Li Pengyu, Guo Ying
Department of Gemology, China University of Geosciences (Beijing), Beijing, 100083, China.
Sci Rep. 2025 Jul 4;15(1):23887. doi: 10.1038/s41598-025-09281-8.
Sugilite jade is an emerging jade material in the jewelry market with various shades of purple in appearance, and there is currently a gap in research on the blue and pink hues it possesses. The mineralogical and colorimetric characteristics of South African sugilite jade were studied using polarized light microscopy, X-ray fluorescence, X-ray powder diffraction, electron microprobe, infrared spectroscopy, and UV-Vis spectroscopy to explore the causes of its color. The primary mineralogical component of sugilite jade is sugilite, with minor constituents including pectolite-serandite, aegirine, alkaline amphibole, and alkaline feldspar. The purple hue of sugilite jade is attributed to the presence of Mn on the A site within the crystal structure of sugilite. It has been observed that the lightness and chroma of this color are positively correlated with the Mn content. The blue color is caused by Cu in pectolite and the pink color is attributed to Mn in serandite. The color of sugilite is primarily influenced by its broad absorption peak in the UV-visible spectrum, which occurs between 500 and 700 nm. The intensity of this peak is directly proportional to the concentration of Mn, which determines the lightness of sugilite jade. The presence of Cu results in a shift of the absorption peak to a higher wavelength, imparting a bluer color to the mineral.
苏纪石玉是珠宝市场上一种新兴的玉石材料,外观呈现出各种紫色调,目前对其拥有的蓝色和粉色调的研究存在空白。利用偏光显微镜、X射线荧光光谱、X射线粉末衍射、电子探针、红外光谱和紫外可见光谱对南非苏纪石玉的矿物学和比色特性进行了研究,以探究其颜色成因。苏纪石玉的主要矿物成分是苏纪石,次要成分包括硅灰石-赛兰石、霓石、碱性角闪石和碱性长石。苏纪石玉的紫色调归因于苏纪石晶体结构中A位上存在的锰。据观察,这种颜色的明度和彩度与锰含量呈正相关。蓝色是由硅灰石中的铜引起的,粉色则归因于赛兰石中的锰。苏纪石的颜色主要受其在紫外可见光谱中500至700纳米之间出现的宽吸收峰影响。该峰的强度与锰的浓度成正比,而锰的浓度决定了苏纪石玉的明度。铜的存在导致吸收峰向更高波长移动,使矿物呈现出更蓝的颜色。