Rtllq Rer,L N T ~Red 1 N Lie1/~

Total Page:16

File Type:pdf, Size:1020Kb

Rtllq Rer,L N T ~Red 1 N Lie1/~ AJ,PHAllF.TICAJ, I,lIlT "F BI RTllq Rer,l n t ~red 1 n lIe1/~. en f or the Yeo.r 1919 ·-~---------'---~~------B-(-O-on-t-.-) -- r:. - (oont) _c_ (oent.) --P- D'InnooAnze. Paele 11761 , (q.b~ta:jf:·fe"']!,~ii #~~~ Brine. 0onAtlln~e I,ouloe 11812 Ceffin.r.ladya EIAie #549 587 828 DipI1.squ'lle. An tonio 356 I Abbott. ~obert cuoker 586 Bredriok. ~hirlcy norethy r.ognwell. Jehn Alfred Jr ]1i'laatll. Eleanor Angela 324 'I 339 14 Ac~ettullo.Leonllrdo Antoni0696 Rrooka. Arthur'lernllrd Cehen. ~ylvia Beatrioe D1Zaoomo. Mary 480 AdamA. J,I111an FranaeR 474 llrookA. Pl1ul JT 156 cole. Oarl F.dlAen 515 906 Dodge. Gardner Murray 162 Ad'tmo. Rioho.rd Phillip 450 Brothera. Alioe Josephine Cole. Esther Winifred 291 Dedge. lIatlllie 373 Adoook.r,eerge Vlll11am 75 BreNn. Ann Hayward 684 Coleman. J.ouine 400 Dehorty. Jumeo Frllnois 235 \ Al'.l'y, 1lar.dy Rmith 209 Bro'"n. AUDtln CowleD .Tr 438 Collelli. Maria Oonatanza 27 Delan. James Anthony 129 ~Ahllronian. Sara" 385,. -own. Chllrlee Frederiek h 891 Celline. Anna Margaret 83 Donahue. William Hareld 300 Albllno. '!'rnnk .ToBoph 795:!h own. ~or""lia 1'I00ttan 831 Collins. Elaie 136 Donlan. Edward 62 Allp.~. o,h~rlee 7heo~ ere 554 Bro'lln. nore 'hy Leuine 434 Cellin". Riohard 629 Donnelly. :tildred Virginia 641 Allen.,Teremla;' !!ervln Jr 925 Bre'lln. ;furiel Fnrn~'IIorth 318 celllns. Virginia 33 Dorney. William Andre'll Jr 145 796 A11M. lIoel 807 Bre'lIn, Peter Crosby Cellins. Will lam Henry 451 Downey. Charles Fredr1~k 391 18 Allle. Ava 469 llre':m. Robert I,eBarren CempoBto. Jeneyh 723 DeNney. Katherine Fl~ming 102 Altieri. Albert JOA"pll 945 BreNn. "ltllnl~y Fairhllnke 415 Ceneooff. Morria 640 Doyle. Murtha I,01l19a 0113 Amp.n~ol:l. J,et~lnll 743 Brynon. ~hll"leo WllAen 127 Conley. Margaret Mary 270 Drapen. EmerAon 92 An~rea. .To.net,!Aar~uer1te 914 Arthur 1':d"llrd 79 Buok • Connelly. Helen Marie 76 Dr1'l~ol1. 1!arg(\ ret Anne 9'/5 Andre'll" ••- 4 lluokley. Allee Mllrtha 648 Cennolly. John Franoi" 44 Dug~u. Vincent Joaoph 2'/4 Andrews. olernllrd HUMell Jr349 llurke. Francla Joseph 540 Cenra~. llarbara Rit~ 964 180 nuggan. Corneliuo 614 Andre:"n.Co',rlea Vllnl;hrop 677 Burke. Henry .Toseph ~onrad. walter 1Iorman 982 Dug,,,,,n. wi11illm James 439 926 Andre~". Leonor~ 8a llurke, Mildred CenAidino. Mary Katherine 101 Duke. Alioo 462 AnneBe.Antolnette "lerp.noe 307 Burke. ")(llter FrllMi. 458 Ceeper. Elizabeth 78 tunmore. PrlD~illa Anne 689 Anneap.. Pletro 751 Burkholder. Dorothy !lay 939 Cooper. JameR Henry 147 48 Dun"". Edwnrd Robert 067 Anziovine. F.n1'loo 166 Burley (Rtillborn) Ceeper. RUBAel1 p.lllett 486 Dupuis. (StHl bc rn) 793 Arduino •.Toaoph 781 llurns. nen~ld llryee 839 Cerbett. Mary 1':llzaheth 266 777 Dupui". P~uline Rena 601 Armltlllt,e (Rt1l1born) 57 BurnA. Dero~hy Ed'llin'-l Corbett. Wlll11tm 1I0rton 421 n'Urbano. Antonio 512 Arnold, Cen"tnn~e 478 Burn". Jehn Charles 277 Cereor'ln. Mary M,~rg:tret 332 Durell. Alfre~ yp.ll~_,d 610 A"h~; on. Ruth 876 BurnA. John ThomnB 3rd 460 Corlis,. WHY Eleaner 783 883 Durkee. Viola Er1i th 108 Atkin~on. Dean Wesley 360 Burn~. lflry J!:llzl1beth Cormier. :ToBeph ArthuT 40 n,vyer. John 832 Atkinsol1. Eleanor RegerB 197 BurnA. Ruth Elizabeth 485 Cerney. ~"eAtsr 1.1 bert Jf 406 88 D,'lyer. Mo.rg~ret 829 AtNood. Bonnar Clarke 303 Butte!'B. Philip Whi teomb COU,lhlan. Charlea J!:r"est Jr 873 nllyer. Paul l1a thaniP.l ·129 Au~ein. Dora Annle 613 :Juttdek.Herbert IngerBell Jr 70 craig. Oeerge Pario 243 BUt.tA. Frederic HarrIngton 2nd 760 Cl'am. Bally 834 Crllndoll. Frederiok Jameo 577 Cr!~nton. Rebert Hoy Jr 222 _B_ Crioaey. l!url'1ng~,on Edgar 372 Crenin. Fr~nola Norm~n 498 Eagan. 1!a ry Jane #340 Bacoari. Riagie 668 Cronin. Joseph B'wten 755 Eago.n. Phillip 924 Bacoari. Luolllne 1 Crenin. ReMmary 902 Earle. Prudonee Ida 904 Baeon • .Teaiah F.aten 2nd 951 Cadmnn 304 Cronkhite. Leeno.rd \'Iolocy 3rd Eokert (Stillborn) 649 oaker. Derethy 987 Cafarelli. r,iev~nn1 461 287 Eekert. I rene Ji;l1za beth 351 Baldwin. lIorm." Wheeleok 35 CalkinB. Patrioia 173 Cresby. John Wesley 520 Edgarton. Cnarles Gardner Jr 100 llllnal'oft. :larh'lra Hale 895 Callanan, James FAward 745 Crosby. Margaret Elellnor 73 FAward". Prlsoilla 37 Banoroft. ~linor 390 C1lmp\1·,11. .Teaeph Aloyaius 323 Crewell. Alan 516 F.gan. r~la deD Fr~ncie 774 Bandlerll. I,avrronoe Hamil ton Cannon. William F.dvlllrd 624 Cugini. Carmiella 798 F.ggle"ton. Margaret Mary 239 907 Capell o. Albert 404 x Curtio, Bel!trioe /.\ury 685 Elliott. Frederie.k 282 ilanker -:i'i2..worl'flv 958 r.4p~ll c. .Tehn 405 cutter. Thelma 993 B11io. Hercort 319 Barbed o. l,eu~" 58 Capone 740 x Curran. nertrude 7 F.llis. Kenneth 93B Baringer. 1{on~y Jay Jr 31'd 316 Caperale. Vlrgilia 508 Enego~R. Phllip 392 BariBane. I,uoia 505 Callrio~ 10.. I.e"i B Frllnk 703 Eng. Virginla 572 Harker. 0eoily 'lelen 523 Capstiok. Rloh/lTd Barton ,Tr 636 .JL Bne. Irene M"ry 556 llarker. Hareld 787 Cardillo. Mary nraoe 816 l1rio"ol1. Frederick Geerge 152 llarker. Harl'let LoulDe 4G5 Ca rey. JameB /.\et :'i a 290 nalieandro.Dominio 310 P.rnat 164 Barner. James Robert 628 778 Cnrey. Rebert Paul Dane. ~lerbert Phillip 969 F.~b.breek. Frederiek Reed 845 llflrret t, :lailey Murgll.troyd 722 Carlet.on. Graoe r'trel1ne 579 n'Angelo. Clllrenoe 273 1':yrl" Helen 334 Barrett. MarR,net 1':l1z"beth 87 Cllrley. Vial ter .ToBeph 930 n~nielR.11:d'1I1n Ashton 720 Thlrry. 00nntunee 8B3 Carlin~. Albert F.rnBst 608 ])'~niela on. !lert I.ind".'l.r~ 314 Barry. .rohn 201 Caron. Edna 493 ll'Antonio.Cenoe3io 562 Barry. ,alph Allen Jr 333 Cnrter. M~rgaret 78a D'Attl1io,I,ina Bi~nea Maria 227 Bartl~y. Robert David 736 Caruso. Antonio nust,lvO 302 Dilu. 'lay Rpeoner 784 BateR. John 749 C'lrune. Pllul1ne 81 navia. norothy 658 Fallon. John Fr'lneie 525 Batey. Arthur .Tames 226 Carvelli. Vinoenzo 276 Davi". Ethal Vlr"ini~ 265 Farrar. Jllmea Edward 936 Baxter. 1.a'/lren06 J~mee 82 Cashman. Beatrice 766 naViA. Jean 119 Farrell. Edward 410 lleale, David PO'llars 754 Cav~nagh. Lila Jeeephine 36 I),\Y. '!'rededok LewiB 491 F~rrell. Joscph Juliuo 103 lleattiA.Mary Leuioe Judge 389 Ced \'OI1~, Donate 269 nay. Vl rgl nia 550 Farrell. Marjerie J,ouiBe 232 Benaon. Elizllbeth 91 Cedrone. Giovanni 71 DeAngolis. Franoesoo 279 FUl'rineten. Ilorothy 817 BcnAon.Marguerite Helen 981 Ces,trOntl. ,'elloe 769 Dearbern, Charleo Henry 21 Faulkner. Bsverley Je'~nette 292 Bentlev.John Melvin Jr 941 Cotrone. Denat~ Preaea 490 DeBourke, Riohard 931 Feather. Barelay 354 Benyon. Jellnette 170 Cetron.,. ()ui~o 678 neokor. Myrtle Marie 803 Federico.. Anna 673 Benyen. Marion 169 Chamber1ctj n. F.d'Uard LaN!'onee 950 Degen(Stillbern) 309 Feeley. Aliee Gertrude 362 Benzaquin. Richard Albert 952 Champagne. Camille nerald 590 Delanoy. noorge Paul 1;93 Feeley, CharleB Ed'llIIrd 50 Beruhe. Mary 983 eh"n Her 571 Del"ne.,. Helen Marie 151 Feeley. Jehn Joseph 72Li Bost. 1':liz" beth 874 Ch(ln~ler. JameR F.dvlflrd 49 DeLueEl'. Ua ria Del era til 545 Feldhoff. Ilnrharn DeForest 732 Bielaki. Amella 901 Ch'~ncllel'. Joan !\artlett 692 DeI.uoe. 'Iunzie 01aoomo 1~1 Fennelly. Orrorge Harria 187 llin:elow. Ervin flonior 161 Chllrette. Rebert Oll~er 542 DeUalo. Giovanni 5 Fer~uAon. Eli~ubeth Clnrk 555 lliroh. T,eul Ae Wad"worth 589 Charin. Josoph l' 174 Demere. Jeseph lI,ugene Adel~rd "er{,uaen. J!:ve1yn Claire 920 I Black. 1':ilesn 220 Ch~rlton. Robert Wallio 802 428 "orgueon. John Joseph 591 Blaiadoll.1':lizabeth Al· 475 Chan~. P.leanor Williston 483 DeMiohele, Idll Anr-olEl 687 Forno.ld. Frl~nces HUDAell 877 frp,ida ChllBO. 11:mlly Caroline 409 Dempsey. Mtlrtin 256 Fe~nenden. Luoi1e 869 lllodgett. Barbara warren 53 Chllao, Hr.<reld Rohert 682 DeRosl!et, Frederiok tl~oh Jr 234 J'l.kot~. Natll1ie 918 , Hlood. Henry Wl nthrop 126 Cheney. Oharles Willl/lm 2nd 955 Deflantis. GiorgIo 511 File. Tunker 472 Bleo~. Marion 1':thel 646 ChiaeJhia. Domlniak 338 lle~l.\nt1 a, Umbert 596 ,'l1lien, Antolne Leon Jr 630 llleom. ll!l.rney 457 '~1:lno. JOBP.llhl ns 530 Desrosiers, F.dwal'd I.oul." 665 F! "her. Janet Kondall 695 neaoabAllo.Demnni~e 221 r.in~etta, r.ievanino 1181 Ilearoohere. Loule !len.lllmin 176 go 1 Flnke. Hohn lAarie Bontempo, 'l1~ela 683 ~ivotto. Florenoe 715 DeAtefu.ne, 1Iioholus 7u8 Fitzgerald, Mary 85 llont~mpe. Patrl~k 250 r.iv~tto. Ml.tda caterino 95 DeRteph,C1no. r,lovannin(\ 546 Fitzgerald, Themas Clement 526 llorten. Clement Vlio"oll 251 CIa rk. Jean 92 DeWolf. lI.~ry 1':",ily 770 Fletoher. Jehn Ruanell 771 Tle~ten, F.l1zllbeth Helen 773 Cla rk, Owen Rohert ~en 83 DiCarlo.. Jllmoe ~eol1dg' 694 Fl1Mhhaul'(h, Rodn''ln Ferreat 592 Bou.hie, Annle Rltll 699 Clllrk, !'i~hard llrevler 80 Diefenderf.Janette ro,' ,ott 419 Fegg. Rebert Ells'llortll 837 Tloudrot. Phillip BrnDat 39B r1o.y+,e;1. Rdna Dorot.hy (;3 Dinian 1emeni~0. Lnurina 580 ,,50 Fogg. walter Atarolrd •• r 836 Bouzan. EdvlIlrd ClohenRY. Inez lI~ry 52 lliLeffi. r,iuoeppa 594 Feley. J'llme" Au"uotine Jr 896 noyn~on,)!.arg'lret ,Bro'lln 866 Cluno. Marle 11:velyn 93 Dilworth, .Tulia Florenoe 435 Follanob<1o.
Recommended publications
  • Full-Waveform Inversion of Gpr Data from the Thur River Aquifer
    FULL-WAVEFORM INVERSION OF GPR DATA FROM THE THUR RIVER AQUIFER Published in Near Surface Geophysics: Klotzsche, A., van der Kruk, J., Meles, G. A., Doetsch, J., Maurer, H., and Linde, N., 2010, Full-waveform inversion of cross- hole ground-penetrating radar data to characterize a gravel aquifer close to the Thur River, Switzerland: Near Surface Geophysics, 8, 635-649. 0 Full-waveform inversion of GPR data from the Thur River aquifer ABSTRACT Crosshole radar tomography is a useful tool for mapping shallow subsurface electrical properties viz. dielectric permittivity and electrical conductivity. Common practice is to invert crosshole radar data with ray-based tomographic algorithms using first arrival traveltimes and first cycle amplitudes. However, the resolution of conventional standard ray-based inversion schemes for crosshole ground penetrating radar (GPR) is limited because only a fraction of the information contained in the radar data is used. The resolution can be improved significantly by using a full-waveform inversion that considers the entire waveform, or significant parts thereof. A recently developed 2-D time-domain vectorial full-waveform crosshole radar inversion code has been modified in the present study by allowing optimized acquisition setups that reduce the acquisition time and computational costs significantly. This is achieved by minimizing the number of transmitter points and maximizing the number of receiver positions. The improved algorithm was employed to invert crosshole GPR data acquired within a gravel aquifer (4 - 10 m depth) in the Thur valley, Switzerland. The simulated traces of the final model obtained by the full-waveform inversion fit the observed traces very well in the lower part of the section and reasonably well in the upper part of the section.
    [Show full text]
  • Stocking Measures with Big Salmonids in the Rhine System 2017
    Stocking measures with big salmonids in the Rhine system 2017 Country/Water body Stocking smolt Kind and stage Number Origin Marking equivalent Switzerland Wiese Lp 3500 Petite Camargue B1K3 genetics Rhine Riehenteich Lp 1.000 Petite Camargue K1K2K4K4a genetics Birs Lp 4.000 Petite Camargue K1K2K4K4a genetics Arisdörferbach Lp 1.500 Petite Camargue F1 Wild genetics Hintere Frenke Lp 2.500 Petite Camargue K1K2K4K4a genetics Ergolz Lp 3.500 Petite Camargue K7C1 genetics Fluebach Harbotswil Lp 1.300 Petite Camargue K7C1 genetics Magdenerbach Lp 3.900 Petite Camargue K5 genetics Möhlinbach (Bachtele, Möhlin) Lp 600 Petite Camargue B7B8 genetics Möhlinbach (Möhlin / Zeiningen) Lp 2.000 Petite Camargue B7B8 genetics Möhlinbach (Zuzgen, Hellikon) Lp 3.500 Petite Camargue B7B8 genetics Etzgerbach Lp 4.500 Petite Camargue K5 genetics Rhine Lp 1.000 Petite Camargue B2K6 genetics Old Rhine Lp 2.500 Petite Camargue B2K6 genetics Bachtalbach Lp 1.000 Petite Camargue B2K6 genetics Inland canal Klingnau Lp 1.000 Petite Camargue B2K6 genetics Surb Lp 1.000 Petite Camargue B2K6 genetics Bünz Lp 1.000 Petite Camargue B2K6 genetics Sum 39.300 France L0 269.147 Allier 13457 Rhein (Alt-/Restrhein) L0 142.000 Rhine 7100 La 31.500 Rhine 3150 L0 5.000 Rhine 250 Doller La 21.900 Rhine 2190 L0 2.500 Rhine 125 Thur La 12.000 Rhine 1200 L0 2.500 Rhine 125 Lauch La 5.000 Rhine 500 Fecht und Zuflüsse L0 10.000 Rhine 500 La 39.000 Rhine 3900 L0 4.200 Rhine 210 Ill La 17.500 Rhine 1750 Giessen und Zuflüsse L0 10.000 Rhine 500 La 28.472 Rhine 2847 L0 10.500 Rhine 525
    [Show full text]
  • Karte Der Erdbebenzonen Und Geologischen Untergrundklassen
    Karte der Erdbebenzonen und geologischen Untergrundklassen 350 000 KARTE DER ERDBEBENZONEN UND GEOLOGISCHEN UNTERGRUNDKLASSEN FÜR BADEN-WÜRTTEMBERG 1: für Baden-Württemberg 10° 1 : 350 000 9° BAYERN 8° HESSEN RHEINLAND- PFALZ WÜRZBUR G Die Karte der Erdbebenzonen und geologischen Untergrundklassen für Baden- Mainz- Groß- Main-Spessart g Wertheim n Württemberg bezieht sich auf DIN 4149:2005-04 "Bauten in deutschen Darmstadt- li Gerau m Bingen m Main Kitzingen – Lastannahmen, Bemessung und Ausführung üblicher Freudenberg Erdbebengebieten Mü Dieburg Ta Hochbauten", herausgegeben vom DIN Deutsches Institut für Normung e.V.; ub Kitzingen EIN er Burggrafenstr. 6, 10787 Berlin. RH Alzey-Worms Miltenberg itz Die Erdbebenzonen beruhen auf der Berechnung der Erdbebengefährdung auf Weschn Odenwaldkreis Main dem Niveau einer Nicht-Überschreitenswahrscheinlichkeit von 90 % innerhalb Külsheim Werbach Großrinderfeld Erbach Würzburg von 50 Jahren für nachfolgend angegebene Intensitätswerte (EMS-Skala): Heppenheim Mud Pfrimm Bergst(Bergstraraßeß) e Miltenberg Gebiet außerhalb von Erdbebenzonen Donners- WORMS Tauberbischofsheim Königheim Grünsfeld Wittighausen Gebiet sehr geringer seismischer Gefährdung, in dem gemäß Laudenbach Hardheim des zugrunde gelegten Gefährdungsniveaus rechnerisch die bergkreis Höpfingen Hemsbach Main- Intensität 6 nicht erreicht wird Walldürn zu Golla Bad ch Aisch Lauda- Mergentheim Erdbebenzone 0 Weinheim Königshofen Neustadt Gebiet, in dem gemäß des zugrunde gelegten Gefährdungsniveaus Tauber-Kreis Mudau rechnerisch die Intensitäten 6 bis < 6,5 zu erwarten sind FRANKENTHAL Buchen (Odenwald) (Pfalz) Heddes-S a. d. Aisch- Erdbebenzone 1 heim Ahorn RHirschberg zu Igersheim Gebiet, in dem gemäß des zugrunde gelegten Gefährdungsniveaus an der Bergstraße Eberbach Bad MANNHEIM Heiligkreuz- S c Ilves- steinach heff Boxberg Mergentheim rechnerisch die Intensitäten 6,5 bis < 7 zu erwarten sind Ladenburg lenz heim Schriesheim Heddesbach Weikersheim Bad Windsheim LUDWIGSHAFEN Eberbach Creglingen Wilhelmsfeld Laxb Rosenberg Erdbebenzone 2 a.
    [Show full text]
  • Quaternary Glaciation History of Northern Switzerland
    Quaternary Science Journal GEOzOn SCiEnCE MEDiA Volume 60 / number 2–3 / 2011 / 282–305 / DOi 10.3285/eg.60.2-3.06 iSSn 0424-7116 E&G www.quaternary-science.net Quaternary glaciation history of northern switzerland Frank Preusser, Hans Rudolf Graf, Oskar keller, Edgar krayss, Christian Schlüchter Abstract: A revised glaciation history of the northern foreland of the Swiss Alps is presented by summarising field evidence and chronologi- cal data for different key sites and regions. The oldest Quaternary sediments of Switzerland are multiphase gravels intercalated by till and overbank deposits (‘Deckenschotter’). Important differences in the base level within the gravel deposits allows the distin- guishing of two complex units (‘Höhere Deckenschotter’, ‘Tiefere Deckenschotter’), separated by a period of substantial incision. Mammal remains place the older unit (‘Höhere Deckenschotter’) into zone MN 17 (2.6–1.8 Ma). Each of the complexes contains evidence for at least two, but probably up-to four, individual glaciations. In summary, up-to eight Early Pleistocene glaciations of the Swiss alpine foreland are proposed. The Early Pleistocene ‘Deckenschotter’ are separated from Middle Pleistocene deposition by a time of important erosion, likely related to tectonic movements and/or re-direction of the Alpine Rhine (Middle Pleistocene Reorganisation – MPR). The Middle-Late Pleistocene comprises four or five glaciations, named Möhlin, Habsburg, Hagenholz (uncertain, inadequately documented), Beringen, and Birrfeld after their key regions. The Möhlin Glaciation represents the most extensive glaciation of the Swiss alpine foreland while the Beringen Glaciation had a slightly lesser extent. The last glacial cycle (Birrfeld Glaciation) probably comprises three independent glacial advances dated to ca.
    [Show full text]
  • Rare Earth Elements As Emerging Contaminants in the Rhine River, Germany and Its Tributaries
    Rare earth elements as emerging contaminants in the Rhine River, Germany and its tributaries by Serkan Kulaksız A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geochemistry Approved, Thesis Committee _____________________________________ Prof. Dr. Michael Bau, Chair Jacobs University Bremen _____________________________________ Prof. Dr. Andrea Koschinsky Jacobs University Bremen _____________________________________ Dr. Dieter Garbe-Schönberg Universität Kiel Date of Defense: June 7th, 2012 _____________________________________ School of Engineering and Science TABLE OF CONTENTS CHAPTER I – INTRODUCTION 1 1. Outline 1 2. Research Goals 4 3. Geochemistry of the Rare Earth Elements 6 3.1 Controls on Rare Earth Elements in River Waters 6 3.2 Rare Earth Elements in Estuaries and Seawater 8 3.3 Anthropogenic Gadolinium 9 3.3.1 Controls on Anthropogenic Gadolinium 10 4. Demand for Rare Earth Elements 12 5 Rare Earth Element Toxicity 16 6. Study Area 17 7. References 19 Acknowledgements 28 CHAPTER II – SAMPLING AND METHODS 31 1. Sample Preparation 31 1.1 Pre‐concentration 32 2. Methods 34 2.1 HCO3 titration 34 2.2 Ion Chromatography 34 2.3 Inductively Coupled Plasma – Optical Emission Spectrometer 35 2.4 Inductively Coupled Plasma – Mass Spectrometer 35 2.4.1 Method reliability 36 3. References 41 CHAPTER III – RARE EARTH ELEMENTS IN THE RHINE RIVER, GERMANY: FIRST CASE OF ANTHROPOGENIC LANTHANUM AS A DISSOLVED MICROCONTAMINANT IN THE HYDROSPHERE 43 Abstract 44 1. Introduction 44 2. Sampling sites and Methods 46 2.1 Samples 46 2.2 Methods 46 2.3 Quantification of REE anomalies 47 3. Results and Discussion 48 4.
    [Show full text]
  • Internationally Coordinated Management Plan 2015 for the International River Basin District of the Rhine
    Internationally Coordinated Management Plan 2015 for the International River Basin District of the Rhine (Part A = Overriding Part) December 2015 Imprint Joint report of The Republic of Italy, The Principality of Liechtenstein, The Federal Republic of Austria, The Federal Republic of Germany, The Republic of France, The Grand Duchy of Luxemburg, The Kingdom of Belgium, The Kingdom of the Netherlands With the cooperation of the Swiss Confederation Data sources Competent Authorities in the Rhine river basin district Coordination Rhine Coordination Committee in cooperation with the International Commission for the Protection of the Rhine (ICPR) Drafting of maps Federal Institute of Hydrology, Koblenz, Germany Publisher: International Commission for the Protection of the Rhine (ICPR) Kaiserin-Augusta-Anlagen 15, D 56068 Koblenz P.O. box 20 02 53, D 56002 Koblenz Telephone +49-(0)261-94252-0, Fax +49-(0)261-94252-52 Email: [email protected] www.iksr.org Translation: Karin Wehner ISBN 978-3-941994-72-0 © IKSR-CIPR-ICBR 2015 IKSR CIPR ICBR Bewirtschaftungsplan 2015 IFGE Rhein Contents Introduction .................................................................................. 6 1. General description .............................................................. 8 1.1 Surface water bodies in the IRBD Rhine ................................................. 11 1.2 Groundwater ...................................................................................... 12 2. Human activities and stresses ..........................................
    [Show full text]
  • Case Study Rhine
    International Commission for the Hydrology of the Rhine Basin Erosion, Transport and Deposition of Sediment - Case Study Rhine - Edited by: Manfred Spreafico Christoph Lehmann National coordinators: Alessandro Grasso, Switzerland Emil Gölz, Germany Wilfried ten Brinke, The Netherlands With contributions from: Jos Brils Martin Keller Emiel van Velzen Schälchli, Abegg & Hunzinger Hunziker, Zarn & Partner Contribution to the International Sediment Initiative of UNESCO/IHP Report no II-20 of the CHR International Commission for the Hydrology of the Rhine Basin Erosion, Transport and Deposition of Sediment - Case Study Rhine - Edited by: Manfred Spreafico Christoph Lehmann National coordinators: Alessandro Grasso, Switzerland Emil Gölz, Germany Wilfried ten Brinke, The Netherlands With contributions from: Jos Brils Martin Keller Emiel van Velzen Schälchli, Abegg & Hunzinger Hunziker, Zarn & Partner Contribution to the International Sediment Initiative of UNESCO/IHP Report no II-20 of the CHR © 2009, KHR/CHR ISBN 978-90-70980-34-4 Preface „Erosion, transport and deposition of sediment“ Case Study Rhine ________________________________________ Erosion, transport and deposition of sediment have significant economic, environmental and social impacts in large river basins. The International Sediment Initiative (ISI) of UNESCO provides with its projects an important contribution to sustainable sediment and water management in river basins. With the processing of exemplary case studies from large river basins good examples of sediment management prac- tices have been prepared and successful strategies and procedures will be made accessible to experts from other river basins. The CHR produced the “Case Study Rhine” in the framework of ISI. Sediment experts of the Rhine riparian states of Switzerland, Austria, Germany and The Netherlands have implemented their experiences in this publication.
    [Show full text]
  • Analysis of Overdeepened Valleys Using the Digital Elevation Model of the Bedrock Surface of Northern Switzerland
    Swiss J Geosci (2010) 103:375–384 DOI 10.1007/s00015-010-0043-z Analysis of overdeepened valleys using the digital elevation model of the bedrock surface of Northern Switzerland Peter Jordan Received: 6 March 2008 / Accepted: 7 June 2010 / Published online: 30 November 2010 Ó Swiss Geological Society 2010 Abstract Based on surface and borehole information, are divided into several sub-basins, indicating a multiphase together with pre-existing regional and local interpretations, evolution of the valleys. Some of the swells or barriers a 7,150 square kilometre Raster Digital Elevation Model separating the sub-basins coincide with known late LGM (DEM) of the bedrock surface of northern Switzerland was retreat stages. In the Suhre valley, an old fluvial valley floor constructed using a 25 m cell size. This model represents a with restricted overdeepened sections is documented. further important step in the understanding of Quaternary sediment distribution and is open to a broad field of appli- Keywords Quaternary cover Á Bedrock surface Á cation and analysis, including hydrogeological, geotech- Overdeepened valleys Á DEM Á GIS nical and geophysical studies as well as research in the field of Pleistocene landscape evolution. An analysis of the overdeepened valleys in the whole model area and, more Introduction specifically in the Reuss area, shows that, in most cases, overdeepening is restricted to the areas covered by the Last Motivation Glaciation Maximum (LGM). However, at various locations relatively narrow overdeepened valleys outreach the tongue A well established knowledge of the bedrock surface basins and the LGM ice shield limits. Therefore, an earlier geometry and the thickness and spatial distribution of and further-reaching glacial event has probably contributed unconsolidated rock is of fundamental interest for a wide significantly to the overdeepening of these valleys.
    [Show full text]
  • Reconstruction of Flood Events Based on Documentary Data And
    Hydrol. Earth Syst. Sci., 19, 4149–4164, 2015 www.hydrol-earth-syst-sci.net/19/4149/2015/ doi:10.5194/hess-19-4149-2015 © Author(s) 2015. CC Attribution 3.0 License. Reconstruction of flood events based on documentary data and transnational flood risk analysis of the Upper Rhine and its French and German tributaries since AD 1480 I. Himmelsbach1, R. Glaser1, J. Schoenbein1, D. Riemann1, and B. Martin2 1Physical Geography, Albert-Ludwigs Universität Freiburg, Freiburg, Germany 2CRESAT, University of Haut-Alsace, Mulhouse, France Correspondence to: J. Schoenbein ([email protected]) Received: 1 December 2014 – Published in Hydrol. Earth Syst. Sci. Discuss.: 7 January 2015 Revised: 11 September 2015 – Accepted: 23 September 2015 – Published: 14 October 2015 Abstract. This paper presents the long-term analysis of flood the small rivers in Alsace compared to those on the Baden occurrence along the southern part of the Upper Rhine River side – an interesting fact – especially if the modern European system and of 14 of its tributaries in France and Germany Flood directive is taken into account. covering the period starting from 1480 BC. Special focus is given on the temporal and spatial variations of flood events and their underlying meteorological causes over time. Ex- 1 Introduction amples are presented of how long-term information about flood events and knowledge about the historical aspect of The knowledge about the occurrence of floods in histori- flood protection in a given area can help to improve the un- cal times, their meteorological causes and their distribution derstanding of risk analysis and therefor transnational risk within the (hydrological) year does provide a deeper under- management.
    [Show full text]
  • Tracer Studies of River-Groundwater Interaction Under Hydropeaking Conditions
    Tracer Studies of River-Groundwater Interaction under Hydropeaking Conditions Dissertation Markus W. Fette 2 Dissertation ETH Nr. 16103 Tracer Studies of River-Groundwater Interaction under Hydropeaking Conditions A dissertation submitted to the SWISS FEDERAL INSTITUTE OF TECHNOLOGY ZURICH for the degree of DOCTOR OF NATURAL SCIENCES presented by MARKUS WOLFGANG FETTE Dipl.-Ing., University of Stuttgart born on September 12, 1973 citizen of Germany accepted on recommendation of Prof. Dr. Bernhard Wehrli, examiner Prof. Dr. Pierre Perrochet, co-examiner Prof. Dr. Anton Schleiss, co-examiner Zürich 2005 3 4 Was den Menschen angeht, so glaube ich an das Individuum, nicht aber an den Individualismus. Was die Natur angeht, so glaube ich an das sinnvolle Zusammenspiel ihrer schöpferischen und zerstörerischen Kräfte, nicht aber an deren Manipulierbarkeit zu eigennützigen Zwecken. Was die Musik angeht, so glaube ich an die Töne, nicht aber an die Noten. Was das Geld angeht, so glaube ich an Münzen und Noten und sonst an gar nichts. Was die ewige Liebe angeht, so glaube ich an ihre fortdauernde Renovierbarkeit, nicht aber an ihre Konservierbarkeit. Was die Religion angeht, so glaube ich an Erfahrung, nicht aber an Überzeugungen. Was Antworten auf die letzten Fragen angeht, so glaube ich an den Gedankenstrich, nicht aber an das Ausrufezeichen. Balts Nill, Musiker (Stiller Has) 5 6 Table of Contents T. Table of Contents.......................................................................... 7 A. Acknowledgements ...................................................................
    [Show full text]
  • Flood Risk Along the Upper Rhine Since AD 1480
    Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Hydrol. Earth Syst. Sci. Discuss., 12, 177–211, 2015 www.hydrol-earth-syst-sci-discuss.net/12/177/2015/ doi:10.5194/hessd-12-177-2015 © Author(s) 2015. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal Hydrology and Earth System Sciences (HESS). Please refer to the corresponding final paper in HESS if available. Flood risk along the upper Rhine since AD 1480 I. Himmelsbach1, R. Glaser1, J. Schoenbein1, D. Riemann1, and B. Martin2 1Physical Geography, Albert-Ludwigs-University Freiburg, Germany 2CRESAT, University of Haut-Alsace, Mulhouse, France Received: 1 December 2014 – Accepted: 9 December 2014 – Published: 7 January 2015 Correspondence to: J. Schoenbein ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 177 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract This paper presents the occurrence, cause and frequency changes of floods, their development and distribution along the southern part of the upper Rhine River and of 14 of its tributaries in France and Germany covering the period from 1480 BC. Special 5 focus is given on the temporal and spatial variations and underlying meteorological causes which show a significant change over space and time. Examples are presented how long-term information can help to improve transnational risk and risk management analysis while connecting single historical and modern extreme events. 1 Introduction 10 The knowledge about the occurrence of floods in historical times, their meteorologi- cal causes and their distribution within the (hydrological) year does provide a deeper understanding of the natural variability of the severity of flood events by providing long- term knowledge about changes in the causes, frequencies and gravities of the floods.
    [Show full text]
  • Intergovernmental Perspective, 1991, V.17 No.4
    ‘commission_ ment in which the Congress declares ists don’t even have to be so clever in everything to be of national interest, fashioning a constitutional justification and then requires the states and lucal because the Supreme Court threw up governments to raise the money and its hands and said to the Congress, do perform the mandates under threat of what you want to do. The Com’t con- civil and, often, criminal annctions. cluded that the Tenth Amendment of- The Constitution has been amend- fers no guidance on where to draw the ed a thousand times over without the line between federal and state power, need to use the cumbersome, constitu- and that the only avenue left for main- tionally provided, amendment process. taining some balance among the gov- The Congress. the Administration, and ernments in our federal system is the courts have ignored the admoni- through the election process. tion of Chief Justice Roger B. “Ikney For the Congress, the end now who said, “If we are at liberty to give old justifies the means, and the Tenth words new meanings—there is no pow- Amendment is dead. When Justice States and cities are having in- er which may not by this mode of con- Robert H. Jackson, in Youn@/own v. creasing difficulty finding the funds struction, be conferred on the general Smvyer (1952), involving President Tru- to provide traditional services and facili- government and denied to the states.” man’s steel plant takeover, stated that ‘Ilrough the Constitution, the states ties —plice, fire, educntion, and tiras- “necessity knows no law,” he was right.
    [Show full text]