Baum Lauren, Arnold Thomas C.
LSU Health Shreveport
LSU Health - Shreveport
Silica, or silicon dioxide (SiO), comprises a silicon atom and 2 oxygen atoms. Silica is the most plentiful mineral on Earth, distributed throughout the Earth's crust as silicate minerals. Silica is the main constituent of more than 95% of rocks and stones. Occupational exposure to silica dust is one of the oldest known forms of lung disease, first documented by Hippocrates in 400 BC describing breathing disorders in metal diggers. In the 1600s, van Diemerbrock noted the harmful effects of inhaling granite dust. Ramazzini provided a detailed description in the 1700s of the lung scarring observed in stone and coal workers. During the industrial revolution, advancing mechanization of production techniques increased workers' risk of contact with higher concentrations of silica dust. In 1832, it was noted that sandstone workers had significantly shorter life expectancies compared to limestone and brick workers, often dying by the age of 40. The Hawks Nest Tunnel disaster of the 1930s was one of the worst industrial disasters in American history. To create a large tunnel that would redirect a river to power a hydroelectric plant in West Virginia, workers drilled through rock in a confined space without ventilation or respiratory protection. Many developed disabling lung damage within a few months due to exposure to high silica concentrations. The burden of silica-associated disease remains high, and silicosis is currently the world's most prevalent chronic occupational disease. Many industries place workers at risk of inhaling silica-containing dust, including abrasive blasting, denim jean manufacture, artificial stone production, brickwork, pottery, porcelain work, tunneling, mining, and structural construction and demolition. Silica exists in amorphous and crystalline forms that have unique physiochemical properties. Amorphic silica is found in biological matter such as plants, sponges, algae, fungi, and bacteria and nonvegetative matter such as volcanic glass, colloidal sols, and powders. Amorphic silica is not considered toxic. Crystalline silica is a mineral commonly known as quartz, present in granite and sandstone. In contrast to the random orientation of molecules in amorphous silica, crystalline silica exhibits a fixed, repeating, polymerized silicon-oxygen tetrahedral framework. Crystalline silica exists in various forms, including α-quartz, β-quartz, α-tridymite, β-tridymite, α-cristobalite, β-cristobalite, keatite, coesite, stishovite, and moganite. α-Quartz is the most common crystalline silica and the most biologically toxic form. Particles of crystalline silica are considered biologically active when small enough in diameter to reach the distal bronchioles and alveoli of the lungs. Such particles are denoted as "respirable crystalline silica" (RCS) and are less than 5 μm in diameter. RCS is released into the atmosphere by crushing, grinding, or cutting silica-containing matter. RCS can easily go unnoticed as it is odorless, colorless, and nonirritating. In 1997, the International Agency for Research on Cancer labeled RCS as a human carcinogen. Silica also exists as "silica nanoparticles" (SiNPs), particles of nanoform silicon dioxide that measure less than 100 nm in diameter. SiNPs have physiochemical characteristics distinct from the bulk form of silica. SiNPs are colloidal metal oxides comprising a siloxane (Si-O-Si-O) core with abundant silanol (Si-OH) surface groups. SiNPs are either mesoporous or solid. The silica matrix of mesoporous SiNPs has many channels and pores, whereas solid SiNPs have no pores. Mesoporous SiNPs have a controllable, uniform pore size, large volume-to-surface ratio, easily modifiable surface chemistry, and exceptional biocompatibility. The silica framework of SiNPs yields many advantageous qualities, such as its stability in acidic conditions, temperature fluctuations, and organic solvents. The pores of mesoporous SiNPs can be filled with various biomolecules. Silicosis, a type of pneumoconiosis, occurs secondary to the inhalation of RCS and causes progressive, irreversible, and fatal lung inflammation and fibrosis. While the condition is preventable, no treatment exists. Silicosis increases susceptibility to Mycobacterial diseases, autoimmune diseases, and bronchogenic carcinoma. This activity reviews the etiology, epidemiology, pathophysiology, clinical findings, evaluation, and management of patients with silicosis.
二氧化硅,即硅 dioxide(SiO₂),由一个硅原子和两个氧原子组成。二氧化硅是地球上含量最丰富的矿物质,以硅酸盐矿物的形式分布在地壳中。二氧化硅是超过95%的岩石和石头的主要成分。职业性接触二氧化硅粉尘是已知最古老的肺部疾病形式之一,最早由希波克拉底在公元前400年记录,描述了金属挖掘工人的呼吸障碍。在17世纪,范·迪默布罗克指出吸入花岗岩粉尘的有害影响。拉马齐尼在18世纪详细描述了在石材和煤炭工人中观察到的肺瘢痕形成。在工业革命期间,生产技术的机械化进步增加了工人接触更高浓度二氧化硅粉尘的风险。1832年,有人指出砂岩工人的预期寿命明显短于石灰石和砖工工人,他们常常在40岁时就去世。20世纪30年代的霍克斯奈斯特隧道灾难是美国历史上最严重的工业灾难之一。为了建造一条大型隧道,将一条河流改道以为西弗吉尼亚州的一座水力发电厂提供动力,工人们在一个没有通风或呼吸防护的密闭空间中钻凿岩石。许多人由于接触高浓度二氧化硅,在几个月内就患上了致残性肺部损伤。与二氧化硅相关疾病的负担仍然很高,矽肺病目前是世界上最普遍的慢性职业病。许多行业使工人面临吸入含二氧化硅粉尘的风险,包括喷砂、牛仔布制造、人造石生产、砌砖、陶器、瓷器制作、隧道挖掘、采矿以及建筑结构施工和拆除。二氧化硅以无定形和结晶形式存在,具有独特的物理化学性质。无定形二氧化硅存在于植物、海绵、藻类、真菌和细菌等生物物质以及火山玻璃、胶体溶胶和粉末等非植物物质中。无定形二氧化硅不被认为有毒。结晶二氧化硅是一种通常称为石英的矿物,存在于花岗岩和砂岩中。与无定形二氧化硅中分子的随机取向不同,结晶二氧化硅呈现出固定的、重复的、聚合的硅 - 氧四面体框架。结晶二氧化硅以多种形式存在,包括α - 石英、β - 石英、α - 鳞石英、β - 鳞石英、α - 方石英、β - 方石英、柯石英、斯石英、超石英和莫干石。α - 石英是最常见的结晶二氧化硅,也是生物毒性最强的形式。当结晶二氧化硅颗粒直径小到足以到达肺部的终末细支气管和肺泡时,就被认为具有生物活性。这种颗粒被称为“可吸入结晶二氧化硅”(RCS),直径小于5μm。RCS通过粉碎、研磨或切割含二氧化硅物质释放到大气中。由于RCS无味、无色且无刺激性,很容易被忽视。1997年,国际癌症研究机构将RCS列为人类致癌物。二氧化硅还以“二氧化硅纳米颗粒”(SiNPs)的形式存在,即直径小于100nm的纳米级二氧化硅颗粒。SiNPs具有与块状二氧化硅不同的物理化学特性。SiNPs是胶体金属氧化物,由具有丰富硅醇(Si - OH)表面基团的硅氧烷(Si - O - Si - O)核心组成。SiNPs要么是介孔的,要么是实心的。介孔SiNPs的二氧化硅基质有许多通道和孔隙,而实心SiNPs没有孔隙。介孔SiNPs具有可控的、均匀的孔径、大的体积与表面积比、易于修饰的表面化学性质以及出色的生物相容性。SiNPs的二氧化硅框架具有许多有利特性,例如在酸性条件、温度波动和有机溶剂中的稳定性。介孔SiNPs的孔隙可以填充各种生物分子。矽肺病是一种尘肺病,继发于吸入RCS,会导致进行性、不可逆且致命的肺部炎症和纤维化。虽然这种疾病是可预防的,但目前尚无治疗方法。矽肺病会增加对分枝杆菌疾病、自身免疫性疾病和支气管源性癌的易感性。本活动回顾了矽肺病患者的病因、流行病学、病理生理学、临床发现、评估和管理。