Abdul, A.S. And R.W. Gillham, 1984. Laboratory studies of the effects of the capillary fringe on streamflow generation. Water Resour. Res., 20: 691-698.
Anderson, M.G. and T.P. Burt. 1978. The role of topography in controlling throughflow generation. Earth-Surface Processes, 3(4): 331-344.
Bergstrom, S., Carolsson, B., Sandberg, G. and Maxe, L., 1985. Integrated modeling of runoff, alkalinity, and pH on a daily basis. Nordic Hydrology, 16: 89-104.
Blowes, D.W. and Gillham, R.W., 1988. The generation and quality of streamflow on inactive uranium tailings near Elliot Lake, Ontario. Jour. of Hydrol., 97: 1-22.
Bonell, M., Pearce, A.J. and Stewart, M.K. 1990. The identification of runoff-production mechanisms using environmental isotopes in a tussock grassland catchment, eastern Otago, New Zealand. Hydrological Processes, 4: 15-34.
Bottomley, D.J., Craig, D. and Johnston, L.M., 1984. Neutralization of acid runoff by groundwater discharge to streams in Canadian Precambrian Shield watersheds. Jour. of Hydrol., 75: 1-26.
Brown, G., McDonnell, J.J., Burns, D. and Kendall, C., 1998. The role of event water, rapid shallow flowpaths and catchment size in summer stormflow. Jour. of Hydrol., in press.
Christopersen, N. and Wright, R.F., 1981. Sulfate budget and a model for sulfate concentrations in streamwater at Birkenes, a small forested catchment in southernmost Norway. Water Resour. Res., 17: 377-389.
Christophersen, N., Seip, H.M. and Wright, R.F., 1982. A model for streamwater chemistry at Birkenes, Norway. Water Resour. Res., 18: 977-996.
Christophersen, N., Kjaernsroed, S. and Rodhe, A., 1985. Preliminary evaluation of flow patterns in the Birkenes catchment using natural 18O as a tracer. Hydrological and Hydrogeochemical Mechanisms and Model Approaches to the Acidification of Ecological Systems, Report 10, Nordic Hydrological Programme, Oslo, Norway, pp. 29-40.
Clothier, B.E. and R.A. Wooding. 1983. The soil diffusivity near saturation. Soil Science Society of America Journal. 47: 636-640.
Crouzet, E., Hubert, P, Olive, Ph. and Siweritz, E., 1970. Le tritium dans les mesures d'hydrologie de surface. Détermination expérimentale du coefficient de ruissellement. Jour. of Hydrol., 11: 217-219.
de Grosbois, E., Hooper, R.P. and Christophersen, N., 1988. A multisignal calibration methodology for hydrochemical models: A case study of the Birkenes model. Water Resour. Res., 24: 1299-1307.
DeWalle, D.R., Swistock, B.R. and Sharpe, W.E., 1988. Three component tracer model for stormflow on a small Appalachian forested catchment. Jour. of Hydrol., 104: 301-310.
Dinçer, T., and Davis, G.H., 1984. Application of environmental isotope tracers to modeling in hydrology. Jour. of Hydrol., 68: 95-113.
Durand, P., Neal, M. and Neal, C., 1993. Variations in stable oxygen isotope and solute concentrations in small submediterranean montane streams. Jour. of Hydrol., 144: 283-290.
Freeze, R.A., 1972. Role of subsurface flow in generating surface runoff, 2. Upstream source areas. Water Resour. Res., 8: 1272-1283.
Fritz, P.J., Cherry, A., Weyer, K.U. and Sklash, M., 1976. Storm runoff analyses using environmental isotopes and major ions. In: Interpretation of Environmental Isotope and Hydrochemical Data in Groundwater Hydrology, IAEA, Vienna, Austria, pp. 111-130.
Genereux, D.P., 1998. Quantifying uncertainty in tracer-based hydrograph separations. Water Resour. Res., 34: 915-920.
Genereux, D.P. and Hemond, H.F., 1990a. Naturally-occurring radon-222 as a tracer for streamflow generation: Steady-state methodology and field example. Water Resour. Res., 26(12): 3065-3075.
Genereux, D.P. and Hemond, H.F., 1990b. Three-component tracer model for stormflow on a small Appalachian forested catchment: Comment. Jour. of Hydrol., 117: 377-380 (with corrigendum, 1991, Jour. of Hydrol., 122: 429).
Genereux, D.P., Hemond, H.F. and P.J. Mulholland, 1993. Use of radon-222 and calcium as tracers in a three-end-member mixing model for streamflow generation on the West Fork of Walker Branch Watershed. Jour. of Hydrol., 142: 167-211.
Harr, R.D., 1977. Water flux in soil and subsoil on a steep forested slope. Jour. of Hydrol., 33: 37- 58.
Harris, D., McDonnell, J. and Rodhe, A., 1995. Hydrograph separation using continuous open system isotope mixing. Water Resour. Res., 31(1): 157-171.
Herrmann, A., Koll, J. Schöniger, M. and Stichler, W., 1987. A runoff formation concept to model water pathways in forested basins. IAHS Publication, 167: 251-263.
Hewlett, J.D. and A.R. Hibbert. 1963. Moisture and energy conditions within a sloping soil mass during drainage. Jour. Geophys. Res. 68: 1081-1087.
Hooper, R.P., Aulenbach, B., Burns, D., McDonnell, J.J., Freer, J., Kendall, C. and Beven, K., 1998. Riparian control of streamwater chemistry: Implications for hydrochemical basin models. IAHS, Publ. No. 248, pp. 451-458.
Hooper, R.P. and Shoemaker, C.A., 1986. A comparison of chemical and isotopic hydrograph separation. Water Resour. Res., 22(10): 1444-1454.
Hooper, R.P., Stone, A., Christophersen, N., de Grosbois, E. and Seip, H.M., 1988. Assessing the Birkenes model of stream acidification using a multisignal calibration methodology. Water Resour. Res., 24: 1308-1316.
Hoover, M.D., and C.R. Hursh. 1943. Influence of topography and soil depth on runoff from forest land. Transactions of the American Geophysical Union. 24: 693-698.
Hursh, C.R., 1936. Storm-water and absorption. Transactions of the American Geophysical Union. 17: 301-302.
Hursh, C.R. and Brater, E.F., 1941. Separating storm hydrographs from small drainage areas into surface and subsurface flow. Transactions of the American Geophysical Union. 22: 863-871.
Jordan, J.P., 1994. Spatial and temporal variability of stormflow generation processes on a Swiss catchment. Jour. of Hydrol., 153: 357-382.
Kendall, C., 1993. Impact of isotopic heterogeneity in shallow systems on stormflow generation. Ph.D. dissertation, University of Maryland, College Park, 310 p.
Kennedy, V.C., Kendall, C., Zellweger, G.W., Wyerman, T.A. and Avanzino, R.J., 1986. Determination of the components of stormflow using water chemistry and environmental isotopes, Mattole River basin, California. Jour. of Hydrol., 84: 107-140.
Kline, S.J., 1985. The purposes of uncertainty analysis. Journal of Fluids Engineering, 107: 153-160.
Kleissen, F.M., Beck, M.B. and Wheater, H.S., 1990. The identifiability of conceptual hydrochemical models. Water Resour. Res., 26: 2979-2992.
Lindstrom, G. and Rodhe, A., 1986. Modeling water exchange and transit times in till basins using oxygen-18. Nordic Hydrology, 17: 325-334.
Matsuo, S. and Irving Friedman. 1967. Deuterium content in fractionally collected rainwater. Jour. Geophys. Res., 72(24): 6374-6376.
McDonnell, J., Bonell, M., Stewart, M.K. and Pearce, A.J., 1990. Deuterium variations in storm rainfall: Implications for stream hydrograph separation. Water Resour. Res., 26(3): 455-458.
McDonnell, J., 1990. A rationale for old water discharge through macropores in a steep, humid catchment. Water Resour. Res., 26(11): 2821-2832.
McDonnell, J.J., Rowe, L. and Stewart, M.K., 1998. A combined tracer-hydrometric approach to assessing the effect of catchment scale on water flowpaths, source and age. IAHS Publ., in press.
McDonnell, J., Stewart, M.K. and Owens, I.F., 1991. Effect of catchment-scale subsurface mixing on stream isotopic response. Water Resour. Res., 27(12): 3065-3073.
Merot, P., Bourguet, M. and le Leuch, M., 1981. Analyse d'une crue à l'aide du traçage naturel par l'oxygène 18 mesuré dans les pluies, le sol, le ruisseau. Catena, 8: 69-81.
Mook, W.G., Groeneveld, D.J., Bouwn, A.E. and Van Gansurjk, A.J., 1974. Analysis of a runoff hydrograph by means of natural oxygen-18. In: Proceedings of the Symposium on Isotope Techniques in Groundwater Hydrology, 1, IAEA, Vienna, Austria, pp. 145-153.
Mosely, M.P., 1979. Streamflow generation in a forested watershed, New Zealand. Water Resour. Res., 15(4): 795-806.
Mulholland, P.J., 1993. Hydrometric and stream chemistry evidence of three storm flowpaths in Walker Branch Watershed. Jour. of Hydrol., 151: 291-316.
Neal, C., Neal, M., Warrington, A., Avila, A., Pinol, J. and Roda, F., 1992. Stable hydrogen and oxygen isotope studies of rainfall and streamwaters for two contrasting holm oamk areas of Catalonia, northeastern Spain. Jour. of Hydrol., 140: 163-178.
Neal, C. and Roiser, P.T.W., 1990. Chemical studies of chloride and stable oxygen isotopes in two conifer afforested and moorland sites in the British Uplands. Jour. of Hydrol., 115: 269-283.
Nolan, K.M. and Hill, B.R., 1990. Storm runoff generation in the Permanente Creek drainage basin, west central California: An example of flood-wave effects on runoff composition. Jour. of Hydrol., 113: 343-367.
O'Gunkoya, O.O. and Jenkins, A., 1991. Analysis of runoff pathways and flow contributions using deuterium and storm chemistry. Hydrological Processes, 5: 309-320.
Obradovic, M.M. and M.J. Sklash, 1986. An isotopic and geochemical study of snowmelt runoff in a small Arctic watershed. Hydrologic Processes. 1(1): 15-30.
Pearce, A.J., 1990. Streamflow generation processes: An Austral view. Water Resour. Res., 26: 3037-3047.
Pearce, A.J., Stewart, M.K. and Sklash, M.G., 1986. Storm runoff generation in humid headwater catchments: 1. Where does the water come from? Water Resour. Res., 22(8): 1263-1272.
Perroux, K.M., Raats, P.A.C. and D.E. Smiles, 1982.Wetting moisture characteristic curves derived from constant-rate infiltration into thin soil samples. Soil Science Society of America Journal, 46: 231-234.
Pionke, H.B. and DeWalle, D.R., 1992. Intra- and inter-storm 18O trends for selected rainstorms in Pennsylvania. Jour. of Hydrol., 138: 131-143.
Rodhe, A., 1987. Groundwater contribution to stream flow in Swedish forested till soil as estimated by oxygen-18. In: Isotope Hydrology, Proceedings of the IAEA Symposium, Vienna, Austria, pp. 55-66.
Roessel, B.W.P., 1950. Hydrologic problems concerning the runoff in headwater regions. Transactions of the American Geophysical Union 31(3): 431-442.
Rose, S., 1993. Environmental tritium systematics of baseflow in Piedmont Province watersheds, Georgia (USA). Jour. of Hydrol., 143: 191-216.
Rose, S., 1996. Temporal environmental isotopic variation within the Falling Creek (Georgia) watershed: Implications for contributions to streamflow. Jour. of Hydrol., 174: 243-261.
Sklash, M.G., Farvolden, R.N. and Fritz, P., 1976. A conceptual model of watershed response to rainfall, developed through the use of oxygen-18 as a natural tracer. Canadian Journal of Earth Science, 13: 271-283.
Sklash, M.G. and Farvolden, R.N., 1979. The role of groundwater in storm runoff. Jour. of Hydrol., 43: 45-65.
Sklash, M.G., Stewart, M.K. and Pearce, A.J., 1986. Storm runoff generation in humid headwater catchments, 2. A case study of hillslope and low-order stream response. Water Resour. Res., 22(8): 1273-1282.
Troendle, C.A. and J.W. Homeyer, 1971. Stormflow related to measured physical parameters on small forested watersheds in West Virginia. Transactions of the American Geophysical Union 52: 204.
Turner, J., Macpherson, D.K. and Stokes, R.A., 1987. The mechanisms of catchment flow processes using natural variations in deuterium and oxygen-18. Jour. of Hydrol., 94: 143-162.
Turner, J. and Macpherson, D.K., 1990. Mechanisms affecting streamflow and stream water quality: An approach via stable isotope, hydrogeochemical, and time series analysis. Water Resour. Res., 26(12): 3005-3019.
van't Woudt, B.D., 1954. On factors governing subsurface storm flow in volcanic ash soils, New Zealand. Transactions of the American Geophysical Union 35(1): 136-144.
Waddington, J.M., Roulet, N.T. and Hill, A.R., 1993. Runoff mechanisms in a forested groundwater discharge wetland. Jour. of Hydrol., 147: 37-60.
Weyman, D.R., 1970. Throughflow on hillslopes and its relation to the stream hydrograph. Bulletin of the International Association of Scientific Hydrology XV(3): 25-32.
Weyman, D.R., 1973. Measurements of the downslope flow of water in a soil. Jour. of Hydrol., 20: 267-288.
Whipkey, R.Z., 1965. Subsurface stormflow from forested slopes. International Association of Scientific Hydrology Bulletin 10(2): 74-85.
Whipkey, R.Z., 1969. Storm runoff from forested catchments by subsurface
routes. In: Floods and Their Computation, International Association of
Scientific Hydrology Publication Number 85.