• Aucun résultat trouvé

Moisture Sorption Isotherms for Two Desiccants

N/A
N/A
Protected

Academic year: 2021

Partager "Moisture Sorption Isotherms for Two Desiccants"

Copied!
3
0
0

Texte intégral

(1)

Publisher’s version / Version de l'éditeur:

Technical Note (National Research Council of Canada. Division of Building Research), 1961-12-01

READ THESE TERMS AND CONDITIONS CAREFULLY BEFORE USING THIS WEBSITE.

https://nrc-publications.canada.ca/eng/copyright

Vous avez des questions? Nous pouvons vous aider. Pour communiquer directement avec un auteur, consultez la

première page de la revue dans laquelle son article a été publié afin de trouver ses coordonnées. Si vous n’arrivez pas à les repérer, communiquez avec nous à PublicationsArchive-ArchivesPublications@nrc-cnrc.gc.ca.

Questions? Contact the NRC Publications Archive team at

PublicationsArchive-ArchivesPublications@nrc-cnrc.gc.ca. If you wish to email the authors directly, please see the first page of the publication for their contact information.

NRC Publications Archive

Archives des publications du CNRC

For the publisher’s version, please access the DOI link below./ Pour consulter la version de l’éditeur, utilisez le lien DOI ci-dessous.

https://doi.org/10.4224/20358977

Access and use of this website and the material on it are subject to the Terms and Conditions set forth at

Moisture Sorption Isotherms for Two Desiccants

Hedlin, C. P.

https://publications-cnrc.canada.ca/fra/droits

L’accès à ce site Web et l’utilisation de son contenu sont assujettis aux conditions présentées dans le site LISEZ CES CONDITIONS ATTENTIVEMENT AVANT D’UTILISER CE SITE WEB.

NRC Publications Record / Notice d'Archives des publications de CNRC: https://nrc-publications.canada.ca/eng/view/object/?id=a6bc9e18-0279-4ffb-9e4b-617672a6d829 https://publications-cnrc.canada.ca/fra/voir/objet/?id=a6bc9e18-0279-4ffb-9e4b-617672a6d829

(2)

-

セMM

DIVISION OF BUILDING RESEARCH

NATIONAL RESEARCH COUNCIL OF CANADA

'fE

C

1HIN II CAlL

NOTlE

No.

354

NOT FOR PUBLICATION

PREPARED BY C. P. Hedlin CHECKED BY G. O. H.

FOR INTERNAL USE

APPROVED BY N. B. H.

DATE December 1961

PREPARED FOR Building Services Section, DBR/NRC

SUBJECT MOISTURE SORPTION ISOTHERMS FOR TWO DESICCANTS

One of the problems associated with studies on the per-formance of sealed, double-glazed window units is the interpretation of internal dew point measurement in relation to moisture gain to the

sealed space. One factor of interest in this regard is the equilibrium

moisture content vs dew point relationship for the desiccant involved.

In order to check the accuracy of published information, and to provide

additional data on the characteristics of one commonly used desiccant and one potentially usable material, a series of measurements were made using the special humidity facilities at Saskatoon.

Davison silica gel, Grade 408, mesh size 12-28, was obtained from the McArthur Chemical Company, Limited, and Type

l3X, 1/16-inch pellet, molecular sieve material was also procured for these tests.

Samples of both were dried to equilibrium in a vacuum oven

at 260 - 265"F. This treatment reduced the moisture content of the

silica gel received from the manufacturer by O. 5 to 0.6% (dry weight

basis).

Samples were weighed, exposed to air of known dew point

at 70of until they were substantially at equilibrium, then reweighed

to find the increase in moisture content. The "atmosphere producer"

and a controlled atmosphere chamber were used in these tests to provide the required air conditions.

Several moisture content - dew point values for silica gel, taken from the Chemical Engineers Handbook, third edition, page 912,

(3)

2

-are included in the attached Table. These values differ considerably

from our experimental values at low dew point temperatures. The

di screpancy cannot be entirely attributed to a difference in initial dryness because the absolute difference between the two sets of data

is substantially less at higher dew point temperatures. The Prairie

Regional Station values were all obtained by a process of 。、ウッイーエゥッョセ

Although adsorption values lie below desorption values, it seems unlikely that hysteresis would account for such large differences.

TABLE I

Dew Point Dry Bulb %Weight increase - dry basis

Temp. Temp.

Silica gel Molec. sieves

1

2

3

1

2

3

-20. 1

69.6

3.2

3.2

13.5

14.3

-12. 1

69.6

3.5

3.7

16.4

17.4

-10. 1

69.7

4. 1

4. 1

16.7

17.6

-0.2

69.4

5.7

5.6

17.6

18.6

+6.5

70. 1

7.2

7.2

7.2

19. 1

19. 1

19.2

+9.6

70. 1

7.3

7.4

7.4

19.2

19.2

19.3

+28.3

70.2

15. 1

15. 1

15.1

21. 1

21. 1

21. 1

+44.7

70. 1

24.2

23.8

23.8

22.4

22.4

Moistur e content - dew point values for silica gel, taken from the Chemical Engineers Handbook:

Dew Point Dry Bulb Temp.

0/0

Moisture content

dry basis

-60

70

6.

-30

70

7.

-10

70

8.2

7

70

10

25

70

14

41

70

23.5

59

70

37.3

Références

Documents relatifs

Statistical results (A) and description of plant growth response variables (B).. infiltration) of the experiment within the EUs located in sun and shaded coffee plantations. Table

À partir de données audiovisuelles, l’analyse comparative de deux situations de formation et des interactions tutorales auxquelles prennent part deux apprentis de première

PIP30 depletion induces accumulation of PA28 γ in residual CBs and enhances the interaction of PA28γ with coilin.. (A) PIP30 depletion induces PA28 γ accumulation

/ La version de cette publication peut être l’une des suivantes : la version prépublication de l’auteur, la version acceptée du manuscrit ou la version de l’éditeur. Access

Both mutants grew normally on 7H11 plates supplemented with anhydrotetracycline (ATc; 100 ng/ml for the M. bovis BCG mutant and 300 ng/ml for the M. tuberculosis mutant) but were

Thus, Markov Random Fields (MRF) whose usefulness is now obvious for projective image pro- cessing, can not be used directly on catadioptric images be- cause of the inadequacy of

The slope of the regression lines obtained for the joint movements versus temperature readings is the movement in inches per degree Fahrenheit change and is a