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

Reply via email to