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Microporosity in carbon blacks

a ,

*

b a a

F. Stoeckli , A. Guillot , A.M. Slasli , D. Hugi-Cleary

aChemistry Department of the University, Avenue de Bellevaux 51, CH-2007 Neuchatel, Switzerlandˆ

bCNRS-IMP, Universite de Perpignan, Avenue de Villeneuve, F-66806 Perpignan, France´

Abstract

Microporous carbon blacks can be characterized by the same techniques as activated carbons, using the classical DR equation and comparison plots based on non-porous materials. The CO2 adsorption isotherm at 273 K, combined with computer modelling, also leads to an assessment of microporosity. The results agree with independent techniques such as immersion calorimetry into liquids of variable molecular dimensions and a modified Dubinin equation. The study also confirms that the comparison plots based on N2 (77 K), CO2 (273 K) and C H6 6 (293 K) do not necessarily lead to overlapping results for the total micropore volume and the external surface area of the carbons.

Keywords: A. Carbon black; C. Adsorption, Modelling; D. Porosity

1. Introduction progress has been made. This includes the use of other

vapours such as benzene at 293 K [14] and, more recently, Carbon blacks [1] and activated carbons [2] both contain of CO between 253 and 353 K and at pressures up to 52 graphitic sheets as building blocks, the difference being the MPa [15–18]. Like CH4 [9], CO2 is a relatively simple extent of order. In the case of carbon blacks, high molecule and its adsorption isotherm can be modelled by temperature treatments may also improve the graphitic computer simulations [19–23].

structure. On the other hand, activated carbons will remain The present study re-examines the assessment of mi- disordered, the extent of the graphitic domains being croporosity in carbon blacks, as described earlier [24–27]

limited to approximately 2–3 nm and 2–4 layers. These and based on comparison plots, isotherms, immersion structural similarities are sufficient to ensure, locally at calorimetry into liquids of variable molecular dimensions least, similarities in the microporosity of the two types of and on differential heats of adsorption. As a novelty, we carbons. It has been shown by the dark-field technique include the use CO isotherms at 273 K and pressures up2 developed by Oberlin et al. [3–5] and, more recently by to 3 MPa, as well as the recent reference isotherm on STM [6–9], that the micropores of activated carbons are Vulcan 3-G [26]. The CO2 isotherms are also analysed locally slit-shaped, at least up to a width of 1 nm. The with the help of model isotherms resulting from computer micropore system may therefore be regarded as a three- simulations, which leads to the corresponding micropore dimensional collection of interconnected slits, the differ- distributions [9,23].

ence with carbon blacks being, to a first approximation, the extent of regularity.

The microporosity of carbon blacks and of other materi- 2. Theoretical background als can be assessed by techniques such as neutron or X-ray

scattering, but it appears that the classical techniques are Adsorption of vapours by microporous carbons is de- still appropriate for a reasonable characterization. Since the scribed by Dubinin’s theory [2,28–30] and its fundamental introduction of the method based on nitrogen comparison equation is the so-called Dubinin–Astakhov equation,

plots by de Boer [10,11] and later by Sing [12,13], n

Na5Naoexp[2(A /E ) ] (1)

N represents the amount adsorbed at relative pressure

* Corresponding author. Fax: 141-32-718-2511. a

E-mail address: fritz.stoeckli@unine.ch (F. Stoeckli). p /p , Ns aois the limiting amount filling the micropores and

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A5RT ln( p /p). At high pressures, the ratio p /p iss s where Nam(DRK) represents the limiting amount adsorbed in the monolayer. Fig. 1 illustrates the case of C H , CCl ,

replaced by the ratio of the fugacities and for temperatures 6 6 4

CH Cl and N adsorbed on carbon black Hoechst [27].

above critical, the saturation pressure is replaced by p (T /c 2 2 2

2 As discussed elsewhere [14,26], N (DRK) is somewhat

T ) [28]. The case where nc 52 corresponds the Dubinin– am

larger than N (BET), but no explanation can be offered Radushkevich equation (DR). Eq. (1) reflects the filling of am

for this difference.

a volume Wo5N V , where V is the molar volume of theao m m

For carbon black Hoechst, benzene leads to a charac- adsorbate. It is similar to that of the liquid at the same

21 21

teristic energy E of 10.8 kJ mol , against 10.4 kJ mol temperature, but not necessarily equal to it, as in the case o

for Vulcan3G and 11.4 kJ mol21 for N-234G, another of CO2 discussed below. The characteristic energy, E,

graphitised carbon black. Lower values, around 9.4–9.8 kJ depends on the adsorbent and on the adsorptive. One may

mol21, have also been reported [14], which confirms that write that E5bE , whereo b depends on the adsorptive

Dubinin’s theory applies to porous and non-porous carbon and by convention, b(C H )51. It has been shown6 6

blacks, but in different domains of p /p .

[30,31] that E is related to the average width L of theo o s

Values of E around 10–11 kJ mol21 are close to the

slit-shaped micropores by o

lower bound of 11.4 kJ mol21 found in the empirical L (nm)o 510.8 /(Eo211.4 kJ mol21) (2) relation (2) and correspond to very wide micropores. It follows that the value of E provides a first indication foro The approximate surface area of these pores is given by the presence or the absence of microporosity in unknown the simple geometrical relation carbons, including carbon blacks. Typical micropores correspond to Eo.18–20 kJ mol21, whereas values below

2 21 3 21

Smi(m g )52000 W (cm go ) /L (nm)o (3) 14–15 kJ mol21reflect either variable degrees of surface heterogeneity, or the presence of super-micropores (1.5–

The total surface area of the carbon Stot5Smi1S ,e 2.5 nm). For such carbons, no molecular sieve effects are where S is the external surface. Se totcan be compared with observed by immersion calorimetry and the characteriza- the area obtained from immersion calorimetry into aqueous tion of their porosity becomes difficult.

solutions of caffeine [30,32] or phenol [33] provided, in Computer modelling of adsorption has become increas- the latter case, that the surface does not contain too much ingly popular and it has been applied to the determination oxygen. These molecules are adsorbed preferentially as of pore-size distributions in carbons. A number of studies monolayers with specific enthalpies of approximately are based on the adsorption of simple molecules such as 20.115 and 20.110 J m22. CH [9,37] and CO [9,20–23]. In this approach, standard4 2 As discussed elsewhere [30,31,34], the following micro- isotherms are modelled for sets of slit-shaped pores

pore distribution between 0.4 and 1.5–2 nm and the experimental isotherm

( 3n 21 ) n 3

f(L )53 W Lo a exp[2aL ] /G(n) (4) can be associated with a modified Dubinin equation

3 n

u(A)5N /Na ao5[a /(a1(A /bK ) )]o (5)

wheren and a are adjustable parameters and Ko5L E ,o o as confirmed by direct curve fitting.

A thermodynamic consequence of the DR equation is the following expression for the enthalpy of immersion of the carbon into the corresponding liquids [2,5,30],

21 1 / 2

DiH (J g )5 2bE W (1o o 1aT )p / 2 Vm1h Si e (6)

where h S represents the wetting of the external surface ofi e the solid. The enthalpies of immersion into liquids of variable molecular dimensions can also be used to assess the micropore distribution of carbons between 0.4 and 1.5 nm [30,31], as illustrated below.

It has been shown [27] that adsorption of different

vapours by non-porous carbon blacks follows the so-called Fig. 1. Logarithmic DRK plot for the adsorption of different DRK equation suggested by Kaganer [35,36] vapours on C black Hoechst: C H at 282 K (6 6 n), 293 K (m), 311 K (h) and 323 K (j); CCl4 at 294 K (d) and 305 K (s);

Na5Nam(DRK) exp[2(A /bE ) ]o2 (7) CH Cl at 293 K (1) and N at 77 K (32 2 2 ).

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is described in terms of a weighted contribution of these the corresponding structural parameters are given in Table isotherms. From a practical point of view, a good choice 1.

seems to be CO at 273 K, where full isotherms can be2 obtained with high-pressure equipment [16–18]. Standard CO isotherms for adsorption in slit-shaped micropores at2

273 K have recently been obtained by the authors, as 4. Results and discussion described elsewhere [9,23].

Fig. 2 shows the combined data for CO (253, 273 and2 298 K) and C H6 6 (298 K) adsorbed on carbon black

3. Experimental XC-72. With Eo522.4 kJ mol21 and b(CO )50.352

[23,26], one obtains a single DR plot. The molar volume of We considered two typical microporous carbon blacks, CO2 is still a matter of debate [15–17,23] and various XC-72 [24,26] and XC-72-16, the product of its activation expressions have been proposed to calculate it [28,38]. For

3 21

by water vapour at 9508C [23]. For comparison purposes, the different carbons, the values of 42.90 cm mol at we also included three active carbons, CAF-B, U-103 and 273 K, given by Ozawa’s equation [38], lead to micropore KF-1500 [18,26], with average micropore sizes of 0.65, volumes W (CO ; 273 K), which are in good agreemento 2 1.15 and 1.38 nm, respectively. These solids had been with those suggested by other adsorbates (see Table 1).

subjected to the same type of analysis [9,18,23] as the Comparison plots with non-porous references like Vulcan carbon blacks used here. 3G or Hoechst, lead to the micropore volumes and external

The adsorption and immersion techniques used to surfaces given in Table 1.

characterize these samples, in particular with CO at 2732 The structural parameters obtained by the different K, have been described in detail elsewhere [1,18,30] and techniques, summarized in Table 1, show clearly the limits

Table 1

Main characteristics of microporous carbon blacks XC-72 and XC-72-16 and of activated carbons CAF-B, U-103 and KF-1500

Sample XC-72 XC-72-16 CAF-B U-103 KF-1500

DR analysis

E (kJ molo 21) C H / N6 6 2 22.4 21.3 28.3 20.7 19.1

E (kJ mol21) CO2 8.6 7.5 10.1 7.7 6.4

L (nm) (DR average)o 0.96 1.08 0.65 1.15 1.38

2 21

Smi (m g ) (average) 145 259 856 631 918

3 21

W (cm go ) C H6 6 0.057 0.130 0.266 0.330 0.580

3 21

W (cm go ) CO2 0.070 0.150 0.274 0.360 0.620

Modelling (CO ; 273 K)2

L (nm) (DR average)o 1.01 1.22 0.75 1.28 1.46

3 21

W (cm go ) C H6 6 0.070 0.155 0.280 0.400 0.66

Comparison plot

3 21

W (cm go ) C H6 6 0.041 0.180 0.30 0.35 0.60

3 21

W (cm go ) CO2 0.075 0.147 0.27 0.38 0.60

3 21

W (cm go ) N2 0.052 2 0.28 0.35 0.63

3 21

W (cm go ) average 0.061 0.152 0.28 0.36 0.61

Comparison plot

2 21

S (m ge ) C H6 6 137 117 32 27 28

2 21

S (m ge ) CO2 75 108 44 19 19

2 21

S (m ge ) N2 103 2 97 70 22

CalorimetryDH (C H )i 6 6 2 21

S (m ge ) 106 139 70 40 14

2 21

S (m ge ) average 105 119 60 39 21

2 21

Stot(m g )5Smi1Se 250 380 916 670 939

2 21

Stot(phenol) (m g ) 257 460 2 2 1167

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Fig. 2. DR plot for adsorption of CO at 253, 273 and 298 K and2

C H at 293 K on carbon black XC-72 (E6 6 o522.4 kJ mol21).

for the characterization of carbons. It appears that a single determination may not be sufficient and the average values obtained for W , So e and Stot give an estimate of the uncertainties resulting from different adsorbates and tech- niques.

After correcting for adsorption on the external surfaces

2 21

S (75 and 108 m ge ) by using the reference isotherm on Vulcan 3G [26], the CO isotherms at 273 K were fitted to2 a weighted contribution of the model isotherms obtained by Monte Carlo simulations, as described previously

[9,23]. The corresponding micropore volumes are close to Fig. 3. Micropore distributions in carbon blacks XC-72 (a) and those obtained by other techniques (DR and comparison XC-72-16 (b) obtained from the analysis of the CO isotherm at2

plots). 273 K based on model isotherms (——), from immersion

As seen in Fig. 3(a) and (b), the normalized pore size calorimetry with liquids of different molecular dimensions (– –) and from Eq. (4) (curve).

distributions for CO (273 K) are in good agreement with2 those obtained from immersion calorimetry [21,22,26] and from Eq. (4). The CO2 histograms lead to average

micropore widths Lo of 1.01 and 1.22 nm, in good 3–3.5 MPa offers a number of advantages. Firstly, a agreement with the values obtained from the DR analysis reliable standard CO2 isotherm is now available for (0.96 and 1.08 nm), using Eq. (2). In the case of carbon comparison plots, in order to establish the presence or the blacks XC-72 and XC-72-16, the histograms and the absence of microporosity in carbonaceous materials. Sec- analysis of the different isotherms with the help of Eqs. (2) ondly, for a finer characterization of the porosity, the and (3) suggest total surface areas of approximately 250 adsorption isotherm can also be used in connection with

2 21

and 380 m g . On the other hand, immersion calorimetry adsorption calorimetry into liquids of different molecular into aqueous solutions of phenol, leads to areas of 257 and dimensions. Finally, micropore distributions can also be

2 21

460 m g . The uncertainties being around 5–10% in derived from this isotherm with the help of model iso- both techniques, the agreement is satisfactory. therms based on computer simulations.

In conclusion, this study shows that it is possible to characterize microporous carbon blacks with the same standard adsorption and calorimetric techniques as acti-

References vated carbons. In the last analysis, this is due to the fact

that both types of solids can be treated as collections of

[1] Donnet JB, Bansal RC, Wang MJ. In: Carbon black, New locally slit-shaped micropores, carbon blacks being closer

York: Marcel Dekker, 1993.

to the ideal model. However, in both cases, reliable [2] Bansal RC, Donnet JB, Stoeckli F. In: Active carbon, New characterization still requires the determination of an York: Marcel Dekker, 1988.

adsorption isotherm and the use of a suitable reference. [3] Oberlin A, Terriere` G, Boulmier JL. J Microscop The choice of adsorptive may also be of great help and it 1974;21:301–8.

appears that the use of CO at 273 K and at pressures up to2 [4] Oberlin A, Terriere G, Boulmier JL. Tanso 1975;80:29–42.`

(5)

[5] Stoeckli F. Carbon 1990;28:1–6. [22] Ravikovitch PI, Vishnyakov A, Russo R, Neimark V. Lang- [6] Donnet JB, Papirer E, Wang W, Stoeckli F. Carbon muir 2000;16:2311–30.

1994;32:183–4. [23] Stoeckli F, Guillot A, Slasli AM, Hugi-Cleary D. Carbon

[7] Daley MA, Tandon D, Economy J, Hippo EJ. Carbon 2001;39:in press.

1996;34:1191–2000. [24] Stoeckli F, Huguenin D, Laederach A. Chimia 1993;47:211–

[8] Stoeckli F, Hugi-Cleary D, Centeno TA. J Eur Ceram Soc 2.

1998;18:1177–86. [25] Stoeckli F, Huguenin D, Laederach A. Carbon

[9] Stoeckli F, Guillot A, Hugi-Cleary D, Slasli A. Carbon 1994;32:1359–62.

2000;38:938–41. [26] Guillot A, Stoeckli F. Carbon 2001;39:in press.

[10] Lippens BC, De Boer JH. J Catal 1965;4:319–23. [27] Hugi-Cleary D, Stoeckli F. Carbon 2000;38:1309–13.

[11] De Boer JH, Linsen BG, van der Plas T, Zondervan GJ. J [28] Dubinin MM. In: Cadenhead DA, editor, Progress in surface

Catal 1965;4:649–53. and membrane science, New York: Academic Press, 1975,

[12] Gregg JS, Sing KSW. In: Adsorption, surface area and pp. 1–70.

porosity, London: Academic Press, 1982, pp. 90–110. [29] Dubinin MM. Carbon 1985;23:373–80.

[13] Carrott PJM, Roberts RA, Sing KSW. Carbon 1987;25:59– [30] Stoeckli F. In: Patrick J, editor, Porosity in carbons —

68. characterization and applications, London: Arnold, 1995, pp.

[14] Carrott PJM, Ribeiro Carrott MML, Cansado IPP, Nabais 67–92.

JMV. Carbon 2000;38:465–74. [31] Stoeckli F, Rebstein P, Ballerini L. Carbon 1990;28:907–9.

´ ´ `

[15] Marcilla-Gomis A, Garcia-Cortes AN, Martı n-Martı nez JM. [32] Stoeckli F, Fragniere M, Huguenin D, Depraz M, Ballerini L.

Carbon 1996;34:1531–8. Carbon 1989;26:915–6.

˜

´ ´ ´

[16] Cazorla-Amoros D, Alcaniz-Monge J, Linares-Solano A. [33] Stoeckli F, Lopez-Ramon V, Moreno-Castilla C. Langmuir

Langmuir 1996;12:2820–4. 2001:3301–6.

˜

[17] Cazorla-Amoros D, Alcaniz-Monge de la Casa-Lillo, [34] Stoeckli F. Carbon 1990;27:962–4.

Linares-Solano A. Langmuir 1988;14:4589–96. [35] Rudzinski W, Everett DH. In: Adsorption of gases on [18] Guillot A, Stoeckli F, Bauguil Y. Adsorp Sci Technol heterogeneous surfaces, New York: Academic Press, 1992,

2000;18:1–14. pp. 42–51.

[19] Samios S, Stubos AK, Kanellopoulos NK, Cracknell RF, [36] Kaganer GM. Dokl Akad Nauk SSSR 1952;116:603–7.

´ ´

Papadopoulos GK, Nicholson D. Langmuir 1997;13:2795– [37] Lopez-Ramon V, Jagiello J, Bandosz TJ, Seaton NA. Lang-

802. muir 1997;13:4435–45.

[20] Jagiello J, Schwarz JA. Langmuir 1993;9:2513–7. [38] Ozawa S, Kusimi S, Ogino Y. J Colloid Interf Sci [21] Vishnyakov A, Ravikovitch PI, Neimark V. Lanmguir 1976;56:83–5.

1999;15:8736–42.

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