11.13
흡착 등온은 기체 또는 액체상 분자가 표면과 어떻게 상호작용하는지 설명하는 수학적 모델입니다. 가장 흔한 등온선 모델 두 가지는 랭뮤어 등온선과 프로인들리히 등온선으로, 이는 유형 I 단층 화학흡착과 관련이 있습니다. 랭뮤어 모델은 네 가지 주요 가정에 기반합니다:
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1형 흡착 등온선은 흡착된 분자의 양과 일정 온도에서 압력을 연관시키는 화학흡착을 설명합니다.
비해리성 흡착에 대한 랭뮤어 등온에 따르면, 흡착은 서로 상호작용하지 않는 동일한 표면 부위에 가역적 단일층을 형성합니다.
표면 M에 가역적으로 흡착하는 기체 A를 생각하자. 흡착은 속도 상수 ka , 탈부착은 kd에 의해 결정된다. 흡착율은 압력과 빈 부위의 수에 따라 달라지며, 탈착율은 점유된 부위의 수에 따라 달라집니다.
평형 상태에서 이 속도를 동일하게 하면 랭뮤어 방정식이 나오며, 분수 커버리지를 압력에 α 파라미터(흡착율과 탈착율 상수의 비율)를 통해 연결됩니다.
변형된 랭뮤어 등온성은 이원자 분자가 원자로 분리되어 흡착 표면의 별도 위치를 차지하는 해리성 흡착을 설명합니다. 평형 상태에서 흡착율과 탈부착율을 동일하게 하고 식을 재배열하면 수정된 랭뮤어 방정식이 됩니다.
두 모델 모두에서 분별 적용 범위는 저압에서 선형적으로 증가하며, 대부분의 지표면 부위가 점유되는 매우 높은 압력에서는 포화에 근접합니다.
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Q1: What is the Langmuir isotherm and how does it describe adsorption?
The Langmuir isotherm describes chemisorption by relating the amount of adsorbed molecules to pressure at constant temperature. It assumes adsorbate molecules form a reversible monolayer on identical, non-interacting surface sites. At equilibrium, the adsorption rate equals the desorption rate, yielding an equation that links fractional coverage to pressure through a parameter representing the ratio of adsorption and desorption rate constants.
Q2: How does fractional coverage change with pressure in the Langmuir model?
At low pressures, fractional coverage increases linearly with partial pressure of gas molecules. As pressure increases, coverage rises more gradually and approaches saturation only at very high pressures where most surface sites are occupied. This behavior reflects the competition between adsorption collisions and desorption from occupied sites.
Q3: What are the four key assumptions underlying the Langmuir isotherm?
The Langmuir model assumes adsorption cannot exceed monolayer coverage, all surface sites are equivalent, molecules adsorb only at vacant sites, and there are no interactions between adsorbed molecules. These assumptions simplify the mathematical treatment of gas-surface interactions and make the model applicable to many chemisorption systems.
Q4: How does dissociative adsorption differ from non-dissociative adsorption?
In non-dissociative adsorption, each molecule occupies one surface site and fills the surface rapidly. In dissociative adsorption, diatomic molecules dissociate into atoms that occupy separate sites, requiring a pair of adjacent vacant sites. This stoichiometric difference means dissociative adsorption progresses more slowly and shows different pressure dependence in the modified Langmuir equation.
Q5: What role do adsorption and desorption rate constants play in the Langmuir equation?
The adsorption rate depends on pressure and vacant sites, governed by the adsorption rate constant. The desorption rate depends on occupied sites, governed by the desorption rate constant. At equilibrium, these rates are equal. The ratio of these constants, called alpha, directly determines how fractional coverage responds to changes in pressure.
Q6: When is the Freundlich isotherm more accurate than the Langmuir model?
The Freundlich isotherm is often more accurate than the Langmuir isotherm at intermediate pressures. Unlike Langmuir, it allows for multiple types of adsorption sites on the solid, each with different heats of adsorption. However, the Freundlich model is not valid at high pressures and is typically applied to adsorption of solutes from liquid solutions onto solids.
Q7: How does dynamic equilibrium establish the Langmuir isotherm relationship?
Dynamic equilibrium occurs when the rate of molecules colliding with and adsorbing onto the surface equals the rate of desorption from occupied sites. At this point, there is no net change in surface coverage. Equating the adsorption and desorption rate expressions and solving yields the Langmuir isotherm, which mathematically relates surface coverage to gas phase pressure.