Rough in thesis

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/"
 

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.
+
+

static/css/starter.css

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