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Kinematic Model of River Ice Motion During Dynamic Breakup      Kinematic Model  River Ice Motion  Dynamic Breakup        font style='font-size:12px;'> 2009/10/26
We begin a study of the dynamics of ice motion during river breakup by formulating a kinematic model. Ice continuity equations are applied to relate the speeds of a breaking front, a convergence fro...
Tracer Test in Fractured Chalk 2.Numerical Analysis     Tracer Test  Fractured Chalk  Numerical Analysis       font style='font-size:12px;'> 2009/10/26
A two-well tracer test carried out in fractured chalk was analyzed using a threedimensional finite-difference model for flow and transport which, was constructed on the basis of the geological and h...
A two-well tracer test was conducted in eastern Denmark, in which a short duration pulse of lithium chloride was injected into a recharge well and made to flow through a fractured chalk aquifer to a...
Potential Evaporation—A Matter of Definition      Potential Evaporation  Matter of Definition        font style='font-size:12px;'> 2009/10/26
The aim of this paper is to discuss the concept of potential evaporation and its use in runoff models. The potential evaporation for forest is defined on basis of estimated minimum canopy resistance...
Low Flow Estimation and Hydrogeology in a Chalk Catchment      Low Flow Estimation  Hydrogeology  Chalk Catchment        font style='font-size:12px;'> 2009/10/26
Procedures to estimate low flow statistics at ungauged sites and their relation to hydrogeology are presented. The discussion is based on an example of a Danish chalk catchment of 242 kmz, within wh...
This contribution investigates the performance of discharge modelling when proceeding from rather simple methods of snowmelt modelling to more sophisticated, distributed approaches. In all cases, th...
Energy balance measurements over a seasonal snow cover were performed near Davos, Switzerland at 2,540 m a.s.1. The energy fluxes were studied over dry and melting snow covers. The beginning of snow...
Currents and vertical mixing characteristics were investigated on the basis of time series of current meter and temperature data from a summer-stratified period in Lake Ontario. The experimental set...
Prediction of Log-Transmissivity 1.Using Specific Capacity     Prediction  Log-Transmissivity  Specific Capacity       font style='font-size:12px;'> 2009/10/26
The log-transmissivity may in many cases be predicted from the log-transformed specific capacity of wells by applying a linear statistical model. The coefficients of the linear equation can be estim...
几条水文学定理·定律和推论研究初探     水文学  定理  定律  推论       font style='font-size:12px;'> 2009/10/26
提出了水文学定理、定律及推论的概念,并结合水文学实际,总结出几条水文学定理、定律和推论,为加快水文学理论在这方面的发展并进一步促进生产技术水平的提高提供参考。
Two physically based models are derived that can be used to predict the log-transmissivity from the lithology, e.g. as logged in boreholes. The first model uses the lithology as the only predictor, wh...
An operational model for estimation of frost heave in field where stratified soil profile appears is presented. The model is developed from the research model described in part B. Soil layers are fi...
A frost heave model which simulates formation of ice lenses is developed for saturated salt-free soils. Quasi-steady state heat and mass flow is considered. Special attention is paid to the transmit...
The overall circulation pattern in spring is rather specific as density-induced currents may be of significance. The density-driven circulation perpendicular to the shore can be described as consist...
Ground thawing and soil warming arc governed by ground heat flux, soil thermal properties and the ice content of the soil, all of which are directly or indircctly inlluenced by the soil moisture sta...

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