LH Gleason JD Hardcastle K 《Science (New York, N.Y.)》1970,167(3918):538-540
The water content of the breccia is 150 to 455 ppm, with a deltaD from-580 to -870 per mil. Hydrogen gas content is 40 to 53 ppm with a deltaD of -830 to -970 per mil. The CO(2) is 290 to 418 ppm with delta (13)C = + 2.3 to + 5.1 per mil and delta(18)O = 14.2 to 19.1 per mil. Non-CO(2) carbon is 22 to 100 ppm, delta(13)C = -6.4 to -23.2 per mil. Lunar dust is 810 ppm H(2)O (D = 80 ppm) and 188 ppm total carbon(delta(13)C = -17.6 per mil). The (18)O analyses of whole rocks range from 5.8 to 6.2 per mil. The temperature of crystallization of type B rocks is 1100 degrees to 1300 degrees C, based on the oxygen isotope fractionation between coexisting plagioclase and ilmenite. 相似文献