Geoscience Reference
In-Depth Information
(1945). Erosional development of streams and their drainage basins; hydrophysical approach to
quantitative morphology.
Geol. Soc. Amer. Bull.
,
56
, 275-370.
Hursh, C. R. (1936). Storm water and absorption.
Trans. Amer. Geophys. Un.
,
17
, 301-302.
(1944). Subsurface-flow.
Trans. AGU
,
25
, 743-746.
Jenkins, A., Ferrier, R. C., Harriman, R. and Ogunkoya, Y. O. (1994). A case study in catchment
hydrochemistry: conflicting interpretations from hydrological and chemical observations.
Hydrol
.
Processes
,
8
, 335-349.
Jones, A. (1971). Soilpiping and stream channel initiation.
Water Resour. Res.
,
7
, 602-610.
Klemes, V. (1986). Operational testing of hydrological simulation models.
Hydrological Sciences J.
,
31
, 13-24.
Leaney, F. W., Smettem, K. R. J. and Chittleborough, D. J. (1993). Estimating the contribution of
preferential flow to subsurface runoff from a hillslope using deuterium and chloride.
J. Hydrol.
,
147
, 83-103.
Liu, Y., Steenhuis, T. S. and Parlange, J.-Y. (1994a). Formation and persistence of fingered flow fields
in coarse grained soils under different moisture contents.
J. Hydrol.
,
159
, 187-195.
(1994b). Closed-form solution for finger width in sandy soils at different water contents.
Water
Resour. Res.
,
30
, 949-952.
Lowdermilk, W. C. (1934). The role of vegetation in erosion control and water conservation.
J. Forest.
,
32
, 529-536.
Marui,A. (1991). Rainfall-runoff process and function of subsurface water storage in a layered
hillslope.
Geograph
.
Review Japan
,
64
, 145-166.
Masiyandima, M. C., VandeGiesen, N.,Diatta, S.,Windmeijer, P. N. and Steenhuis, T. S. (2003). The
hydrology of inland valleys in the sub-humid zone of West Africa: rainfall-runoff processes in
the M'be experimental watershed.
Hydrol. Processes
,
17
, 1213-1225.
McDonnell, J. J. (1990). A rationale for old water discharge through macropores in a steep, humid
catchment.
Water Resour. Res.
,
26
, 2821-2832.
McDonnell, J. J., Stewart, M. K. and Owens, I. F. (1991a). Effect of catchment-scale subsurface mixing
on stream isotopic response.
Water Resour. Res.
,
27
, 3065-3073.
McDonnell, J. J., Owens, I. F. and Stewart, M. K. (1991b). A case study of shallow flow paths in a steep
zero-order basin.
Water Resour. Bull.
,
27
, 679-685.
McGlynn, B. L., McDonnell, J. J. and Brammer, D. D. (2002). Areview of the evolving perceptual
model of hillslope flowpaths at the Maimai catchments, New Zealand.
J. Hydrol.
,
257
, 1-26.
Morton, A. (1993). Mathematical models: questions and trustworthiness.
Brit. J. Philos. Sci.
,
44
,
659-674.
Mosley, M. P. (1979). Streamflow generation in a forested watershed, New Zealand.
Water Resour.
Res.
,
15
, 795-806.
Mulvany, T. J. (1850). On the use of self registering rain and flood gauges.
Inst. Civ. Eng. Proc.
(Dublin)
,
4
(2), 1-8.
Newman, B. D., Campbell, A. R. and Wilcox, B. P. (1998). Lateral subsurface flow pathways ina
semiarid ponderosa pine hillslope.
Water Resour. Res.
,
34
, 3485-3496.
Noguchi,S., Tsuboyama, Y.,Sidle, R. C. and Hosoda, I. (1999). Morphological characteristics of
macropores and the distribution of preferential flow pathways in a forested slope segment.
Soil
Sci. Soc. Amer. J.
,
63
, 1413-1423.
Novakowsky, K. W. and Gillham, R. W. (1988). Field investigations of the nature of water-table
response to precipitation in shallow water-table environments.
J. Hydrol.
,
97
, 23-32.
Onodera, S. (1991). Subsurface water flow in the multi-layered hillslope.
Geograph
.
Review Japan
,
64
(Ser. A), 549-568.