Greetings List,
Finishing up the layout on my masters thesis written with Bean ---> LyX
a terrific combo for OS X. Thanks to everybody involved in improving
and developing this wonderful program.
running LyX 1.5.5 on PPC Mac OS X 10.5.4
Problem:
When two sided document is chosen (koma-script Book Class, or Book
Class) alternating Right Left pages fails when \pagenumbering{roman}
goes to \pagenumbering{arabic}. Problem does not occur when using all
{arabic}. I tried \frontmatter and \mainmatter first but that caused
bizarre numbering with the child documents. I've attached a main file
and a child document that recreates the problem.
Question:
I am using the ragged2e package for my whole document but would like
the chapter Abstracts justified. How do I add "justified" to a single
page? (such as the abstract page of the attached child document).
Thank you for your time,
Zan
#LyX 1.5.5 created this file. For more info see http://www.lyx.org/
\lyxformat 276
\begin_document
\begin_header
\textclass scrbook
\begin_preamble
\usepackage{ragged2e}
\raggedright
\setlength{\parindent}{20pt}
\renewcommand{\theequation}{Eq. \arabic{equation}}
\usepackage{graphicx}
\usepackage[font=small,labelfont=small,labelfont=bf,labelsep=period]{caption}
\newcommand{\sups}[1]{\raisebox{1ex}{\small #1}}
\newcommand{\subs}[1]{\raisebox{-.8ex}{\small #1}}
\usepackage{indentfirst}
\end_preamble
\language english
\inputencoding auto
\font_roman default
\font_sans default
\font_typewriter default
\font_default_family default
\font_sc false
\font_osf false
\font_sf_scale 100
\font_tt_scale 100
\graphics default
\paperfontsize 12
\spacing double
\papersize letterpaper
\use_geometry true
\use_amsmath 0
\use_esint 0
\cite_engine natbib_authoryear
\use_bibtopic false
\paperorientation portrait
\leftmargin 1.75in
\topmargin 1in
\rightmargin 1in
\bottommargin 1in
\secnumdepth 3
\tocdepth 3
\paragraph_separation indent
\defskip medskip
\quotes_language english
\papercolumns 1
\papersides 1
\paperpagestyle plain
\tracking_changes false
\output_changes false
\author ""
\author ""
\end_header
\begin_body
\begin_layout Chapter
\paragraph_spacing single
Annual Water and Solute Export from the Yukon River and its Tributaries
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset VSpace vfill*
\end_inset
\end_layout
\begin_layout Standard
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
addcontentsline{toc}{section}{Abstract}
\end_layout
\end_inset
\end_layout
\begin_layout Standard
\paragraph_spacing single
\noindent
\align center
\series bold
ABSTRACT
\end_layout
\begin_layout Standard
\paragraph_spacing single
Annual export of eleven major and trace solutes are determined for the Yukon
River based on summing 42 tributary contributions.
First we show that annual discharge of the Yukon River at three mainstem
locations can be computed by summing calculated annual discharges from
42 tributaries.
Annual discharge for the ungaged tributaries is calculated from basin area
and average annual precipitation over that area using a previously published
regional regression equation.
Based on tributary inputs we estimate an average annual discharge for the
Yukon River of 211\InsetSpace ~
\family roman
\series medium
\shape up
\size normal
\emph off
\bar no
\noun off
\color none
\begin_inset Formula $km^{3}\: yr^{-1}$
\end_inset
\family default
\series default
\shape default
\size default
\emph default
\bar default
\noun default
\color inherit
.
This value is within 2% of the average measured annual discharge at the
USGS gaging station at Pilot Station, AK for water years 2001 through 2005.
Next, annual loads for 11 solutes are determined by combining annual discharge
with point measurements of solute concentrations in tributary river water.
Based on the sum of tributary water we find that the Yukon River discharges
approximately 33 million metric tons of dissolved solids each year at Pilot
Station.
Discharged solutes are dominated by cations calcium and magnesium (5.66x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
and 1.42x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
\begin_inset Formula $g\: yr^{-1}$
\end_inset
) and anions bicarbonate and sulfate (17.2x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
and 5.42x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
\begin_inset Formula $g\: yr^{-1}$
\end_inset
.
These loads compare well with loads calculated using the USGS computer
program LOADEST based on daily discharge and 34 instantaneous solute concentrat
ion measurements at three locations along the Yukon River.
Annual solute loads determined by summing tributary contributions show
an average difference from LOADEST calculations of 9% for eleven solutes
at three locations along the mainstem of the Yukon River.
These findings show that annual solute yields for a major subarctic river
can be determined from tributary basin contributions based on calculated
annual discharge and distributed point measurements of solute concentration.
\end_layout
\begin_layout Standard
\begin_inset VSpace vfill*
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Section
Introduction
\end_layout
\begin_layout Standard
Freshwater inputs to the Arctic Ocean play an important role in nutrient
cycling along the North American and Asian continental shelfs
\begin_inset LatexCommand citep
key "Rudels1991"
\end_inset
.
The northern high latitudes are known to be experiencing warming at a faster
rate than the global average
\begin_inset LatexCommand citep
key "Serreze2000"
\end_inset
.
The observed and predicted warming of this region has motivated research
in quantifying the freshwater budget of the Arctic Ocean and predicting
how that budget is likely to change in the future.
A number of investigations have focused specifically on the transport of
water and solutes from the largest circumpolar rivers
\begin_inset LatexCommand citep
key "Holmes2002,mcclelland2006,Peterson2002"
\end_inset
.
Although the Yukon River debouches into the Bering Sea some 300km south
of the Chukchi Sea region of the Arctic Ocean, bathymetric contours and
strong coastal currents favor water and sediment export north through the
Bering Strait
\begin_inset LatexCommand citep
key "McManus1974"
\end_inset
.
The Yukon River is the fifth largest circumpolar river in terms of annual
water discharge, and carries the second greatest annual sediment load
\begin_inset LatexCommand citep
key "Holmes2002"
\end_inset
.
\end_layout
\begin_layout Standard
Investigations of annual solute export from major rivers are useful for
describing integrated solute production processes occurring over large
land areas.
In the Mackenzie River Basin water chemistry correlated with mineral and
rock sources within tributary subbasins
\begin_inset LatexCommand citep
key "Reeder1972a"
\end_inset
.
A more recent study by
\begin_inset LatexCommand citet
key "Millot2003"
\end_inset
found that solute yields attributed to chemical weathering of silicate
minerals varied by a factor of four among tributaries and was influenced
by lithology, and abundance of soil organic matter.
In tributaries to the Lena River of eastern Siberia,
\begin_inset LatexCommand citet
key "Huh1998"
\end_inset
show that net CO
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
subs{2}
\end_layout
\end_inset
consumption from silicate mineral weathering is comparable to consumption
calculated for tropical basins.
In western Siberia, solute load correlated with permafrost distribution,
with higher loads being found in rivers having less extensive or absent
permafrost
\begin_inset LatexCommand citep
key "Frey2007"
\end_inset
.
\end_layout
\begin_layout Standard
A first step in identifying landscape controls on surface water chemistry
is to analyze solute export from individual tributaries.
There are 41 tributaries of the Yukon River draining areas greater than
1000\InsetSpace \thinspace{}
\begin_inset Formula $km^{2}$
\end_inset
(Table
\begin_inset LatexCommand ref
reference "tab:Basin-characteristics-and"
\end_inset
).
Determining individual tributary contributions to total Yukon River flow
is complicated because nearly all of these rivers are ungaged where they
enter the Yukon River mainstem.
This task is further complicated by limited water chemistry data available
for each tributary.
The quantity of solutes and sediment exported from a river basin generally
scales with the quantity of water exported, though the exact relationship
is variable
\begin_inset LatexCommand citep
key "Dingman1994,drever1997,Stallard1995,Syvitski2000"
\end_inset
.
In order to determine the contribution to Yukon River dissolved load by
tributaries the annual water export of each tributary must
\end_layout
\end_body
\end_document
#LyX 1.5.5 created this file. For more info see http://www.lyx.org/
\lyxformat 276
\begin_document
\begin_header
\textclass scrbook
\begin_preamble
\usepackage{ragged2e}
\raggedright
\setlength{\parindent}{20pt}
\renewcommand{\theequation}{Eq. \arabic{equation}}
\usepackage{graphicx}
\usepackage[font=small,labelfont=small,labelfont=bf,labelsep=period]{caption}
\newcommand{\sups}[1]{\raisebox{1ex}{\small #1}}
\newcommand{\subs}[1]{\raisebox{-.8ex}{\small #1}}
\usepackage{indentfirst}
\end_preamble
\language english
\inputencoding auto
\font_roman default
\font_sans default
\font_typewriter default
\font_default_family default
\font_sc false
\font_osf false
\font_sf_scale 100
\font_tt_scale 100
\graphics default
\paperfontsize 12
\spacing double
\papersize letterpaper
\use_geometry true
\use_amsmath 0
\use_esint 0
\cite_engine natbib_authoryear
\use_bibtopic false
\paperorientation portrait
\leftmargin 1.75in
\topmargin 1in
\rightmargin 1in
\bottommargin 1in
\secnumdepth 3
\tocdepth 3
\paragraph_separation indent
\defskip medskip
\quotes_language english
\papercolumns 1
\papersides 2
\paperpagestyle plain
\tracking_changes false
\output_changes false
\author ""
\author ""
\end_header
\begin_body
\begin_layout Standard
\paragraph_spacing double
\noindent
\align center
\size largest
Water and Solute Export from the Yukon River and its
\newline
Tributaries
\size default
\end_layout
\begin_layout Standard
\paragraph_spacing double
\noindent
\align center
\size larger
by
\newline
\begin_inset VSpace smallskip
\end_inset
\end_layout
\begin_layout Standard
\paragraph_spacing onehalf
\noindent
\align center
\size largest
Zanden Arthur Frederick
\size larger
\begin_inset VSpace defskip
\end_inset
\end_layout
\begin_layout Standard
\noindent
\align center
\size large
B.S.
Western Washington University, 2001
\end_layout
\begin_layout Standard
\begin_inset VSpace vfill
\end_inset
\end_layout
\begin_layout Standard
\paragraph_spacing double
\noindent
\align center
\size large
A thesis submitted to the
\size default
\newline
\size large
Faculty of the Graduate School of the
\newline
University of Colorado in partial
fulfillment
\newline
of the requirement for the degree of
\newline
Masters of Arts
\newline
Department
of Geography
\newline
2008
\size default
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
thispagestyle{empty}
\end_layout
\end_inset
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
pagenumbering{roman}
\end_layout
\end_inset
\end_layout
\begin_layout Standard
\noindent
\align center
\begin_inset VSpace bigskip
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset VSpace medskip*
\end_inset
\end_layout
\begin_layout Standard
\paragraph_spacing single
\noindent
\align center
This thesis entitled:
\newline
Water and Solute Export from the Yukon River and its
Tributaries
\newline
Written by Zanden A.
Frederick
\newline
Has been approved for the Department of Geography
\newline
\begin_inset VSpace 1in*
\end_inset
\end_layout
\begin_layout Standard
\noindent
\align center
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
underline{
\backslash
hspace{3in}}
\end_layout
\end_inset
\newline
Suzanne P.
Anderson, Committee Chair
\end_layout
\begin_layout Standard
\noindent
\align center
\begin_inset VSpace bigskip*
\end_inset
\end_layout
\begin_layout Standard
\noindent
\align center
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
underline{
\backslash
hspace{3in}}
\end_layout
\end_inset
\newline
Robert G.
Striegl, Committee Member
\end_layout
\begin_layout Standard
\noindent
\align center
\begin_inset VSpace bigskip*
\end_inset
\end_layout
\begin_layout Standard
\noindent
\align center
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
underline{
\backslash
hspace{3in}}
\end_layout
\end_inset
\newline
John Pitlick, Committee Member
\end_layout
\begin_layout Standard
\begin_inset VSpace 1in*
\end_inset
\end_layout
\begin_layout Standard
\align right
Date
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
underline{
\backslash
hspace{2in}}
\end_layout
\end_inset
\newline
\begin_inset VSpace vfill*
\end_inset
\end_layout
\begin_layout Standard
\paragraph_spacing single
\align center
The final copy of this thesis has been examined by the signatories, and
we find that both the content and form meet acceptable presentation standards
of scholarly work in the above mentioned discipline
\end_layout
\begin_layout Standard
\begin_inset VSpace bigskip*
\end_inset
\end_layout
\begin_layout Standard
\paragraph_spacing double
\noindent
\align center
\begin_inset ERT
status open
\begin_layout Standard
\backslash
thispagestyle{empty}
\end_layout
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
addcontentsline{toc}{section}{Abstract}
\end_layout
\end_inset
\end_layout
\begin_layout Standard
\noindent
\align left
Frederick, Zanden A.
(M.A., Department of Geography)
\end_layout
\begin_layout Standard
\noindent
\align left
Water and Solute Export from the Yukon River and its Tributaries
\end_layout
\begin_layout Standard
\noindent
\align left
Thesis directed by Assistant Professor Suzanne P.
Anderson
\end_layout
\begin_layout Standard
33 million metric tons of dissolved solids each year at Pilot Station.
Discharged solutes are dominated by cations calcium and magnesium (5.66x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
and 1.42x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
\begin_inset Formula $g\: yr^{-1}$
\end_inset
) and anions bicarbonate and sulfate (17.2x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
and 5.42x10
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
sups{12}
\end_layout
\end_inset
\begin_inset Formula $g\: yr^{-1}$
\end_inset
.
These loads compare well with loads calculated using the USGS Loadest computer
program based on daily discharge and 34 instantaneous solute concentration
measurements at three locations along the Yukon River.
Annual solute loads determined by summing tributary contributions show
an average difference from loads calculated with Loadest of 9% for eleven
solutes at three locations along the mainstem of the Yukon River.
These findings show that annual solute yields for a major subarctic river
can be determined from tributary basin contributions based on calculated
annual discharge and distributed point measurements of solute concentration.
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset LatexCommand tableofcontents
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset FloatList table
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset FloatList figure
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\begin_inset ERT
status collapsed
\begin_layout Standard
\backslash
pagenumbering{arabic}
\end_layout
\end_inset
\end_layout
\begin_layout Standard
\begin_inset Include \include{zanchild1.lyx}
preview false
\end_inset
\end_layout
\begin_layout Standard
\newpage
\end_layout
\begin_layout Standard
\paragraph_spacing single
\begin_inset LatexCommand bibtex
options "bibtotoc,apalike2"
bibfiles "water"
\end_inset
\end_layout
\end_body
\end_document