Periodic heat flow in a stratified medium, with application to permafrost problems by Arthur H. Lachenbruch

Cover of: Periodic heat flow in a stratified medium, with application to permafrost problems | Arthur H. Lachenbruch

Published by U.S. G.P.O. in Washington .

Written in English

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Subjects:

  • Heat -- Transmission.,
  • Frozen ground -- Thermal properties.,
  • Earth temperature.,
  • Geophysics.

About the Edition

A discussion of temperature fluctuations in a stratified medium caused by a periodically varying surface temperature, with special reference to the effects of seasonal temperature variation on gravel fills, the natural active layer and permafrost.

Edition Notes

Book details

Statementby Arthur H. Lachenbruch.
SeriesExperimental and theoretical geophysics, Geological Survey bulletin -- 1083-A
The Physical Object
Paginationvi, 36 p. :
Number of Pages36
ID Numbers
Open LibraryOL22967677M

Download Periodic heat flow in a stratified medium, with application to permafrost problems

PERIODIC HEAT FLOW IN A STRATIFIED MEDIUM WITH APPLICATION TO PERMAFROST PROBLEMS By ARTHUR H. LACHENBRUCH ABSTRACT Solutions to the Fourier heat equation for quasi-steady periodic flow in a stratified semi-infinite medium can be Cited by: 2.

A discussion of temperature fluctuiations in a stratified medium caused by a periodically varying surface with application to permafrost problems book with special reference to the effects of seasonal temperature variation on gravel fills, the natural active layer and permafrost.

Periodic heat flow in a stratified medium with application to permafrost problems Bulletin A By: A.H. Lachenbruch. Conditions of the problem for periodic temperature field in a two-layer medium.

The complete changes of temperature in the mediums considered t 1 (x, τ) and t 2 (x, τ) represent the daily temperature fluctuations t ˜ 1 (x, τ) and t ˜ 2 (x, τ) relative to the mean daily values t ¯ 1 (x, τ) and t ¯ 2 (x, τ).Cited by: 1.

Lachenbruch A H Periodic heat flow in a stratified medium, with application to permafrost problems Experimental and Theoretical Geophysics (Geological Survey Bulletin ) (Washington, DC: United States Government Printing Office) pp 1–34Cited by: Lachenbruch () derived solutions to the problem of periodic temperature and heat flow variations in a stratified semi-infinite medium and showed examples of their application to ground temperature by: Periodic heat flow in a stratified medium with application to permafrost problems.

Article. In his book on permafrost research, Sumgin subdivided the history of Russian permafrost studies. Lachenbruch, A.H., Periodic heat flow in a stratified medium with application to permafrost problems. U.S. Geological Survey Bulletin A (United States Government Printing Office.

FULLY DEVELOPED & PERIODIC FLOWS Advantages of fully developed regime • The case of developed flow in a duct or passage of constant cross-section will be referred to as single-slab fully-developed flow, since such flows can be simulated by performing calculations on a single-slab of computational Size: KB.

Chapter 4: Modeling Periodic Flow and Heat Transfer This tutorial is divided into the following sections: Introduction Prerequisites Problem Description Setup and Solution Summary Further Improvements Introduction Many industrial applications, such as steam generation in a boiler or air cooling in the coil of File Size: KB.

Periodic heat flow in a stratified medium with application to permafrost problems, (). Permafrost temperature records: Indicators of climate change, Eos Trans. Lachenbruch, A. H.,Periodic with application to permafrost problems book flow in a stratified medium with application to permafrost problems, U.S.

Geol. Surv. Bull., A, 1–   An engineering method of calculating the thawing depth of permafrost in a multilayer base is proposed. The method includes an exact analytical solution of the problem of nonstationary heat conduction in a multilayer medium, including efficient thermal insulation with phase transitions (Stefan's problem) with a stepped calculation for each layer.

Comparing the computational results Author: V. Ivanov, V. Merzlyakov, A. Plotnikov. Periodic boundaries are used for the inlet and outlet of the flow domain.

The inlet and outlet profiles for the ve-locities must be identical. Constant mass flow rate of air is assumed in the flow direction due to the periodic flow conditions.

Also a mean bulk temperature of K is applied at the inlet. The physical properties of the airFile Size: KB. book Co., 5. Lachenbruch, A.H.: Periodic Heat Flow in a Stratified Medium with Appli- cation to Permafrost Problems.

Geol. Survey Bull. A, 36 pp. The simulation and implications of thermal plumes produced by Arctic con struction in smooth terrain Cited by: 6. PERIODIC HEAT FLOW IN A STRATIFIED MEDIUM WITH APPLICATION TO PERMAFROST PROBLEMS, Arthur H.

Lachenbruch; Geological Survey Bulletin 10B3A () 2-,;- ~-;; d GENERAL The Anderson System concept grew out of an awareness that. The effect of this on a building is that in the hot period heat flows from the environment into the building, where some of it is stored, and at night during the cool period, the heat flow is reversed: from the building to the environment.

As the cycle is repetitive, it can be described as periodic heat flow. Tutorial 2. Modeling Periodic Flow and Heat Transfer Introduction: Many industrial applications, such as steam generation in a boiler or air cooling in the coil of an air conditioner, can be modeled as two-dimensional periodic heat ow.

This tutorial illustrates how to set up and solve a periodic heat transfer problem, given a pregenerated Size: KB. Periodic heat flow in a stratified medium with application to permafrost problems, Lachenbruch. A.H., Permafrost, the active layer, and changing climate, Methodology to identify the reference rock sites in regions of medium-to-high seismicity: an application in Central ItalyCited by:   A tube bank is considered with the required boundary conditions as given in video.

The whole analysis is demonstrated from modelling to contours of solution. Chapter A: Periodic heat flow in a stratified medium with application to permafrost problems Chapter B: Directional resistivity measurements in exploration for uranium deposits on. ANALYTICAL HEAT TRANSFER Mihir Sen Department of Aerospace and Mechanical Engineering University of Notre Dame Notre Dame, IN May 3, decomposition of the flow into mean and periodic components, and used finite-element simulations to solve for the mean flow over the cylinder.

Periodic component of the flow contributes to an artificial body force in the Navier-Stokes equation. According to our simulations, time-averaged Nusselt numbers are not strongly affected by oscillations. Periodic Heat Flow. In nature the variation of climatic conditions produces a non- steady state.

Diurnal variations produce an approximately repetitive hour cycle of increasing and decreasing temperatures. The effect of this on a building is that in the hot period heat flows from the outdoors into the building, where some of it is stored.

evidence from permafrost in the Alaskan Arctic, Science, v.p. Exercises 1) Create a model of heat flow through a m thick chunk of ground. I would recommend that you do this in m thick layers, so that you don't have to work with too many reservoirs and fluxes. As you do this, consider what the.

Outflow at one periodic boundary is inflow at the other inflow outflow Periodic heat transfer • Also known as streamwise-periodic or fully-developed flow. • Used when flow and heat transfer patterns are repeated, e.g: – Compact heat exchangers. – Flow across tube banks. • Geometry and boundary conditions repeat in streamwise Size: KB.

1 COMPUTER METHODS AND MODELING IN GEOLOGY TEMPERATURE PROFILES IN PERMAFROST The parts of this exercise for students are in normal text, whereas answers and explanations for faculty are italicized.

Permafrost is perennially frozen ground that. /lp/wiley/climate-and-the-limits-of-permafrost-a-zonal-analysis-5i4LasTtk2. Journals / Periodic heat flow in a stratified medium with application to permafrost problems. Lachenbruch, Lachenbruch.

Permafrost in organic soils of northern Alberta. Lachenbruch A. PERIODIC HEAT FLOW IN A STRATIFIED MEDIUM WITH APPLICATION TO PERMAFROST PROBLEMS USGS A 8vo, wps, light wear, lib, vg, 36 pp., 3 plts, 8 figs. Price: $ (stock#USGSBA) Lachenbruch A. and Nrewer M. DISSIPATION OF THE TEMPERATURE EFFECT OF DRILLING A WELL IN ARCTIC ALASKA 8vo, wps, light wear, vg, 37.

Periodic heat flow in a stratified medium with application to permafrost problems by A.H. LachenbruchDirectional resistivity measurements in exploration for uranium deposits on the Colorado plateau, by G.V. KellerDissipation of the temperature effect of drilling a well in Arctic Alaska by A.H.

Lautenbruch and M.C. BrewerPulse-transient. Keywords: heat transfer, heat exchangers, mass flow rate, Nusselt number, periodic flow. I INTRODUCTION Many industrial applications, such as steam generation in a boiler, air cooling in the coil of air conditioner and different type of heat exchangers uses tube banks to accomplish a desired total heat File Size: 1MB.

Periodic heat flow through building section is practically being used for air-conditioning applications. An effort has been made to combine the non-periodic transient heat flow due to instantaneous rise in outdoor temperature with periodic heat flow.

The study becomes useful to predict. 2Lachenbruch, A. Periodic heat flow in a stratified medium with applica-tion to permafrost problems. U.S. Geolog-ical Survey Bulletin A, 36 pp. SMaykut, G.

and N. Untersteiner. Some results from a time dependent thermodynamic model of sea ice. Journal of Geophysical Research, 76(6): 4Holter, M. et al. BASIC HEAT TRANSFER AND SOME APPLICATIONS IN POLYMER PROCESSING (A version of this was published as a book chapter in Plastics Technician’s Toolbox, Volume 2, PagesSPE ) John Vlachopoulos and David Strutt Heat transfer is a branch of engineering science which seeks to determine the rate of energyFile Size: KB.

Periodic heat flow in a stratified medium with applica- tion to permafrost problems. U.S. Geolog- ical Survey Bulletin A, 36 pp. 8Maykut, G. and N. Untersteiner. Some results from a time dependent thermodynamic model of sea ice. Journal of Geophysical Research, 76(6): rHolter, M.

et al. Research needs. • Define a specified periodic mass flow rate. • Model periodic heat transfer with specified temperature boundary conditions. • Calculate a solution using the pressure-based solver.

time t, and let H(t) be the total amount of heat (in calories) contained in c be the specific heat of the material and ‰ its density (mass per unit volume). Then H(t) = Z D c‰u(x;t)dx: Therefore, the change in heat is given by dH dt = Z D c‰ut(x;t)dx: Fourier’s Law says that heat flows from hot to cold regions at a rate • > 0 proportional to the temperature Size: KB.

The relationship between pile spacing and the amount of heat introduced into the permafrost can be taken from the following equation: Q = C(S 2 -A)T.

^ v ' mc where: S = the spacing of the piles, ft A = the area of tne hole, sf T. = temperature rise of permafrost, F mc * * Q = Latent heat of the slurry, Btu/ft of pile [57] Since the natural.

Key Words: Dry materials, infinite slabs, moist materials, periodic heat flow, temperature dependence, thermal conductivity, thermal diffusivity. Introduction Water migrates when a temperature gradient is applied to a moist porous material.

This fact has to be borne in mind when designing experiments to measure the thermal properties of moist. Periodic heat flow means that heat flow is a continu-ous function of time and repeats itself at regular inter­ vals. A semi-infinite solid has only one bounding plane and extends to infinity in all other directions.

The problem of determining the temperature in a homo­ geneous semi-infinite solid undergoing periodic heat flow has been. Periodic Heat Flow in a Stratified Medium with Application to Permafrost Problems. U.S. Geological Survey. Bulletin A. 36 p. _____. Three-dimensional heat conduction in permafrost beneath heated buildings.

U.S. Geological Survey. Bulletin B. pp. BB _____. Thermal effects of the ocean on permafrost. Geological Society.ENVIROM,IENTAL GEOLOGY AND FOUNDATION PROBLEMS and extent of permafrost vary, and the consequences of building on ice-rich ground vary as well.

Lachenbruch, A. H.,Periodic heat flow in a stratified medium with application to permafrost problems: U.S. Geol Survey Bull.p.Pernnfrost, in Fairbridge, R. H., ed. The local equivalence ratio distribution in a flame affects its shape and response under velocity perturbations.

The forced heat release response of stratified lean-premixed flames to acoustic velocity fluctuations is investigated via chemiluminescence measurements Cited by: 6.

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