Quartz glass develops internal stress when exposed to non-uniform temperatures. At any given temperature, quartz glass exhibits a specific atomic structure that is most "suitable" or stable under those thermal conditions. The spacing between atoms changes with temperature—this is known as thermal expansion. When quartz glass experiences uneven heating or cooling, differential expansion occurs.
Stress typically arises when hotter regions attempt to expand but are constrained by surrounding cooler areas. This results in compressive stress, which usually does not damage the product. If the temperature is high enough to soften the quartz glass, the stress may be relieved. However, if the cooling process is too rapid, the viscosity of the material increases too quickly, and the atomic structure cannot adjust in time to accommodate the temperature drop. This leads to the formation of tensile stress, which is more likely to cause structural damage.
Stress increases progressively as the temperature drops and can reach high levels after cooling ends. In fact, when the viscosity of quartz glass exceeds 10^4.6 poise, the temperature is referred to as the strain point—at this stage, the viscosity is too high for stress relaxation to occur.
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Mechanical processing such as cutting, grinding, and polishing can introduce surface lattice distortion, resulting in machining stress. For example, cutting with a grinding wheel generates localized heat and mechanical pressure at the edge, leading to stress concentration. Improper techniques during drilling or slotting can create notches that act as crack initiation sites.
When used as a structural material, fused quartz may bear mechanical loads such as pressure or bending, generating macroscopic stress. For instance, quartz containers holding heavy substances develop bending stress.
Although fused quartz has an extremely low coefficient of thermal expansion (~0.5×10⁻⁶/°C), rapid temperature changes (e.g., heating from room temperature to high temperatures or immersion in ice water) can result in localized thermal expansion or contraction, causing instantaneous thermal stress. Laboratory glassware made of quartz may fracture under such thermal shocks.
Under long-term cyclic thermal environments (e.g., furnace linings or high-temperature optical windows), repeated thermal expansion and contraction can accumulate fatigue stress, accelerating material aging and cracking.
When fused quartz comes into contact with strong alkaline solutions (e.g., NaOH) or high-temperature acidic gases (e.g., HF), its surface may undergo chemical corrosion or dissolution, disrupting structural uniformity and causing chemical stress. Alkaline attack can cause surface volume changes or form microcracks.
In chemical vapor deposition (CVD) processes, coating quartz with materials like SiC may introduce interfacial stress due to mismatches in thermal expansion coefficients or elastic moduli between the film and the substrate. Upon cooling, such stress may cause film delamination or substrate cracking.
During melting, residual gas bubbles or impurities (e.g., metal ions or unmelted particles) may become trapped in fused quartz. The difference in physical properties (e.g., thermal expansion coefficient or modulus) between these inclusions and the surrounding glass can lead to localized stress concentration, increasing the risk of crack formation around bubbles under load.
Impurities in raw materials or melting defects can lead to microcracks in the quartz. When subjected to external loads or temperature fluctuations, stress concentration at crack tips can intensify, accelerating crack propagation and ultimately compromising the material's integrity.