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Rough in thesis

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Matthew Dillon 2015-06-21 15:03:13 -08:00
parent 889cc7d728
commit 83909b0570
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13
config.toml
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@ -2,23 +2,28 @@ baseurl = "https://akdillon.net"
languageCode = "en-us" languageCode = "en-us"
title = "AKDillon" title = "AKDillon"
canonifyurls = true canonifyurls = true
SectionPagesMenu = "main"
[[menu.main]]
name = "MRD CE Thesis"
weight = -30
identifier = "mrd_ce_thesis"
url = "/mrd_ce_thesis/"
[[menu.main]] [[menu.main]]
name = "Audio" name = "Audio"
weight = 50 weight = -20
identifier = "audio" identifier = "audio"
url = "/audio/" url = "/audio/"
[[menu.main]] [[menu.main]]
name = "About" name = "About"
weight = 100 weight = -10
identifier = "about" identifier = "about"
url = "/about/" url = "/about/"
[[menu.main]] [[menu.main]]
name = "Contact" name = "Contact"
weight = 150 weight = 0
identifier = "contact" identifier = "contact"
url = "/contact/" url = "/contact/"

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content/mrd_ce_thesis/index.md Normal file
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@ -0,0 +1,36 @@
+++
date = "2015-06-21T12:19:11-08:00"
draft = true
title = "MRD Civil Engineering Thesis Info"
aliases = [
"/pages/mrd-ce-ms/index.html"
]
+++
### Abstract
> Frost heave is typically associated with the formation of segregation ice in
> fine-grained soil. Coarse-grained soil is generally considered to be non-frost
> susceptible. Field observations and laboratory experiments show that
> coarse-grained soil can be extremely ice-rich in specific conditions. Previous
> studies have shown that oscillation of the frozen-unfrozen boundary can lead to
> the formation of ice by a mechanism different from the segregation ice
> mechanism. Conditions related to the formation of ice in coarse-grained soil
> were investigated using modern laboratory techniques. Fourteen tests were
> conducted on five soil types. The thickness of soil subjected to freeze-thaw
> cycles was varied and controlled by the magnitude and duration of applied soil
> temperatures. The thickness of the ice formed increased when the sample
> drainage was limited or prevented during cooling. Under specific conditions,
> the formation of a discrete ice layer was observed in coarse-grained soils.
> Seven samples were scanned with the μCT scanner at the completion of the
> warming and cooling tests. The sub-samples scanned were analyzed in 2D
> cross-sections, and charac- terized as 3D reconstructions. Frost heave induced
> by the formation of ice was observed in both fine- and coarse-grained soils,
> including soils that were found to be traditionally non-frost susceptible.
### [Download](http://storage.googleapis.com/thermokarst-misc/ce_thesis/MRDillonCEThesisManuscript.pdf)
PDF format manuscript, 166 pages. Science Commons, 2012.

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static/css/starter.css
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@ -48,3 +48,39 @@ a:hover {
border-top: 1px solid #eee; border-top: 1px solid #eee;
padding-top: 15px; padding-top: 15px;
} }
blockquote {
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color: #777;
font-style: italic;
margin: 1em 2em;
padding-left: 1em;
text-align: left;
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blockquote cite {
color: #555;
display: block;
font-size: 14px;
font-size: 0.875rem;
line-height: 1.71429;
}
blockquote cite:before {
content: "\2014 \0020";
}
blockquote cite a {
color: #555;
}
blockquote cite a:visited {
color: #555;
}
blockquote.blockquote-reverse {
border-left: none;
border-right: 1px solid #ddd;
padding: 0 1em 0 0;
text-align: right;
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