Abstract
1-D1H nuclear magnetic resonance profiles have been used to image the penetration of D2O into waterlogged archaeological wood. A series of well characterised plugs were sampled from different depths, reflecting different degrees of degradation and orientation with respect to the wood structure, of an oak timber from the Mary Rose. The ingress of D2O was Fickian in character and the diffusion coefficients,D, are reported as a function of depth into the timber for each orientation. The behaviour ofD could be approximated by a surface layer, with a higher diffusion coefficient, and a lower diffusion core region. The differences in the values ofD in the different orientations are rationalised in terms of the known structure of decayed wood. Theoretical uptake curves were calculated from a numerical evaluation of the analytical solution for diffusion into a multiple-layer model. Saturation of the surface layer was predicted to occur prior to diffusion into the core, with a characteristic change of gradient displayed in the uptake curve. Good agreement was achieved with experiments that sampled the different decay environments. Concentration distributions, and uptake curves, were calculated using these models for a typical archaeological timber.
Similar content being viewed by others
References
Grattan D.W., Clarke R.W.: Conservation of Marine Archaeological Objects (Pearson C., ed.), chap. 9. London: Butterworths 1987.
Barbour R.J.: Archaeological Wood: Properties, Chemistry, and Preservation (Rowell R.M., Barbour R.J., eds.), chap. 7. Washington: American Chemical Society 1990.
Christensen G.N., Williams E.J.: Aust. J. Appl. Sci.2, 411 (1951)
Christensen G.N.: Aust. J. Appl. Sci.2, 430 (1951)
Baines E.F., Levy J.F.: J. Inst. Wood Sci.8, 109 (1979)
Grattan D.W.: Conservation of Marine Archaeological Objects (Pearson C., ed.), chap. 3. London: Butterworths 1987.
Hoffmann P., Jones M.A.: Archaeological Wood: Properties Chemistry and Preservation (Rowell R.M., Barbour R.J., eds.), chap. 2. Washington: American Chemical Society 1990.
Wison A.T., Chang C.T.P.: Prog. Nucl. Magn. Reson. Spectrosc.31, 343 (1997)
Stilbs P.: Prog. Nucl. Magn. Reson. Spectrosc.19, 1 (1987)
Karger J., Pfeifer H., Heink W.: Adv. Magn. Reson.12, 1 (1988)
McDonald P.J., Pritchard T., Roberts S.P.: J. Colloid Interface Sci.177, 439 (1996)
Hughes P.D.M., McDonald P.J., Rhodes N.P., Rockcliffe J.W., Smith E.G., Wills J.: J. Colloid Interface Sci.177, 208 (1996)
Jane F.W.: The Structure of Wood, 2nd edn. London: A. & C. Black 1970.
Meylan B.A., Butterfield B.G.: Three Dimensional Structure of Wood: a Scanning Electron Microscope Study. London: Chapman & Hall 1972.
Butterfield B.G., Meylan B.A.: Three Dimensional Structure of Wood: an Ultrastructural Approach. London: Chapman & Hall 1980.
Crank J.: The Mathematics of Diffusion, 2nd edn., chap. 4. Oxford: Oxford University Press 1975.
Robertson M.B., Ward I.M., Klein P.G., Packer K.J.: Macromolecules30, 6893 (1997)
Mills R.: J. Phys. Chem.77, 685 (1973)
Barrie J.A., Levine J.D., Michaels A.S., Wong P.: Trans. Faraday Soc.59, 869 (1963)
Ash R., Baker R., Petropopoulos J.H.: Br. J. Appl. Phys.16, 854 (1963)
Ash R., Barrer R.M., Palmer D.G.: Br. J. Appl. Phys.16, 873 (1965)
Tittle C.W.: J. Appl. Phys.36, 1486 (1965)
Ozisik M.N.: Boundary Value Problems of Heat Conduction, 2nd edn., chap. 6. New York: Wiley 1993.
Fukuda M., Kawai H.: Polym. Eng. Sci.34, 330 (1994)
Fukuda M., Kawai H.: Polym. Eng. Sci.35, 709 (1995)
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Robertson, M.B., Packer, K.J. Diffusion of D2O in archaeological wood measured by 1-D NMR profiles. Appl. Magn. Reson. 17, 49–64 (1999). https://doi.org/10.1007/BF03162068
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF03162068