976 resultados para Warner, Frederick Maltby, 1865-1923. Governors--Michigan
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Historia de la influencia del higienismo en la evolucin del espacio escolar de la ciudad de Vitoria entre 1865-1931.
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The pressures placed on the natural, environmental, economic, and cultural sectors from continued growth, population shifts, weather and climate, and environmental quality are increasing exponentially in the southeastern U.S. region. Our growing understanding of the relationship of humans with the marine environment is leading us to explore new ecosystem-based approaches to coastal management, marine resources planning, and coastal adaptation that engages multiple state jurisdictions. The urgency of the situation calls for coordinated regional actions by the states, in conjunction with supporting partners and leveraging a diversity of resources, to address critical issues in sustaining our coastal and ocean ecosystems and enhancing the quality of life of our citizens. The South Atlantic Alliance (www.southatlanticalliance.org) was formally established on October 19, 2009 to implement science-based policies and solutions that enhance and protect the value of coastal and ocean resources of the southeastern United States which support the region's culture and economy now and for future generations. The Alliance, which includes North Carolina, South Carolina, Georgia, and Florida, will provide a regional mechanism for collaborating, coordinating, and sharing information in support of resource sustainability; improved regional alignment; cooperative planning and leveraging of resources; integrated research, observations, and mapping; increased awareness of the challenges facing the South Atlantic region; and inclusiveness and integration at all levels. Although I am preparing and presenting this overview of the South Atlantic Alliance and its current status, there are a host of representatives from agencies within the four states, universities, NGOs, and ongoing southeastern regional ocean and coastal programs that are contributing significant time, expertise, and energy to the success of the Alliance; information presented herein and to be presented in my oral presentation was generated by the collaborative efforts of these professionals. I also wish to acknowledge the wisdom and foresight of the Governors of the four states in establishing this exciting regional ocean partnership. (PDF contains 4 pages)
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Ed. by Xabier Artiagoitia, Patxi Goenaga & Joseba A. Lakarra.
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No ano de 1923, o Clube de Regatas Vasco da Gama disputa pela primeira vez a Primeira Diviso do Campeonato Carioca de Futebol. A equipe conquista o ttulo tendo, entre seus jogadores, homens negros e mulatos. Com vitrias expressivas, aquela trajetria passa a ocupar um lugar importante no imaginrio construdo sobre as primeiras dcadas do futebol brasileiro. Toda esta construo est fundamentada na obra de Mario Filho, O Negro no Futebol Brasileiro. O livro relata o feito vascano como uma trajetria herica, na qual um time formado por negros e mulatos precisou superar preconceitos raciais para alcanar seus objetivos. A proposta desta pesquisa comparar a narrativa de Mario Filho com o que foi escrito nos jornais da poca. O objetivo verificar se h mais incoerncias ou coincidncias entre o que Mario Filho escreveu e o que os jornais noticiaram. Ao retomar os jornais da dcada de 1920, verificamos como a imprensa enxergava o acontecimento poca e, se o preconceito racial estava presente nas pginas dos jornais, assim como nos faz crer a obra de Mario Filho. A comparao revelou que, em alguns momentos, a narrativa de Mario Filho encontra respaldo integral nas notcias publicadas no ano de 1923. No entanto, em outras oportunidades o autor no encontra nenhum respaldo nas outras fontes consultadas.
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The aim of this study was to investigate the historical catch record from the Castle Fishery on the River Derwent over the period 1923 - 1989, to determine if changes had taken place in the composition of the catch and to examine the influence of flow on the performance of the fishery. The River Derwent is situated in West Cumbria, North West England. It flows from its source on Scafell Pike (NGR NY 229 089) westwards discharging into the Irish sea at Workington, a distance of 52 km. Over its length it receives water from an additional 214 km of stream, 5 large lakes and approximately 30 small tarns. The catchment drains a total area of 663 km2. The study concludes that through the time period there was considerable variation in catch between years. The trend was for the catch to increase steadily over the period 1923 - 1958, declining rapidly in 1959, after which catches increased steadily reaching a peak in the mid-sixties, before declining towards the end of the decade. During the seventies and eighties catches remained relatively stable at between 300 - 600 salmon per year until 1988 when over 2000 salmon were reported caught, the greatest number in any year over the study period.
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The biography of Charles Bradford Hudson that follows this preface had its seeds about 1965 when I (VGS) was casually examining the extensive files of original illustrations of fishes stored in the Division of Fishes, National Museum of Natural History, Smithsonian Institution. I happened upon the unpublished illustration of a rainbow trout by Hudson and was greatly impressed with its quality. The thought occurred to me then that the artist must have gone on to do more than just illustrate fishes. During the next 20 years I occasionally pawed through those files, which contained the work of numerous artists, who had worked from 1838 to the present. In 1985, I happened to discuss the files with my supervisor, who urged me to produce a museum exhibit of original fish illustrations. This I did, selecting 200 of the illustrations representing 21 artists, including, of course, Hudson. As part of the text for the exhibit, Drawn from the Sea, Art in the Service of Ichthyology, I prepared short biographies of each of the artists. The exhibit, with an available poster, was shown in the Museum for six months, and a reduced version was exhibited in U.S. and Canadian museums during the next 3 years.
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Diogenes senex Heller, 1865 sensu stricto is redescribed from specimens collected in Australia, particularly in and around the type locality of Sydney. A neotype has been designated. Comparisons of this material with other specimens identified as D. senex by a number of authors has shown that at present only the Australian material truly represents Heller's taxon.
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N_(1923)(RNH_2)RNH_2LewisRNH_2RNH_2Ag~+Zn~(2+)Cd~(2+)Sc~(3+)RNH_2(ZnCl_2, Zn(SCN)_2, CdCl_2)RNH_21RNH_2AgNO_3RNH_2AgNO_32RNH_(2(0)) + Ag~+ + NO_3~- <-> (RNH_2)_2AgNO_(3(0))IRNMR2RNH_3NO_3AgNO_3RNH_2RNH_3NO_3Ag(I)Ag(I)AgS_2O_3~-Ag(S_2O_3)_2~(3-)AgS_2O_3~-/Ag(S_2O_3)_2~(3-)NO_3~-RNH_3NO_3S_2O_3~(2-)IRS_2O_3~(2-)3RNH_2ZnCl_2RNH_2ZnCl_2pHRNH_2ZnCl_22RNH_(2(0)) + ZnCl_2 <-> (RNH_2)_2ZnCl_(2(0))1/D = 2/(C_(RMH_(2(o)))) X + (1 + from i = 1 to 4 of _i C_(cl~-)~i)/(K C_(cl~-)~2 C_(RNH_(2(0))) (XZn~(2+)) ([HCl] = 2.8 M)RNH_2ZnCl_2(RNH_3Cl)_(3(0)) + ZnCl_2 <-> (RNH_3Cl)_2ZnCl_(2(0))4RNH_2ZnBr_2, ZnI_2RNH_2ZnBr_2ZnI_2pH, RNH_2ZnCl_2ZnBr_2, ZnI_22RNH_(2(0)) + ZnX_2 <-> (RNH_2)_2ZnX_(2(0)) (x~- = Br~-, I~-) RNH_2RNH_2RNH_2ZnX_2ZnI_2 > ZnBr_2 > ZnCl_2 5RNH_2Zn(SCN)_2 Zn(SCN)_2RNH_2RNH_3NO_3Zn(II)RNH_2Zn(SCN)_22RNH_(2(0)) + Zn(SCN)_2 <-> (RNH_2)_2Zn(SCN)_(2(0)) RNH_3NO_3Zn(SCN)_4~(2-)(RNH_3NO_3)_(2(0)) + Zn(SCN)_4~(2-) <-> (RNH_3)_2Zn(SCN)_(4(0)) + 2NO_3~- RNH_2RNH_3NO_3Zn(II)6RNH_2CdCl_2Cd(II) RNH_2RNH_3ClCdCl_23RNH_(2(o)) + CdCl_2 <-> (RNH_2)_3CdCl_(2(0)) (RNH_3Cl)_(3(o)) + CdCl_2 <-> (RNH_3Cl)_3CdCl_(2(0))RNH_2CdBr_2, CdI_2, Cd(SCN)_2(RNH_2)_2CdX_2 (X~- = Br~-, I~-, SCN~-)CdX_2Cd(NO_2)_2 < CdCl_2 < CdBr_2 < Cd(SCN)_2 < CdI_2CdX_2X~-Cd(II)7RNH_2Sc_2(SO_4)_3 RNH_2Sc~(3+)1.25[(RNH_3)_2SO_4]_(2(0)) + Sc(SO_4)_3~(3-) <-> (RNH_3)_3Sc(SO_4)_3(RNH_3)_2SO_(4(0)) + 1.5SO_4~(2-)IRSO_4~(2-)Sc~(3+)RNH_2Zn(II)-Cd(II)
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R-NH_2HXRNH_3X-NH_2RNH_2N_(1923)N_(1923)IIIFeIIIZn IICdIIAgIScIIIN_(1923)TiIVHgCl_2Hg(CH_3COO)_2Cu(CH_3COO)_2N_(1923)N_(1923)N_(1923)HgCl_2 pH3-4.5Cl~-N_(1923)HgCl_2HgIIRNH_2HgCl_2RHN_(2(0)) + HgCl_2 <-> Hg(RNH_2)Cl_(2(0))Cl~-2RNH_3Cl_((0)) + HgCl_2 <-> (RNH_3Cl)_2HgCl_(2(0))2RNH_3Cl_((0)) + HgCl_4~(2-) <-> (RNH_3)_2HgCl_(4(0)) + 2Cl~-H = -48.82 KJ/molIRNMRN_(1923)Hg(CH_3COO)_2 HgCl_2Hg(CH_3COO)_2RNH_(2(0)) + Hg(CH_3CCO)_2 <-> Hg(RNH_2)(CH_3COO)_(2(0)) (CH_3COONH_3R)_(2(0)) + Hg(CH_3COO)_2 <-> (CH_3COONH_3R)_2Hg(CH_3COO)_(2(0))11.858.11N_(1923)Cu(CH_3COO)_2 RNH_2CuIIRNH_2Cu(Oh_3coo)_22RNH_(2(0)) + Cu(CH_3COO)_2 <-> Cu(RNH_2)_2(CH_3COO)_(2(0))IRCu(RNH_2)_2(CH_3COO)_2(RNH_3)_2SO_4TiIV pH0.84H_2SO_4N_(1923)TiIV3(RNH_3)_2SO_(4(0)) + Ti(OH)_3~+ + SO_4~(2-) <-> 2(RNH_3)_3Ti(OH_3)(SO_4)_(2(0))N_(1923)(RNH_3)_3Ti(OH)_3(SO_4)_2NMRIRNMRD_2ONMRIRSO_4~(2-)TiIV10.15H = 66.49 KJ/molGN_(1923) N_(1923)1Hg(II)2Hg(II)Zn(II)Cd(II)CH_3COOH3CH_3COOHCu(II)Co(II)Ni(II)4H_2SO_4(RNH_3)_2SO_4Ti(IV)-Fe(II)
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1234N_(1923)Zn(II)Cd(II)Re(III)N_(1923)ZnCl_2CdCl_2Zn(SCN)_2N_(1923)HPMBPREIIIN_(1923)Sc(III)N_(1923)(TBP, DBBP)Zn(II)Cd(II)1. N_(1923)TBPDBBPZnCl_2 N_(1923)TBPDBBPZnCl_2(RNH_3Cl)_3ZnCl_2B(RNH_3Cl)_2ZnCl_2B (B = TBPDBBP)ZnCl_2 + (RNH_3Cl)_3_((o)) + TBP_((o)) ~(K_(12)(TBP) (RNH_3Cl)_3ZnCl_3ZnCl_2TBP_((o)) ZnCl_2+Z/3(RNH_3Cl)_(3(o)) + DBBP_((o)) (RNH_3Cl)_2 ZnCl_2DBBP_((o))(RNH_3Cl)_3ZnCl_(2(o)) + TBP_((o))~(B_(12)(TBP) (RNH_3Cl)_3ZnCl_2TBP_((o)) (RNH_3Cl)_3ZnCl_(2(o)) + DBBP_((o)) ~(B_(12)(DBBP) (RNH_3Cl)_2ZnCl_2DBBP_((o)) + RNH_3Cl_((o))Zn(II)DBBP>TBPDD_1/DD_IRNMR2.N_(1923)TBPZn_(SCN)_2N_(1923)TBPZn(SCN)_2TBPZn(SCN)_2N_(1923)TBPZn(SCN)_2Zn(SCN)_23TBP. (RNH_3)_2Zn(SCN)_4TBP,Zn(SCN)_4~(2-) + (RNH_3NO_3)_(2(o)) + TBP_((o)) (RNH_3)_2Zn(SCN)_4TBP_((o)) + 2NO_3~-(RNH_3)_2Zn(SCN)_(4(o)) + TBP_((o)) ~(B'12) (RNH_3)_2Zn(SCN)_4TBP_((o)) (a) (RNH_3NO_3)_(2(o)) + Zn(SCN)_23TBP_((o)) + 2SCN~-~("12)(RNH_3)Zn(SCN)_4TBP_((o))+2TBP_((o))+2NO_3~- (b) (RNH_3NO_3)_(2(o)) + (RNH_3)_2Zn(SCN)_(4(o)) + 2SCN~- + Zn(SCN)_2.3TBP_((o)) ~("12)R(RNH_3)_2Zn(SCN)_4.TBP_((o)) + 2NO_3~- + TBP_((o)) (c) "'_(12) > '_(12) > "_(12)cabSCN~- > Cl~_IR3. N_(1923)TBPDBBPCdIIN_(1923)TBPDBBPCd(II)(RNH_3Cl)_2CdCl_2BCdCl_2 + 2/3 (RNH_3Cl)_(3(o)) + B_((o)) ~(K_(12)) (RNH_3Cl)_2CdCl_2B_((o)) (RNH_3Cl_3)CdCl_2_((o)) + B_((o)) ~(BR)(RNH_3Cl)_2CdCl_2B_((o)) + RNH_3Cl_((o))Zn(II)Zn(II) > Cd(II)IRNMR. N_(1923)HPMBPREIIIN_(1923)HPMBPREIIIRE~(3+ = La~(3+), Pr~(3+), Eu~(3+), Gd~(3+), Tb~(3+), Er~(3+), Yb~(3+)Y~(3+)RNH_3Ln(PMBP)_4Pr(III)Ln~(3+) + 4HPMBP_((o)) + RNH_3Cl_((o)) RNH_3LN(PMBP)_(4(o)) + 4H~+ + Cl~- Ln(PMBP)_(3(o)) + RNH_3Cl_((o)) RNH_3Ln(PMBP)_(4(o)) + H~+ + Cl~- RZRNH_3ClPr(III)IRNMRN_(1923)Sc(III)RNH_3NO_3Sc(III)Sc(OH)_2~+SCN~-, NO_3~-RNH_3nO_3Sc(III)PHSc(OH)_2~+ + SCN~- + 2(RNH_3NO_3)_(2((o)) (RNH_3nO_3)_4.Sc(OH)_2SCN_((o)) Sc(OH)_2~+ + SCN~- + NO_3~- + (RNH_3NO_3)_(2(o)) (RNH_3NO_3)_2.Sc(OH)(SCN)NO_3 + OH~-
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(P_(350))N_(1923)(Na,H)ClZn()IR~1H NMR(PNH_3Cl)_(3/2)ZnCl_2P_(350),1gK_(BC)=2.10,1g=0.46,,
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N1923(RNH_2)N1923()(),PO_4~(3-),()(),N1923()(),N1923 N1923,>99,
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HEH/EHP(HA)N_(1923)(RNH_3C1)HC1Zn()RNH_3Cl,HAZn();HA,RNH_3C1Zn(),
