By J. P. O'Kane
This Festschrift containing 16 invited essays and papers is a tribute to the prestigious Irish hydrologist James Dooge at the party of his seventieth birthday. His former scholars, colleagues and acquaintances in fourteen international locations, have supplied a diverse choice on his favorite issues: circulation in open channels and unsaturated soil, and in addition from his significant curiosity of modern years, huge scale hydrology and worldwide change.
The ebook has 3 sections. the 1st part on hydrological approaches includes six papers. the second one part on huge scale hydrology has 4 papers. Six ancient, reflective and philosophical essays at the previous and way forward for the hydrological sciences shape the 3rd component to the booklet
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Extra info for Advances in Theoretical Hydrology. A Tribute to James Dooge
Horton Memorial Lecture, Annu. Meet. Am. Meteorol. , January, 1991. , 1986. The role of soil moisture in climate modelling. Final Project Report, EEC/NBST Project CLI-038-EIR(H). Centre for Water Resources Research, University College Dublin. 26 QJ. , 1952. The exact pattern of concentration dependent diffusion in a semi-infinite medium, Part II. Textile Res. , 22: 823-827. H. , 1911. Studies on soil physics, I. Flow of air and water through soils. J. Agric. , 4: 1-24. Haverkamp, R. , 1981. A comparative study of three forms of the Richard equation used for predicting one-dimensional infiltration in unsaturated soil.
T h e p a r a m e t e r k may be found using field measurements of z B( r ) or simple models of saturated flow to drains. A more detailed treatment requires a two-dimensional theory of saturated/unsaturated flow. 2. Surface boundary condition for infiltration of rain 3 2 of 1 rain into peat is a prescribed flux at ζ = 0 , T h e boundary condition for infiltration equal to the rainfall rate Q ( m m ~ s " ) : fx = = /M2 θ < 0 S at ζ = 0 (18) Vapour flux is not normally considered during infiltration.
XVIth General Assembly of European Geophysical Society, Wiesbaden, April, 1991. J. Hydrol. (submitted). 27 Chapter 3 The hydrology of milled peat production J. PHILIP O'KANE Abstract Dried peat is used as a fuel in a number of countries. Drawing on concepts in hydrology and soil physics we present a physically based theory of water movement in unsaturated peat. We apply the theory to the simulation of the drying of a layer of milled peat during a typical production period of four days. The control variables are: (1) the depth to the drained water table, (2) the depth of the milled layer, and (3) the timing and frequency of harrowing.