From 83909b05707526036a758a356f230c03c2f4039c Mon Sep 17 00:00:00 2001
From: Matthew Dillon <mrdillon@alaska.edu>
Date: Sun, 21 Jun 2015 15:03:13 -0800
Subject: [PATCH] Rough in thesis

---
 config.toml                    | 13 ++++++++----
 content/mrd_ce_thesis/index.md | 36 ++++++++++++++++++++++++++++++++++
 static/css/starter.css         | 36 ++++++++++++++++++++++++++++++++++
 3 files changed, 81 insertions(+), 4 deletions(-)
 create mode 100644 content/mrd_ce_thesis/index.md

diff --git a/config.toml b/config.toml
index 92bb233..e59fee1 100644
--- a/config.toml
+++ b/config.toml
@@ -2,23 +2,28 @@ baseurl = "https://akdillon.net"
 languageCode = "en-us"
 title = "AKDillon"
 canonifyurls = true
-SectionPagesMenu = "main"
+
+[[menu.main]]
+    name = "MRD CE Thesis"
+    weight = -30
+    identifier = "mrd_ce_thesis"
+    url = "/mrd_ce_thesis/"
 
 [[menu.main]]
     name = "Audio"
-    weight = 50
+    weight = -20
     identifier = "audio"
     url = "/audio/"
 
 [[menu.main]]
     name = "About"
-    weight = 100
+    weight = -10
     identifier = "about"
     url = "/about/"
 
 [[menu.main]]
     name = "Contact"
-    weight = 150
+    weight = 0
     identifier = "contact"
     url = "/contact/"
 
diff --git a/content/mrd_ce_thesis/index.md b/content/mrd_ce_thesis/index.md
new file mode 100644
index 0000000..4d3a540
--- /dev/null
+++ b/content/mrd_ce_thesis/index.md
@@ -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.
+
+
diff --git a/static/css/starter.css b/static/css/starter.css
index 759a3a8..aeb037d 100644
--- a/static/css/starter.css
+++ b/static/css/starter.css
@@ -48,3 +48,39 @@ a:hover {
   border-top: 1px solid #eee;
   padding-top: 15px;
 }
+
+blockquote {
+  border-left: 1px solid #ddd;
+  color: #777;
+  font-style: italic;
+  margin: 1em 2em;
+  padding-left: 1em;
+  text-align: left;
+}
+
+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;
+}