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Contract Reduces Scientists' Workload
MAINTENANCE HPLC set-up with system layout (flat screen). On the left, a Waters Micromass 996 with Photo Diode Array detection. Janssen Pharmaceuticals outsources central management of 17,000 lab instruments COMPREHENSIVE MAINTENANCE contract reduces scientists’ workload Els van den Brink, Images: FOODnote Janssen Pharmaceuticals Beerse, a J&J subsidiary, has Not only has Beerse maintenance been outsourced, but outsourced the maintenance of all its lab equipment. The also equipment from the Janssen-labs in Geel (raw materials production) and Merksem (clinical facility). After eighteen months decision has big advantages; the equipment’s maintenan- and proven success, J&J is rolling this approach out to other ce status is clear, maintenance is more efficient, up-time is European sites. In Belgium, 17,000 lab instruments are centrally increased and costs are lower thanks to economies of scale managed – 14,000 of them in Beerse. Outsourcing doesn’t just with existing suppliers. But above all, outsourcing reduces relieve the lab managers of a task, but also provides them with a the administrative workload for lab managers and analysts. complete overview of their equipment maintenance strategy so they can manage their equipment based on Key Performance 2 LABinsights | December 2017 MAINTENANCE Indicators (KPIs). Scientists can call on a dedicated team Pilot study of qualified engineers onsite who address acute problems The 14,000 instruments in Beerse are housed in 12 buildings. affecting critical equipment. Valued at half a billion euros, this equipment costs 10 million euro a year in maintenance, Van Deun says. Centralizing the KPIs maintenance of so much equipment is a major effort, so it was At Janssen, Senior Manager of Laboratory Services Jan Van done in phases. -
Dating Methods and the Quaternary
c01.fm Page 1 Wednesday, March 23, 2005 3:21 AM 1 Dating Methods and the Quaternary Whatever withdraws us from the power of our senses; whatever makes the past, the distant or the future, predominate over the present, advances us in the dignity of thinking beings. Samuel Johnson 1.1 Introduction The Quaternary is the most recent period of the geological record. Spanning the last 2.5 million years or so of geological time1 and including the Pleistocene and Holocene epochs,2 it is often considered to be synonymous with the ‘Ice Age’. Indeed, for much of the Quaternary, the earth’s land surface has been covered by greatly expanded ice sheets and glaciers, and temperatures during these glacial periods were significantly lower than those of the present. But the Quaternary has also seen episodes, albeit much shorter in duration, of markedly warmer conditions, and in these interglacials the temperatures in the mid- and high-latitude regions may have exceeded those of the present day. Indeed, rather than being a period of unremitting cold, the hallmark of the Quaternary is the repeated oscillation of the earth’s global climate system between glacial and interglacial states. Establishing the timing of these climatic changes, and of their effects on the earth’s environment, is a key element in Quaternary research. Whether it is to date a particular climatic episode, to estimate the rate of operation of past geological or geomorphological processes, or to determine the age of an artefact or cultural assemblage, we need to be able to establish a chronology of events. -
Beheerboerderij Weerstandersstraat, Beerse Archeologienota 2017H20
Beheerboerderij Weerstandersstraat, Beerse Archeologienota 2017H20 RAAP België - Rapport 125 Beheerboerderij Weerstandersstraat, Beerse Archeologienota Archeologisch Vooronderzoek Verslag van de Resultaten Bureauonderzoek – 2017H20 Nazareth 2017 0 Beheerboerderij Weerstandersstraat, Beerse Archeologienota 2017H20 Colofon Opdrachtgever: Agentschap voor Natuur en Bos Titel: Beheerboerderij Weerstandersstraat Beerse Archeologienota Archeologisch Vooronderzoek Bureauonderzoek - 2017H20 Status: Definitief Datum: 20 september 2017 Auteur: Hannes Van Crombrugge Projectcode: 2017H20 Raapproject: BEWE01 Erkend archeoloog: RAAP België (OE/ERK/Archeoloog/2016/00154) Bewaarplaats documentatie: RAAP België, Steenweg Deinze 72, 9810 Nazareth Bevoegd gezag: agentschap Onroerend Erfgoed RAAP België BVBA Steenweg Deinze 72 9810 Nazareth telefoon: 09/311 56 20 - 0498/44 16 99 E-mail: [email protected] © RAAP België bvba, 2017 RAAP België aanvaardt geen aansprakelijkheid voor eventuele schade voortvloeiend uit het gebruik van de resultaten van dit onderzoek of de toepassing van de adviezen. 1 Beheerboerderij Weerstandersstraat, Beerse Archeologienota 2017H20 Inhoudsopgave Inhoudsopgave ........................................................................................................................................ 2 Samenvatting ........................................................................................................................................... 3 1 Verslag van resultaten: bureauonderzoek 2017H20 ...................................................................... -
PROVINCIE ANTWERPEN BESTUURLIJK ARRONDISSEMENT ANTWERPEN Pagina 1 Van 48 PROVINCIE ANTWERPEN Datum: 17/08/2017
PROVINCIE ANTWERPEN Datum: 17/08/2017 (1) (2) (3) (4) (5) (6) (7) (8) (9) (10) (11) (12) (13) (14) (15) (16) (17) D tot. C O diagn bijk erk opm V - V V + (V 1bis) C B C M C H CB AW CB AW B CB AW M BEG CAP BESTUURLIJK ARRONDISSEMENT ANTWERPEN VZW Emmaüs DE GROTE ROBIJN Korte Sint-Annastraat 4 2000 Antwerpen 16 23 Telefoon: 03 231 25 75 12-18j 0-18j j-m j-m Fax: E-mail: [email protected] VER Zorgbedrijf Antwerpen CENTRA BIJZONDERE JEUGDZORG ZORGBEDRIJF ANTWERPEN Ballaarstraat 35 53 2018 Antwerpen 25 43 4 3 3 Telefoon: 03 334 44 50 0-18j 0-18j 0-18j j-m j-m j-m Fax: E-mail: [email protected] AFDELINGEN: PROVINCIE ANTWERPEN BESTUURLIJK ARRONDISSEMENT ANTWERPEN Pagina 1 van 48 PROVINCIE ANTWERPEN Datum: 17/08/2017 (1) (2) (3) (4) (5) (6) (7) (8) (9) (10) (11) (12) (13) (14) (15) (16) (17) D tot. C O diagn bijk erk opm V - V V + (V 1bis) C B C M C H CB AW CB AW B CB AW M BEG CAP 18 3 DE WENDING 13 0-18j j-m Lamorinièrestraat 236 12-18j j-m 2018 Antwerpen 29 3 PENNSYLVANIA FOUNDATION 13 0-18j j-m Gouverneur Holvoetlaan 28 0-18j j-m 2100 Antwerpen VZW Elegast ELEGAST Belgiëlei 203 20 158 2018 Antwerpen 12 15 6-18j 94 32 6 26 j-m Telefoon: 03 286 75 25 0-12j 0-18j 0-18j 0-18j j-m j-m j-m j-m Fax: E-mail: [email protected] AFDELINGEN: PROVINCIE ANTWERPEN BESTUURLIJK ARRONDISSEMENT ANTWERPEN Pagina 2 van 48 PROVINCIE ANTWERPEN Datum: 17/08/2017 (1) (2) (3) (4) (5) (6) (7) (8) (9) (10) (11) (12) (13) (14) (15) (16) (17) D tot. -
Ravels - Tilburg PPEERDRD Ilburg Ravelsravels -- Ttilburg Monumental Statue of Renier N12N12
Baarle-Hertog/Nassau N 15 Merksplas - i Tourism & UiT Hoogstraten1 Beguinage / Beguinage Museum 2 Taxandria Museum ON RIM IO M T U • A P N W D O I A R L L D H E • L R 3 I A T I ONIO A D RIM M G N T U Castle of E • A N O P • W PA E M D T O I RIMOIN A R L L D H E • L R A IT I A D G N Some statues you should absolutely not miss E O •P M ATRIMOINE the Dukes of Brabant Baarle-Hertog/Nassau N 15 4 Meduceum Renier Snieders (1930) 5 On the Patersplein (Monk’s Centre of cultural life ‘de Warande’ square) you will find the 14 6 City hall / Archives monumental statue of Renier Snieders. The statue was made BaBaarlarle-Hee-Hertog/Nrtog/Nassau ! Breda N119 7 Marketplace / St Peter’s Church as a memorial for this Dutch 13 N KAMPHEIDE doctor and writer. Snieders KAMPHEIDE ZWART WATER ZWART WATER 23 ONIO M IM UN TR D A IA • P L W O R • L L D A I H D E R N IT O A M G E E• IN Merksplas - PATRIMO Tip Hoogstraten DOMBERGHEIDE DOMBERGHEIDE 8 He izide ENGELAND was born in 1812 in Bladel, The ENGELAND National Playing e Heizid Ravels - Tilburg 22 NIEUWE BOSSEN NIEUWE BOSSEN Kas telei DEN DOOLHOF DEN DOOLHOF n dekensweg Vel PPEEERRDDSVVEEN 21 Ko n Have a walk around Turnhout and E MerksplasMeMerksplrksplasas 20 lis abe HoogsHoogsHoogsttratentratenen Steenweg op Merksplas th Netherlands, but later had a le Wouwerstraat i Oosthoven NN124124 wg op St RavelsRavels -- TTilburgilburg umlaan bile N12N12 u 24 J Plamaten19 einstraat f Font ree nend Til- e Begi Koning Albertstraat 22 n N 25 elestr NIO M MOO NOI MUU RI I M N N T R D D 1 A T AI t I • • P A LA • P L W W W W W O O O O R • • R L • L L D L D A I A I H H D E D R E N I R N TI O AT M O GA E M EG I E •EPAT O NNI 18 •PARTIRMIMO ai Beginhof nsstraa Hoveniersstraat aa e Ka Gul K e FIFIFILLILIPPIPKKEEKNENSVNSVISVIJIJVJVVEERER let de brand new signposting w densporenlei aste t Card Museum Ka ieu ndek N el Patersstraat dreef Li rel Oomst Brugstraat at 23 straat tra doctor’s practice in Turnhout. -
13. Late Pliocene-Pleistocene Glaciation
13. LATE PLIOCENE - PLEISTOCENE GLACIATION W. A. Berggren, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts The discussion in this chapter is broken down into two increase in the former exceeding that of the latter; or parts: the first deals with glaciation in the North Atlantic as (v) less detritals, clay and carbonate deposited per unit time revealed in the data obtained on Leg 12; in the second part (that is, decreased sedimentation rate) with the decrease in an attempt is made to provide a chronologic framework of the latter exceeding the former. In view of the demon- Late Pliocene-Pleistocene glaciation and to correlate gla- strable increase in sedimentation rate above the preglacial/ cial/interglacial sequences as recorded in land and deep-sea glacial boundary at Sites 111, 112 and 116 due to increased sediments. amounts of detrital minerals and the fact that glacial periods in high latitudes are characterized by a carbonate GLACIATION IN THE NORTH ATLANTIC minimum (Mclntyre et al., in press) it can be seen that the One of the most significant aspects of Leg 12 was the correct explanation for the increase in natural gamma activ- various results which were obtained regarding glaciation in ity in the glacial part of the section is rather complex. Thin the North Atlantic. Glacial sediments were encountered at bands of carbonate were found at various levels intercalated all sites in the North Atlantic with the exception of Site with detrital-rich clays which indicates interglacial intervals, 117 (for the purpose of this discussion the North Atlantic so that the correct explanation probably lies with (iii) encompasses Sites 111 through 117; Sites 118 and 119 are above. -
Archeologische Begeleiding Verkaveling Beekakkers in Beerse
ADAK RAPPORT 4 Archeologische begeleiding verkaveling Beekakkers in Beerse S. DELARUELLE & J. VAN DONINCK De Archeologische dienst Antwerpse Kempen is een projectvereniging van de gemeenten Beerse, Oud-Turnhout, Turnhout en Vosselaar met steun van de Vlaamse gemeenschap en de provincie Antwerpen. Colofon Opdrachtgever Hermans BVBA Project Beerse-Beekakkers Projectcode 07004 Vergunning 2007/46/13506 Auteurs Stephan Delaruelle & Jef Van Doninck Kaarten & plannen Stephan Delaruelle (©NGI/GIS Vlaanderen) Foto’s & tekeningen Stephan Delaruelle Omslagontwerp Hanna Maes ISBN / © AdAK , december 2007 Niets uit deze uitgave mag worden verveelvoudigd en/of openbaar gemaakt door middel van druk, fotokopie, microfilm of op welke andere wijze dan ook, zonder voorafgaande schriftelijke toestemming van de Archeologische Dienst Antwerpse Kempen. Beerse-Beekakkers AdAK Samenvatting Op 10 mei 2007 werd door de Archeologische Dienst Antwerpse Kempen (AdAK) in samenwerking Hermans BVBA een archeologische begeleiding van de aanleg van de wegkoffers uitgevoerd binnen de verkaveling Beekakkers aan de Beekakkerstraat te Beerse. Tijdens het onderzoek werd de ontgraving van de centraal gelegen wegkoffer opgevolgd alsook de sanering van de achterliggende gebieden, waarbij in totaal ca. 1500 m2 werd onderzocht. Tijdens het onderzoek werden geen archeologisch relevante sporen vastgesteld. Opmerkelijk was ook dat natuurlijke sporen grotendeels ontbraken. Doordat het plangebied tot voor kort in gebruik was als kwekerij voor buxusplanten, waren in de onaangeroerde bodem groene en oranje verkleuringen af te lezen, die vermoedelijk te maken hebben met de het gebruik van meststoffen en insecticiden. In het bodemprofiel was ook af te lezen dat een groot gedeelte van het terrein was afgegraven en omgezet bij de inrichting van het plantenbedrijf, zoals ook door de eigenaar was aangegeven. -
Bijlagen.Pdf
Bijlagen Inhoud Bijlage 1: Het hoe en waarom van een ruimtelijk structuurplan..........................................................7 1.1. Het wetgevend kader.........................................................................................................................7 1.1.1. Het decreet van 18 mei 1999 ...........................................................................................................7 1.1.2. Omzendbrief RO 97/02 over het gemeentelijk structuurplanningsproces........................................7 1.2. Aanpak structuurplanning Wuustwezel..........................................................................................8 1.2.1. Planningsmethodiek .........................................................................................................................8 1.2.2. Communicatie en organisatie.........................................................................................................10 Bijlage 2: Verbanden met het Ruimtelijk Structuurplan Vlaanderen (RSV)......................................14 2.1. Deelstructuren in het RSV ..............................................................................................................14 2.2. Buitengebied....................................................................................................................................14 2.2.1. Doelstellingen voor het buitengebied .............................................................................................14 2.2.2. Functies in het buitengebied ..........................................................................................................15 -
An Attempt at Correlation of Main Climatostratigraphic Units of the Quaternary in the Marginal Zones of Continental Glaciations in Europe
ANNALES UNIVERSITATIS MARIAE CURIE-SKŁODOWSKA LUBLIN - POLONIA VOL.XLVIII, 14_____________________________ SECTIOB_____________________________________ 1993 Instytut Geologii Uniwersytetu Warszawskiego Leszek LINDNER, Leszek MARKS An Attempt at Correlation of Main Climatostratigraphic Units of the Quaternary in the Marginal Zones of Continental Glaciations in Europe Próba korelacji głównych jednostek klimatostratygraficznego podziału czwartorzędu w brzeżnej strefie zasięgu zlodowaceń kontynentalnych w Europie INTRODUCTION Studies of the Quaternary palaeogeographical evolution in the marginal zone of conti nental glaciations in Europe must be based on good knowledge of rhythmus of climatic changes in that time. Such changes in most cases were expressed by coolings that favou red development of 8 continental glaciations (Fig. 1) and warmings which were typical of climatic conditions during 7 interglacials, all during this part of the Quaternary that is na med the Pleistocene (Figs 2-4). From a climatostratigraphic point of view these glacia tions and interglacials, together with preceding main coolings and warmings of the Early Quaternary (Prepleistocene) as well as the following - the youngest warming of the Holo cene, are considered to be the main units of the inland Quaternary (M. D. Baraniecka 1990; L. Li n d n e r 1991b). These units are more and more frequently correlated with the 18O stages that record the main Quaternary climatic changes in deep-sea sediments (D.Q. Bowen 1989; D.Q. Bowen etal. 1989; L.Lindner 1984,1988a,b, 1991 a, b;F. Wiegank 1982; 1987; L. N. Voznyachuk 1985; V. A. Zubakov 1986, 1988, 1990; V. A. Zubakov and 1.1. Borzenkova 1990), which enables their mu tual correlations (Table 1). -
Provinciaal Ruimtelijk Uitvoeringsplan
provinciaal ruimtelijk uitvoeringsplan Voorstudie PRUP Retentiezone Laak Beerse Memorie van toelichting inclusief m.e.r.-screening Ruimtelijk planner: Steven Muylaert Dienst Ruimtelijke Planning Dienst Colofon Opdrachtgever: Dienst Ruimtelijke Planning Provincie Antwerpen Koningin Elisabethlei 22, 2000 Antwerpen tel.: 03 240 66 00 fax: 03 240 66 79 [email protected] contactpersoon: Stein Temmerman [email protected] 03/240.56.10 Opdrachthouder: D+A Consult nv Meiboom 26 1500 Halle contactpersoon: Steven Muylaert [email protected] 02/371.02.57 Dossiernummer: <ROPR/08-45> D+A Consult nv Inhoud 1. Inleiding ........................................................................................................................ 5 1.1. Aanleiding van de opdracht ....................................................................................... 5 1.2. Procesverloop .......................................................................................................... 5 2. Algemene situering ......................................................................................................... 6 2.1. Macro ..................................................................................................................... 6 2.2. Meso ...................................................................................................................... 6 2.3. Micro ...................................................................................................................... 7 3. Planningscontext ........................................................................................................... -
Geografische Afbakening Van De Zorgregio's
Geografische afbakening van de zorgregio’s Inhoudstafel 1. Situering .......................................................................................................................................... 3 2. Het huidige zorgregiodecreet .......................................................................................................... 4 3. Methodologie .................................................................................................................................. 5 4. Criteria voor afbakening .................................................................................................................. 7 4.1. Criteria voor afbakening op kleinstedelijk niveau ................................................................... 7 4.2. Criteria voor afbakening op regionaalstedelijk niveau ........................................................... 7 5. Voorstel tot afbakening per provincie op kleinstedelijk niveau ...................................................... 8 5.1. Provincie Limburg .................................................................................................................... 9 5.2. Provincie West-Vlaanderen ................................................................................................... 12 5.3. Provincie Vlaams-Brabant ..................................................................................................... 17 5.4. Provincie Oost-Vlaanderen .................................................................................................... 24 -
V. 2016A -Stages)
Global chronostratigraphical correlation table for the last 2.7 million years v. 2016a -stages) benthic δ18O records cores Vostok and Dome-C (EDC) Section Jingbian ChiLoPart time scale est European Stages 18 W American Stages normal reversed 78.47ºS 106.86ºE Magnetic susceptibility stack of 57 globally distributed Antarctic Isotope Record 37º40’54”N 53º41’48”N biozonation biozonation ItalianMediterranean Marine Stages Sea 75.10ºS 123.35ºE Coarse grained admixture 108º31’15”E BiogenicComposite Silica record Content collating108º21’06”E overlapping core segments System Series Subseries, ChronsStages Palaeomagnetic record Chinese Loess Sequence BDP-96-1 [4, 6, 7, 12-19, 22, 25-27, 29-33, 48-50]; Russian Plain StagesNorth New Zealand Stages Age Marine Isotope Stages Planktonic Foraminifera Calcareous Nannoplankton‘Standard Stages’ (supeAge r Lake Baikal Sequence BDP-96-2 [GC-1,1-49]; BDP-98 [4] North British Stages Age (Ma) Age Subchrons, (Ma) 18 -8 3 (Ma) (Ma) Excursion events Stage 5 4 Atlantic Indo-Pacific 1 0 Oatm.‰ -450 -400 0 SUS 10 m / kg 100 75% % weight D >63 µm 0% 0 10 20 30 40 50% 0 Holocene 0 0 0.5 km 0.5 km S0 depth composite 0.0117 L 0.041 Laschamp 2 Termination I - 14 ka down core depth section Valdaian a 1.0 km L1 Weichselian Devensian Wisconsinan 4 5a 1.0 km t S1 0.1 arantian 0.1 5 m_ 0.1 e | MD95-2042 Tyrrhenian Eemian Ipswichian Mikulinian Sangamonian 0.121 Blake 5e T Termination II - 130 ka NN21 CN15 CN15 2.0 km Warthe 6 2.0 km L2 Moscovian 14 m_ Drenthe ‘Tottenhill’ Haweran 0.188 Iceland Basin Illinoian 0.2 0.2 7a 0.2 2.5 km Dnieper 0.2 0.211 ? LR04 stack S2 0.239 Pringle Falls 7e 8 Termination III - 243 ka PRZ 9a L3 Saalian 0.3 0.3 3.0 km 2.5 km Wacken olstonian pre-Illinoian A 0.3 9e S3 W M 10 / Dömnitz Termination IV - 337 ka PT1b NN20 b Fuhne 0.4 i 0.4 S4 0.4 12 11 3.3 km 20 m_ Holsteinian Hoxnian Likhvinian d Termination V - 424 ka 2.8 km L5 Elsterian Anglian Okian pre-Illinoian B 0.5 d Gt.