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Course Number: NEW 05, Fall 2009

College/University: UNL

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New Username and Password 1. New user sites will be able to access Internet CIS when they receive their usernames and passwords. They will not have to wait until the activation date. 2. Each site will receive bookmarks with the site's username and password that can be distributed to students so they can use Internet CIS at home. 3. The site's username and password can be published in a school newspaper but not on...

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Username New and Password 1. New user sites will be able to access Internet CIS when they receive their usernames and passwords. They will not have to wait until the activation date. 2. Each site will receive bookmarks with the site's username and password that can be distributed to students so they can use Internet at CIS home. 3. The site's username and password can be published in a school newspaper but not on a website. 4. A link from the school website to CIS for Internet is acceptable as...

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UNL - NEW - 05
Job SearchJob Search Overview Steps to a Successful Job Search Ways to Choose an Occupation Identify Your SkillsStep 1 - Choose an OccupationStep 2 - Develop a Plan Step 3 - Collect Information Collect Important Information Job Applicatio
UNL - NEW - 05
OccupationsOccupations1. From the homepage, go to Occupations. 2. Select FAQs. What is an occupation? How do I find information in occupations? What should I keep in mind when choosing an occupation? How do I use CIS to choose an occupation? What
UNL - NEW - 05
School SortUndergraduate/Graduate School Sort Describes categories that may be used in choosing a college Lets you decide which characteristics are important to youCreates a list of schools in Nebraska and the United States for you to explore f
UNL - NEW - 05
New Username and Password1. New user sites will be able to access Internet CIS when they receive their usernames and passwords. They will not have to wait until the activation date. 2. Each site will receive bookmarks with the site's username and p
UNL - SARA - 2000
FromRealitytoDatabases: aOnetoManyRelationshipStefanoSpaccapietraDatabase Laboratory Swiss Federal Institute of Technology Lausanne (EPFL) joint work withChristine PARENT & Christelle VANGENOThttp:/lbd.epfl.chOutlines s sDatabase design ess
UNL - CHAPTER - 2
WOLF v. COCA-COLA COMPANYUnited States Court of Appeals, Eleventh Circuit. 200 F.3d 1337 (2000)BLACK, Circuit Judge: Appellant Sheila Wolf filed suit against Appellee Coca-Cola Company (Coca-Cola) and a number of individual defendants after being
UNL - WILLBORNCH - 17
SMITH v. CITY OF JACKSON, MISSISSIPPI United States Supreme Court 125 S.Ct, 1536 (2005) MR. JUSTICE STEVENS announced the judgment of the Court and delivered the opinion of the Court with respect to Parts I, II, and IV, and an opinion with respect to
UNL - WILLBORNCH - 16
DESERT PALACE, INC. v. COSTA United States Supreme Court 123 S. Ct. 2148 (2003) Justice THOMAS delivered the opinion of the Court. The question before us in this case is whether a pla
UNL - WMF - 2
WMF2EPS: A Windows Metafile Converter for Windows 95/98/ME, Windows NT4.0, 2000, XP-Version 1.32, 24-Aug-2002Author: Wolfgang Schulter EMail: wmf2eps@gmx.de Homepage: http:/www.wmf2ep
Cornell - CS - 211
Nested and Inner classes Reading for these lectures: Weiss, Section 15.1 (Iterators and nested classes), Section 15.2 (Iterators and inner classes). ProgramLive, Section 12.48-queens solution /* For each i, 0 <= i < b.length(), queen in row i is in
Cornell - CS - 211
CS211 About Prelim 1The prelim is 7:30-9:00PM, Thursday, 11 March 2001, Uris Auditorium The only reason for not taking it then is that you have a conflict with another evening prelim. If this is the case, please let Gries know by Sunday evening, 7 M
Cornell - CS - 17
public class ListRecursion { public static void main(String[] args) {List2 list = new List2(); list.display();list.add("A"); list.display();list.add("B"); list.display();list.add("C"); list.display();list.del("A"); list.display(
Cornell - CS - 211
public class ListRecursion { public static void main(String[] args) {List2 list = new List2(); list.display();list.add("A"); list.display();list.add("B"); list.display();list.add("C"); list.display();list.del("A"); list.display(
UNL - APETERSON - 1
Math 106 Honors (Quiz 6) Make sure you show all your work!Name.1. (4 points) (no calculator) Find the solution of the differential equation y = 3 sin x - 4 cos x that satisfies y() = 5.2. (5 points) (no calculator) Find all antiderivatives of
UNL - APETERSON - 1
Math 106 Honors (Quiz 9) Make sure you show all your work! 1. (20 points) Evaluate the following integrals: (a) xe4x dxName.(b)1 2x2 -4x+52dx(c)x2 ex dx3(d) 1 9-x2dx(e)x8 ln x dx
UNL - CROPTECHNO - 2005
Water Potential in Plants=+The slide set is divided into two parts.Part one investigates the significance of water potential in plants and explains the equation for estimating water potential in plants.Part IWhat is Water Potential? I
UNL - CROPTECHNO - 2005
WSSA Site of Action and Classification Number: 1 2 3 4 5 6 7 8 9 10 12 13 14 15 22 28 ACCase = acetyl-CoA carboxylase inhibitor ALS = acetolactate synthase inhibitor MT = microtubule assembly inhibitor GR = growth regulator PSII(A) = photosystem II,
UNL - CROPTECHNO - 2005
GranitePage 1 of 2Graniteimage:rock type igneous distinguishing features completely crystallized, large, well formed interlocking crystals vis eye, no preferred crystal orientation, fairly light in color (white, gra main minerals quartz, feld
UNL - CROPTECHNO - 2005
Official Series Description - BAYAMON SeriesLOCATION BAYAMON Established Series Rev. GRB 08/1999PRBAYAMON SERIESThe Bayamon series consists of very deep, well drained, very slowly permeable soils on coastal plains interspersed among limestone
UNL - CROPTECHNO - 2005
Official Series Description - HOLDREGE SeriesLOCATION HOLDREGE Established Series Rev. CWL, LGR, RRZ 10/2002NE+KS OKHOLDREGE SERIESThe Holdrege series consists of very deep, well drained, moderately permeable soils formed in calcareous loess.
UNL - CROPTECHNO - 2005
Official Series Description - HOUSTON_BLACK SeriesLOCATION HOUSTON BLACK Established Series Rev. CLN:ACT:JMG 02/97TXHOUSTON BLACK SERIESThe Houston Black series consists of very deep, moderately well drained, very slowly permeable soils that f
UNL - CROPTECHNO - 2005
Official Series Description - THREEBEAR SeriesLOCATION THREEBEAR Established Series Rev. GAH-AR-JAL 05/2005IDTHREEBEAR SERIESThe Threebear series consists of moderately deep to a fragipan, moderately well drained soils formed in loess and rewo
UNL - CROPTECHNO - 2005
UNL - CROPTECHNO - 2005
Official Series Description - CECIL SeriesLOCATION CECIL Established Series Rev. AG:BJW 9/97NC+AL GA SC VACECIL SERIESThe Cecil series consists of very deep, well drained moderately permeable soils on ridges and side slopes of the Piedmont upl
UNL - CROPTECHNO - 2005
Lava fountain and lava flows on Pu`u `O`o, Kilauea Volcano, Hawai`iPhoto InformationPhotograph by J.D. Griggs on June 2, 1986Braided lava flows spread from a lava fountain on the side of Pu`u `O`o cone, located on the southeast rift zone of Kil
UNL - CROPTECHNO - 2005
SandstoneSandstoneimage:rock type sedimentary distinguishing features made up of relatively coarse particles, which can often be seen without a hand lens. feels gritty, like sandpaper, can see sedimentary structures, such as layering, fossils e
UNL - CROPTECHNO - 2005
ShaleShaleimage:rock type sedimentary distinguishing features very fine grained, composed of clay-sized minerals, often breaks into platy fragments, some contain fossils main minerals quartz, clay minerals weathering behavior small particle siz
UNL - CROPTECHNO - 2005
BasaltGneissimage:rock type metamorphic distinguishing features completely crystallized, crystals visible with the naked eye, but anisotropic pressure during crystallization leads to a preferred orientation of many newly formed minerals, which
UNL - CROPTECHNO - 2005
GraniteGraniteimage:rock type igneous distinguishing features completely crystallized, large, well formed interlocking crystals visible to the naked eye, no preferred crystal orientation, fairly light in color (white, gray, pink). main minerals
UNL - CROPTECHNO - 2005
Official Series Description - DRUMMER SeriesLOCATION DRUMMER Established Series Rev. JBF-JDA-TJE 10/2001IL+IN OH WIDRUMMER SERIESThe Drummer series consists of very deep, poorly drained soils formed in loess or other silty material and in the
UNL - CROPTECHNO - 2005
Official Series Description - DOUGH SeriesLOCATION DOUGH Tentative Series Rev. BWC/GB 03/1999CODOUGH SERIESThe Dough series consists of shallow, well drained soils that formed in residuum from sandstone. Dough soils are on mesa tops and benche
UNL - CROPTECHNO - 2005
coalPeat / Coalpeatlignitebituminousanthraciterock type sedimentary / metamorphic depending on degree of alteration distinguishing features dark colored, low density, can contain fossils main minerals carbonised plant remains - not a mine
UNL - CROPTECHNO - 2005
Official Series Description - PAXTON SeriesLOCATION PAXTON Established Series Rev. MFF-SMF 09/2004CT +MA NH NY RI VTPAXTON SERIESThe Paxton series consists of well drained loamy soils formed in lodgement till. The soils are very deep to bedroc
UNL - CROPTECHNO - 2005
slateSlateimage:rock type: metamorphic distinguishing features: very fine grained rock, often easily split into thin plates, surfaces often shiny due to formation of preferentially oriented metamorphic minerals (see schist). The boundary betwee
UNL - CROPTECHNO - 2005
Official Series Description - MARLOW SeriesLOCATION MARLOW Established Series Rev. SALP-SHG-CAW 07/2001NH+MA ME NY VTMARLOW SERIESThe Marlow series consists of well drained soils that formed in loamy till on drumlins and glaciated uplands. The
UNL - CROPTECHNO - 2005
Official Series Description - MENFRO SeriesLOCATION MENFRO Established Series Rev. RWF-RLT 08/2004MO+ILMENFRO SERIESThe Menfro series consists of very deep, well drained, moderately permeable soils formed in thick loess deposits on upland ridg
UNL - CROPTECHNO - 2005
BasaltBasaltimage:rock type igneous distinguishing features completely crystallized, but very small crystals generally invisible to the naked eye, black or very dark gray in color, sometimes contains gas bubbles (as shown in image above), weath
UNL - CROPTECHNO - 2005
GabbroGabbroimage:rock type igneous distinguishing features completely crystallized, large crystals, easily visible with the naked eye, dark in color main minerals plagioclase feldspar, olivine, pyroxene weathering behavior large crystals gener
UNL - CROPTECHNO - 2005
Official Series Description - PENISTAJA SeriesLOCATION PENISTAJA Established Series Rev. JJF/RJA/LWH/SAZ/WWJ 04/2002NM+AZPENISTAJA SERIESThe Penistaja series consists of very deep, well drained, moderately permeable soil that formed in mixed a
UNL - CROPTECHNO - 2005
Official Series Description - YAGGY SeriesLOCATION YAGGY Established Series Rev. RMM, PRF, JCW 08/2003KSYAGGY SERIESThe Yaggy series consists of very deep, somewhat poorly drained soils on flood plains in river valleys of the Great Bend Sand P
UNL - CROPTECHNO - 2005
Class Notes - Geology 101 Rock IPage 1 of 1Class Notes - Geology 101 Rock IdentificationIgneos rocks formed through crystallization from molten rock. Slow cooling of magma deep below the earth's surface causes coarse crystalline rocks with cryst
UNL - CROPTECHNO - 2005
Parent Material and Soil FormationCreated by Jim Ippolito & Mike Hanna College of Agricultural Sciences Colorado State UniversityNext1 283 5 46 7Click here to endColluvium Photo: Source: http:/pubs.usgs.gov/of/2002/of02-437/gallery.htm
UNL - CROPTECHNO - 2005
Parent Material and Soil FormationCreated by Jim Ippolito & Mike Hanna College of Agricultural Sciences Colorado State UniversityNext1 283 5 46 7Click here to endColluvium Photo: Source: http:/pubs.usgs.gov/of/2002/of02-437/gallery.htm
UNL - CROPTECHNO - 2005
2 2 P = G
UNL - CROPTECHNO - 2005
Experiment Summary Statements1) The mutagen applied to the truebreeding seed induced phenotype variations in the soybeans. 2)The mutagen induced mutations (changes) in the genetic makeup of the plant which were passed on to offspring, and thus the u
UNL - CROPTECHNO - 2005
Class Notes - Geology 101 Rock IPage 1 of 1Class Notes - Geology 101 Rock IdentificationIgneos rocks formed through crystallization from molten rock. Slow cooling of magma deep below the earth's surface causes coarse crystalline rocks with cryst
UNL - CROPTECHNO - 2005
Table 1.1.Classification scheme for soils (Soil Survey Staff, 1975)TaxonomiclevelNumberof classesExamples(Abbreviations)Order10Alfisol (alf) deciduous forestAridisol (id) dry/arid, desertEntisol (ent) beginning: no horizonHistosol (
UNL - CROPTECHNO - 2005
Table 1.4.Series descriptions for Holdrege, Nora, Sharpsburg and Valentine soilsHoldrege SeriesThe Holdrege series consists of deep, well-drained, nearly level to moderately sloping soils formed in loess on uplands.In a representative profile t
UNL - CROPTECHNO - 2005
TopographyIts Influence on drainage, organic matter accumulation, and profile developmentNext1253 4Click for final slide1 This soil developed on the hilltop which is relatively flat. Therefore the soil is relatively deep and well drai
UNL - CROPTECHNO - 2005
TopographyIts Influence on drainage, organic matter accumulation, and profile development1253 4Click on a number to look at the soil profile.Summary1 This soil developed on the hilltop which is relatively flat. Therefore the soil is
UNL - CROPTECHNO - 2005
(phyllite) schistSchistimage:rock type: metamorphic distinguishing features: often distinct foliation fabric due to preferred alignment of newly formed minerals, such as muscovite. Novices sometimes confuse foliation with sedimentary layering,
UNL - CROPTECHNO - 2005
UNL - CROPTECHNO - 2005
Soil Series 122Winter 1986NITROGEN CARBON TRANSFORMATION IN SOIL (NCSOIL) USER'S GUIDE BY J.D. HASKETT J.A.E. MOLINA C.E. CLAPPThe University of Minnesota, including the Agricultural Experiment Station, is committed to the policy that all perso
UNL - B - 2009
AMC's Math MessengerWHAT:WHO: WHen: WHeRe: WHy:Fall 2008 - SpecialColleges/Universities administering the MAA's AMC 10/12 ContestInstitutions of Higher education hosting High school Math students WednesdAy, February 25, 2009 your College or Un
UNL - B - 1
2003 AMC 8 Teacher Nomination Form for theEDYTH MAY SLIFFE AWARDfor Distinguished Junior High/Middle School Mathematics TeachingOnly one name may be submitted from a 2003 AMC 8 registered school and it should be the mathematics teacher who has be
UNL - SCOHN - 08
Second-Order, Linear Equations 1 1. A second-order, linear ordinary dierential equation is one of the form (t)u + (t)u + (t)u = f (t). (1)We assume that (t) = 0 for t in an open interval I. We can thus write the equation as u + p(t)u + q(t)u = g(t)
UNL - SCOHN - 1
Second-Order, Linear Equations 1 1. A second-order, linear ordinary dierential equation is one of the form (t)u + (t)u + (t)u = f (t). (1)We assume that (t) = 0 for t in an open interval I. We can thus write the equation as u + p(t)u + q(t)u = g(t)
UNL - MATH - 2
Math 203 Review for Exam II Your second exam covers Chapters 5-8 of your textbook. This review sheet is meant to help you, but is not meant to be a substitute for studying from the book. In particular, I have tried to include all the topics we cover
UNL - MATH - 203
Math 203 Review for Exam II Your second exam covers Chapters 5-8 of your textbook. This review sheet is meant to help you, but is not meant to be a substitute for studying from the book. In particular, I have tried to include all the topics we cover
UNL - MATH - 314
Second Test, Math 314: Linear Algebra. 1. (20 points) Let A an 5 5 matrix. Assume that 2 0 0 2 D= 0 0 0 0 0 0 and 1 2 1 0 0 0 2 0 1 1 A = P -1 DP , where 0 0 0 0 0 0 3 0 0 0 4 0 0 0 4 1 0 1 0 0 0 2 0 0 1 1 0 0 0 2 P = (a) Wri
UNL - MBRITTENHA - 2
Statistics is all about drawing conclusions about the opinions behavior structure of large populations based on information about a relatively small part of that population, called a sample. Samples can be gathered in a variety of ways: Convenience s