双语化学辞典Chem Lexicon
概念 · 表面化学 · 吸附 Surface chemistry · Adsorption

物理吸附Physisorption

拼音Pinyin wù lǐ xī fù 别名Also 范德华吸附;physical adsorption; van der Waals adsorption

定义Definition

物理吸附是吸附质分子与吸附剂表面之间仅依靠范德华力(主要是色散力)发生的吸附,不形成化学键。它吸附热小、速度快、可逆、无选择性,可形成多分子层。

Physisorption is adsorption held only by van der Waals forces, mainly dispersion, between adsorbate and surface, with no chemical bond formed. It has a small heat of adsorption, is fast, reversible and non-selective, and can build up multiple layers.

特征Characteristics

吸附热一般为 5–40 kJ/mol,与吸附质的液化热相近;不需要活化能,几乎瞬间达到平衡;降低压力或升高温度即可脱附,吸附质分子结构不变;任何气体在任何固体表面都会发生物理吸附,越易液化的气体(沸点越高)吸附量越大;低温下吸附量大,可在单层之上继续吸附形成多层。

Heats of adsorption are typically 5–40 kJ/mol, close to the heat of liquefaction; no activation energy is needed, so equilibrium is reached almost instantly; lowering the pressure or raising the temperature desorbs the adsorbate unchanged; every gas physisorbs on every solid, and gases that liquefy more easily (higher boiling points) adsorb more; uptake is large at low temperature and can continue beyond a monolayer into multilayers.

应用:表面积与孔结构测定Use: surface area and porosity

77 K 下氮气在固体表面的物理吸附是测定比表面积(BET 法)和孔径分布(BJH 法、密度泛函法)的标准方法。IUPAC 把吸附等温线分为六类(I–VI 型),I 型对应微孔材料,IV 型带滞后环对应介孔材料。活性炭比表面积可达 1000–3000 m²/g,某些金属有机框架超过 7000 m²/g。

Nitrogen physisorption at 77 K is the standard method for specific surface area (BET) and pore-size distribution (BJH and density-functional methods). IUPAC classifies isotherms into six types, I to VI: type I indicates micropores and type IV, with a hysteresis loop, mesopores. Activated carbon reaches 1000–3000 m²/g, and some metal–organic frameworks exceed 7000 m²/g.

其他应用Other uses

物理吸附用于活性炭除味脱色、硅胶和分子筛干燥、变压吸附分离空气(沸石分子筛优先吸附 N₂ 制氧)、储存甲烷和氢气,以及气相色谱的固定相分离。

Physisorption is used for odour and colour removal with activated carbon, drying with silica gel and molecular sieves, air separation by pressure-swing adsorption (zeolites preferentially take up N₂ to give oxygen), methane and hydrogen storage, and separation on gas-chromatography stationary phases.

年表Timeline

  • 1938

    BET 理论用于表面积测定

    BET theory is applied to surface-area measurement

  • 1951

    BJH 孔径分析方法提出

    The BJH pore-analysis method is proposed

  • 1985

    IUPAC 发布吸附等温线分类

    IUPAC publishes its isotherm classification

相关公式Formulas

BET 多层吸附等温式 BET isotherm→
\[\frac{p}{V(p_0 - p)} = \frac{1}{V_mc} + \frac{c - 1}{V_mc}\cdot\frac{p}{p_0},\qquad S = \frac{V_mN_A\sigma}{V_\text{mol}}\]
例题Worked example

若 V_m = 100 cm³(STP)/g:S = 100/22414 × 6.022×10²³ × 0.162×10⁻¹⁸ m² ≈ 435 m²/g。

V_m = 100 cm³(STP)/g gives S ≈ 435 m²/g.