Friday, December 4, 2015

An Introduction to Synthetic Gem Materials

An Introduction to Synthetic Gem Materials

 Robert Weldon
Synthetic Emeralds
A synthetic gem material is one that is made in a laboratory, but which shares virtually all chemical, optical, and physical characteristics of its natural mineral counterpart, though in some cases, namely synthetic turquoise and synthetic opal, additional compounds can be present.

Synthetic gem crystals have been manufactured since the late 1800s, and their production is often marked by a need for them in industrial applications outside of the jewelry industry. The first success was in producing synthetic ruby of faceting quality. Synthetic crystals are used in communications and laser technology, microelectronics, and abrasives. Because synthetics for jewelry applications can be “made to order” [i.e. consistent color and crystal shape] given the right ingredients, time, and the facilities to grow them, they are likely to be much less rare than natural gems of equal size, clarity, and saturation of color. Because of this, and because it is possible to confuse them with gems that are naturally occurring, there are strict guidelines regarding how they are marketed and sold.

In the United States, the Federal Trade Commission requires that any gem material produced in a laboratory be described in a way that leaves no doubt that it was not produced naturally. It is considered to be a deceptive practice if a synthetic gem material’s origin is not clearly disclosed throughout the distribution channel at the time of sale, from the manufacturer to the consumer. There are also a number of industry organizations such as the American Gem Trade Association (AGTA), the International Colored Gemstone Association (ICA), and the World Jewellery Confederation (CIBJO) that have formulated specific guidelines for their members regarding the disclosure of synthetic gems at the time of sale.
In the last decade fewer new kinds of man-made gem materials have been marketed. This suggests that the repertoire of synthetic gem materials is close to reaching its limit in terms of the creation of new materials, but it is not limited in production which is still very significant. During the last century, researchers have developed a number of different ways to create these synthetic gem materials in the laboratory. Most of these methods fall into two major categories – melt or solution.

In melt processes, the chemical composition of melt is the same as the composition of the resulting crystal. In solution processes, the solution or melt has a different chemical composition than that of the resulting crystal. Constituents are dissolved in the solution or melt at high temperature, and the crystal forms initially on a seed crystal as the melt temperature is lowered. Some of the main synthetic processes include:

FLAME FUSION OR VERNEUIL PROCESS (MELT PROCESS)

The first commercially successful synthetic gems were created by the flame fusion process. This process involves dropping powdered chemicals through a high-temperature flame, where it melts and falls onto a rotating pedestal to produce a synthetic crystal. Today it remains the least expensive and most common way to make gems such as synthetic corundum and spinel.

CRYSTAL PULLING OR CZOCHRALSKI PROCESS (MELT PROCESS)

Pulling emerged in the early 1900s. In this process, nutrients are melted in a crucible and the synthetic crystal grows from a seed that is dipped into the melt, and then slowly pulled away from the melt as it grows. Gems synthesized by pulling include synthetic alexandrite, chrysoberyl, corundum, and garnet.

FLUX GROWTH (SOLUTION PROCESS)

Today some synthetic gems, such as emerald, ruby, sapphire, alexandrite, and spinel can be created through a flux-growth process. Flux is a solid material that, when melted, dissolves other materials in the same way that water dissolves sugar. As the dissolved chemical solution gradually cools, synthetic crystals form.

Growing a synthetic gem by the flux method requires patience and significant investment. Crystal growth can take up to a year, and the equipment is very expensive. But the results, especially when it comes to emerald, are well worth the time and effort.

HYDROTHERMAL GROWTH (SOLUTION PROCESS)

Like the flux process, the hydrothermal growth process is slow and expensive. But it’s the only method for successfully growing synthetic quartz. This process requires heat and pressure and imitates the conditions deep in the earth that result in the formation of natural gems. Nutrients are dissolved in a water solution, and then synthetic crystals form as the solution cools.

While the following list encompasses the commonly seen synthetics, over the years there have also been experimental synthetic gems. These include malachite, color change synthetic spinel and others. But because nature produces these products more readily, they are not often seen today. Some of the synthetic gems that are more frequently encountered include:

SYNTHETIC DIAMOND (THIS IS NOT FREQUENTLY ENCOUNTERED)

These diamonds, grown in a laboratory, share most of the characteristics of their natural counterparts: they are essentially carbon.

Chemical vapor deposition (CVD) – diamond growth in a vacuum chamber due to a chemical reaction which releases carbon atoms that precipitate on diamond seed plates.

CVD Synthetic Diamonds
Some synthetic diamonds are produced by chemical vapor deposition (CVD), such as this group.
High pressure, high temperature (HPHT) – diamond growth from a melt flux which dissolves carbon at higher temperatures, and the diamonds form on seed crystals in a lower temperature portion of the growth chamber.
HPHT synthetic diamonds
Some diamonds are made in high pressure high temperature environments, including this collection of synthetic diamonds in a variety of colors.

SYNTHETIC CORUNDUM (WIDELY AVAILABLE)

Synthetic corundum, which includes ruby and sapphire, can be made by the greatest number of processes. Because of this, synthetic corundum is available at many price levels, from very affordable to very expensive.
Flame fusion synthetic corundum
Synthetic corundum can be made in a variety of ways including this colorful collection of flame fusion crystals, seen before cutting.

Ruby – in the late 1800s, ruby became the first gem to be created in a laboratory by Auguste Verneuil. In 1902, he announced the development of his flame-fusion process for synthesizing this beautiful gem.
 
Synthetic rubies
Synthetic ruby can be produced via flux growth processes (crystal and cut stone on left), and flame fusion (boule and cut stone on right).
Sapphire – some of the earliest examples of synthetic sapphires are in original pieces of art nouveau and art deco jewelry. Many synthetic sapphires are still made by flame fusion, but flux-grown sapphires have been available since the 1960s. Flux-grown, pulled and hydrothermal synthetic sapphires can be very convincing substitutes for the natural gem. Color change synthetic sapphire, made to imitate alexandrite, has been popular since the early 1900s. Induced inclusions caused star effects in some synthetic ruby and sapphire.
Synthetic star sapphires
Synthetic sapphires can be manufactured to show asterism (star effect), in cabochon cut stones, such as these.

SYNTHETIC EMERALD (WIDELY AVAILABLE) AND OTHER BERYLS (RARE)

Synthetic beryl is available in many colors including yellow, red, blue (aquamarine) and green (emerald). In the late 1980s and 1990s, Russia became a significant producer of these synthetic gems and is still a major supplier of hydrothermally grown gemstones such as synthetic beryl and synthetic corundum, along with others like synthetic diamond and synthetic alexandrite.
Synthetic beryl crystals
These are examples of synthetic beryl crystals and cut stones (including the synthetic emerald variety—the green stones).
Emerald – in the late 1930s, scientists finally synthesized a commercially profitable flux-grown version of this desirable deep green gem. Hydrothermal synthetic emerald for jewelry came on the scene in 1960.

SYNTHETIC QUARTZES (WIDELY AVAILABLE)

Gem-quality quartz, such as citrine, rose quartz, smoky quartz, and amethyst, is attractive. But natural gem-quality quartz is plentiful so scarcity is not the reason that researchers went to the trouble of developing a way to synthesize gem-quality quartz. The reason is that it plays a key role in technology. It can generate an electric current when it’s placed under pressure and can vibrate in precise response to alternating current. These virtues are put to practical use in watches, clocks, communications equipment, filters, and oscillators.

Amethyst: Lab-grown amethyst and other synthetic quartz varieties found their way into jewelry after being developed for industrial applications. The first hydrothermal quartz appeared in laboratories in the 1890s. It wasn’t until World War II that synthetic quartz was widely available commercially.
Natural and synthetic amethyst and synthetic rock crystal quartz crystal
Natural amethyst and rock crystal quartz crystals (left) and synthetic amethyst and synthetic rock crystal quartz crystal (right).

SYNTHETIC SPINEL (WIDELY AVAILABLE)

Early in the twentieth century, researchers trying to grow synthetic blue sapphire produced synthetic blue spinel by accident. Since then, synthetic spinel has been commonly used as a substitute for many natural gems. In the 1990s, a new Russian-made, flux-grown synthetic spinel was introduced in a variety of colors including red, a color not widely available through the older flame-fusion process.
Synthetic spinels
Synthetic spinels seen here are in crystal form as they appear from the manufacturer. The faceted stones can be found in any color, and are often used to simulate various natural gemstones.

SYNTHETIC OPAL (OCCASIONALLY SEEN)

In the 1970s, the Gilson Company developed a three-step process to make convincing synthetic opal. First, microscopic spheres of silica are created through precipitation. Next, the spheres settle in acidic water for more than a year. Finally, a hydrostatic press consolidates the spheres without distorting the stacked arrangement that creates opal’s play-of-color.
Synthetic opals
These synthetic opals are sometimes seen in the market, and to the unpracticed eye may appear to be highly valuable, natural white and black opal.

SYNTHETIC ALEXANDRITE (RARE)

Since there is not enough natural alexandrite to meet demand, various synthetics have appeared in the marketplace over the last few decades. Alexandrite has been synthesized by a number of different processes, including Czochralski, floating zone, and flux. Also, synthetic corundum with color-change is often used to imitate natural alexandrite. On rare occasions, synthetic color-change spinel may be encountered in the market.
Synthetic alexandrite
Synthetic alexandrites, such as this stone (shown in its incandescent and daylight colors) are somewhat rare. Less rare are imitations of alexandrite, including color-change synthetic spinel and sapphire.

宝石的种类

宝石矿物是具有宝石价值的天然矿物的总称。决定宝石价值的主要因素是颜色艳丽、透明无瑕、光泽灿烂,或是呈现变彩、变色、星光猫眼等光学效应;产出稀少;坚硬耐久,摩斯硬度在六以上,化学稳定性高。 
  宝石矿物多是自然元素、氧化物或含氧盐类矿物,其中硅酸盐矿物占近半数。自然界已发现的矿物已超过3000种,然而具有宝石价值者尚不及10%,其中的珍贵宝石矿物种属有钻石(金刚石)、祖母绿(绿柱石)、红宝石(刚玉)、蓝宝石(刚玉)、猫眼(金绿宝石)、变石(翠绿宝石)和翡翠(硬玉)等。 
   
  钻石以无色透明、光彩辉煌者为瑰宝;而祖母绿、红宝石和蓝宝石等,则以其瑰丽的色彩享得美名。国际宝石界把除钻石以外的宝石统称为有色宝石。这不仅是因为在价值和档次上有差别,而且从宝石质量评价、琢磨技术指标(如颜色分级和车工标准化)方面,钻石比有色宝石更有严格和特定的要求。 
   
  可充当宝石的矿物材料,尤其是高中档宝石,并不完全是天然产物。它们中有许多是与天然宝石矿物具有相同的化学组成、晶体结构以及物理和化学性质的人工合成矿物和各种仿制品。国际宝石市场上的主要高、中档宝石矿物总共约20余种,按摩斯硬度列述如下。 
   
  金刚石的宝石名为钻石,因其高硬度(摩斯硬度10)、高折射率(N=2.417)和强色散(O.044)而光辉绝伦、坚硬无比,素有“宝石之王”美名,是最珍贵的宝石。 
   
  钻石常呈黄、褐、蓝、绿和粉红等色,但以无色的为特佳。世界上重量超过620克拉(合124克)的特大宝石级金刚石共发现10粒,其中最大的名卡利南(Cullinan),重3106克拉(合621.35克),大小5×6.5×10厘米,1905年发现于南非的普雷米尔岩管。中国常林钻石,重158.786克拉,1977年发现于山东临沭县,列为世界名钻。世界金刚石主要产地有澳大利亚、扎伊尔、博茨瓦纳、前苏联、南非、巴西、纳米比亚、加纳、中非、塞拉利昂和中国等。 

刚玉 摩斯硬度9,宝石品种有红宝石、蓝宝石及星光红宝石和宝光蓝宝石,均属珍贵宝石。 
   
  红宝石因含氧化铬而呈鲜红色,以鸽血红为名贵。蓝宝石则是除红色以外的各色(包括无色)刚玉宝石的通称。蓝宝石颜色与铁、钛的氧化物含量有关,以艳蓝、天蓝色的为上品,而矢车菊蓝色的为特优。 
   
  红宝石主要产自缅甸、斯里兰卡巴基斯坦坦桑尼亚和泰国。蓝宝石主要来自澳大利亚、 缅甸、 柬埔寨、克什米尔斯里兰卡、泰国和美国,中国也有发现。现已发现的最大红宝石重3450克拉,最大的星光红宝石重138.7克拉,均产自缅甸。著名星光蓝宝石“印度之星”重536克拉,产于斯里兰卡。 
   
  金绿宝石 摩斯硬度8.5,宝石品种有猫眼和变石:都是宝石中的珍品。 
   
  猫眼是一种呈蜜黄至褐黄色、微透明至半透明状,有微细针、管状包裹体(平行C-轴排列)的金绿宝石变种,因其弧形抛光面呈现迷人的猫眼光学效应而享盛名。自然界具猫眼现象的其他宝石矿物还有如海蓝宝石猫眼、碧玺猫眼等,惟金绿宝石猫眼质量最佳,最名贵,因斯里兰卡(原称锡兰)特产,故也称锡兰猫眼。 
   
  变石也称亚历山大石,一种含微量氧化铬的金绿宝石变种,具有在日光下为玻璃状绿色、白炽光下现蔗莓红色的变色效应(或称变石效应)而出名。主要产地有斯里兰卡和前苏联,以及巴西、缅甸和津巴布韦等。 
   
  黄玉 摩斯硬度8。宝石品种颜色丰富,有淡黄、葡萄酒黄、蓝、绿和粉红等色,以葡萄酒黄色和蓝色的为上品。 现在世界上已发现的最大宝石级黄玉单晶产自巴西,晶体黄色透明,重117千克,大小43×41×40厘米。巴西也是世界上最主要的优质黄玉宝石原料来源地。其他产地有澳大利亚、缅甸、斯里兰卡、美国、前苏联、巴基斯坦和中国等。 
   
  尖晶石 摩斯硬度8。宝石矿物有红、粉红、蓝、绿和紫等色。主要品种有:红晶宝石,又名红宝尖晶石因含微量氧化铬而呈血红和玫瑰红色;蓝晶宝石,因似蓝宝石又名蓝宝尖晶石;锡兰石,因含微量铁而呈绿黑色;具四道和六道星光的星光尖晶宝石。产地有斯里兰卡、缅甸和阿富汗等。 

绿柱石 宝石名绿宝石。摩斯硬度7.5~8,绿柱石由于含痕量或微量的不同的过渡族元素而呈不同的颜色,宝石品种有:翠绿色的祖母绿;天蓝、蓝绿色的海蓝宝石 ;红、玫瑰红色的艳绿宝石;金黄色的黄绿宝石:无色的透绿宝石。 
   
  绿宝石中以祖母绿最为珍贵,素有“绿色宝石之王”的美誉,产地中以哥伦比亚为最著名,还有巴西、前苏联、南非、阿富汗、赞比亚、津巴布韦、印度和巴基斯坦等。已发现的最大祖母绿晶体重24000克拉,1956年发现于南非。 
   
  海蓝宝石亦为名贵品种,以天蓝色的为上品。世界上已发现的最大海蓝宝石晶体重110.5千克,长48.5厘米,1910年发现于巴西。巴西也是世界上优质海蓝宝石的主要产地。美国、前苏联、中国、马达加斯加、巴基斯坦和印度等也有产出。 
   
  锆石 摩斯硬度7~7.5。主要宝石品种有红锆石、蓝锆石和无色锆石。无色透明锆石由于高色散(0.039)可充当钻石代用品。 
   
  世界上已发现的最大的绿蓝色锆石宝石重208克拉,产自斯里兰卡。宝石级锆石主要产自泰国等中南半岛诸国、澳大利亚、坦桑尼亚、挪威和中国等。 
   
  电气石 宝石名碧玺。摩斯硬度7~7.5。宝石品种有粉红-红色碧玺、蓝色碧玺、绿色碧玺、双色-多色碧玺和碧玺猫眼等,以红色和蓝色品种为珍贵。 
   
  已知最大的碧玺晶体重12千克,长130厘米,柱径40厘米,1978年发现于巴西。主是产地有巴西、斯里兰卡、美国、前苏联、缅甸、坦桑尼亚和马达加斯加等。 
   
  石榴子石 摩斯硬度6.5~7.5。宝石品种的石榴子石随其端员组分和所含过渡元素杂质的不同而呈现各种艳丽颜色,其中以鲜艳红色和娇翠绿色的为最佳。 
   
  主要宝石矿物种或变种石榴子石有血红至紫红的镁铝榴石、紫红至棕红的铁铝榴石、玫瑰至紫红色的红榴石、绿至翠绿色的钙铝榴石、橙黄至褐红色的桂榴石、绿或粉红色的水钙铝榴石、蜜蜡黄至橙黄色的锰铝榴石、翠绿色的翠榴石、黄至绿黄色的黄榴石、黑色的黑榴石和祖母绿色的钙铬榴石。优质钙铬榴石享有“乌拉尔祖母绿”之美称。捷克和斯洛伐克、前苏联、美国、肯尼亚、坦桑尼亚、斯里兰卡、巴西、印度和中国等都有产出。 
   
  锂辉石 摩斯硬度7,宝石品种有:紫锂辉石,一种含微量锰、铁的玫瑰红至丁香紫色变种;翠铬锂辉石,一种含微量铬的翠绿色变种;还有猫眼宝石品种。产出地主要有美国、巴西、缅甸、马达加斯加和巴基斯坦等。 
   
  石英 摩斯硬度7,石英宝石矿物分显晶质和隐晶质两类。前者主要品种有水晶、紫水晶、黄水晶、烟晶虹彩水晶、石英猫眼、芙蓉石(蔷微石英)、发晶、鬃晶 ;后者包括光玉髓、绿玉髓、各色玛瑙、缠丝玛瑙、缟玛瑙、苔纹玛瑙、水胆玛瑙和碧玉等,其中以浓艳丁香紫色水晶、水晶猫眼、绿玉髓、蓝玛瑙和水胆玛瑙为上品中国和其他很多国家都有产出。 
   
  橄榄石 摩斯硬度6.5,宝石级橄榄石多为贵橄榄石以透明并呈橄榄绿色、金黄绿色者为上品。世界上已知最大宝石级绿色橄榄石单晶重319克拉,发现于缅甸。主要产地有埃及、缅甸、美国、中国和挪威等。 
   
  硬玉 宝石名翡翠,通常是由很细小的晶体紧密交织而成的致密块状集合体。摩斯硬度6.5~7。颜色有白、粉红、绿、淡紫、紫罗兰紫、褐和黑等色,以纯正匀净、浓艳翠绿色又质地细腻、温润为高档。缅甸素以特产优质翡翠著称于世,美国和前苏联也有产出。 
   
  软玉是透闪石-阳起石系列矿物的显微纤维状集合体变种。摩斯硬度5~6,韧性较强。 
   
  软玉是仅次于翡翠的名贵玉种,以其温润、纯朴赢得吉祥、纯洁和高贵象征之美誉呻国对软玉的开发利用有近3000年的历史,精湛绝美的玉雕艺术堪称东方瑰宝。主要品种有白玉、青玉、碧玉、托帕石和墨玉,以羊脂白玉为名贵品种。中国的新疆和台湾盛产软玉,尤以新疆和田玉著称于世。前苏联、加拿大、新西兰、澳大利亚和美国等也有产出 
   
  长石 摩斯硬度6~6.5。主要宝石品种有:月光石,呈淡蓝白色,柔和晕彩闪光的透长石或更长石;虹彩拉长石,显现变彩的拉长石 ;还有钠长石猫眼和艳绿、天蓝色的天河石等品种。主要产地有前苏联、美国、加拿大、斯里兰卡、马达加斯加、印度、缅甸和挪威等。 
   
  黝帘石 摩斯硬度6。主要宝石品种是坦桑石,一种含微量钒的蓝至紫罗兰色透明的黝帘石变种,以及蓝色猫眼宝石。 
   
  方柱石 摩斯硬度6。宝石品种有呈海蓝色、紫罗兰色、粉红色、黄色的透明宝石和猫眼宝石,后者由内部平行C-轴排列的管状孔穴包裹体所致。主要产出地有缅甸、斯里兰卡、巴西、印度、马达加斯加、坦桑尼亚和莫桑比克等。 
   
  贵蛋白石 中文名欧泊。摩斯硬度5.5~6.5。欧泊宝石以色彩缤纷、变幻鲜明强烈的为优质。主要品种有:白欧泊,一种底色透明、无色至乳白色的贵蛋白石;黑欧泊,一种底色呈黑色或深绿、深蓝、深灰或褐色的贵蛋白石,以黑色的最佳,为欧泊宝石中的名贵品种 ;火欧泊,一种底色黄、橘黄、紫红色的贵蛋白石。澳大利亚欧泊的质量和产量均居世界之首,其他产出地有捷克和斯洛伐克、墨西哥、印度尼西亚和巴西等。 
   
  绿松石 宝石名松石,也称土耳其玉,多为隐晶质块状产出,摩斯硬度5.5~6。自然界中绿松石常因铁离子置换一定量的铜而呈现黄绿、蓝绿和苹果绿色,天蓝色的少见,而以呈知更鸟蛋蓝色的为最佳,质地纯净密实的为优质。著名产地有伊朗、美国、前苏联、中国和埃及等。 
   
  青金石 宝石名指一种含星点状黄铁矿、蓝方石和方钠石等矿物,而有如繁星似锦、通体碧蓝的块状青金石宝石 ,摩斯硬度5.5。阿富汗自古以来以盛产优质青金石著称。前苏联、智利、美国和加拿大等亦有产出。 
   
  紫硅碱钙石 一种单斜晶系的钾、钙、钠的含水硅酸盐矿物,多呈隐晶质块状,摩斯硬度5~6。宝石级矿物为淡紫和紫红色,以质地细腻、花纹清晰为优质玉石;纯净透明至半透明的可作宝石。