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Designing an Interactive Game to Encourage Cognitive Empathy As a Bullying Prevention Tool
International Journal of Engineering & Technology, 7 (4.19) (2018) 144-157 International Journal of Engineering & Technology Website: www.sciencepubco.com/index.php/IJET Research paper Designing an Interactive Game to Encourage Cognitive Empathy as a Bullying Prevention Tool Hanif Baharin1*, ShukorSanimMohdFauzi2, Azlina Ahmad3, Fazillah Mohmad Kamal4 1,3Institute of Visual Informatics, Universiti Kebangsaan Malaysia, 2UniversitiTeknologi MARA 4Faculty of Quantitative Sciences, Universiti Utara Malaysia *Corresponding Author Email: [email protected] Abstract Bullying can have detrimental consequences to the victims, hence there is a need for bullying prevention programs at school. In this paper, we describe a gameplay model which may be usedto elicit cognitive empathy as a part of anti-bullying program among schoolchildren. We interviewed 79 schoolchildren from four schools in order to find out their understanding of bullying and their play behavior, and we observed their play behaviorduring recess. We found that most schoolchildren in our study instinctively know that bullying is wrong because it hurt others but attributethe consequences to self as imposed by authorities as the reason why hurting others is wrong. We argue that, this shows that they demonstrate affective empathy but would benefit from cognitive empathy training. From our findings we came out with design guidelines and produced a bullying morality conceptual model, which then informed our gameplay model. To validate the gameplay model, we designed and tested an indoor physical computing game prototype that encourages player to collectively exercise their cognitive empathy. The results from our game testing shows that the game mechanics proposed in our gameplay model do encourage players to exercise the empathy. -
Adamsite-(Y), a New Sodium–Yttrium Carbonate Mineral
1457 The Canadian Mineralogist Vol. 38, pp. 1457-1466 (2000) ADAMSITE-(Y), A NEW SODIUM–YTTRIUM CARBONATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC JOEL D. GRICE§ and ROBERT A. GAULT Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada MARK A. COOPER Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada ABSTRACT Adamsite-(Y), ideally NaY(CO3)2•6H2O, is a newly identified mineral from the Poudrette quarry, Mont Saint-Hilaire, Quebec. It occurs as groups of colorless to white and pale pink, rarely pale purple, flat, acicular to fibrous crystals. These crystals are up to 2.5 cm in length and form spherical radiating aggregates. Associated minerals include aegirine, albite, analcime, ancylite-(Ce), calcite, catapleiite, dawsonite, donnayite-(Y), elpidite, epididymite, eudialyte, eudidymite, fluorite, franconite, gaidonnayite, galena, genthelvite, gmelinite, gonnardite, horváthite-(Y), kupletskite, leifite, microcline, molybdenite, narsarsukite, natrolite, nenadkevichite, petersenite-(Ce), polylithionite, pyrochlore, quartz, rhodochrosite, rutile, sabinaite, sérandite, siderite, sphalerite, thomasclarkite-(Y), zircon and an unidentified Na–REE carbonate (UK 91). The transparent to translucent mineral has a vitreous to pearly luster and a white streak. It is soft (Mohs hardness 3) and brittle with perfect {001} and good {100} and {010} cleav- ␣  ␥ ° ° ages. Adamsite-(Y) is biaxial positive, = V 1.480(4), = 1.498(2), = 1.571(4), 2Vmeas. = 53(3) , 2Vcalc. = 55 and is nonpleochroic. Optical orientation: X = [001], Y = b, Z a = 14° (in  obtuse). It is triclinic, space group P1,¯ with unit-cell parameters refined from powder data: a 6.262(2), b 13.047(6), c 13.220(5) Å, ␣ 91.17(4),  103.70(4), ␥ 89.99(4)°, V 1049.1(5) Å3 and Z = 4. -
The Journal of Gemmology Editor: Dr R.R
he Journa TGemmolog Volume 25 No. 8 October 1997 The Gemmological Association and Gem Testing Laboratory of Great Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London Eel N SSU Tel: 0171 404 1134 Fax: 0171 404 8843 e-mail: [email protected] Website: www.gagtl.ac.uklgagtl President: Professor R.A. Howie Vice-Presidents: LM. Bruton, Af'. ram, D.C. Kent, R.K. Mitchell Honorary Fellows: R.A. Howie, R.T. Liddicoat Inr, K. Nassau Honorary Life Members: D.). Callaghan, LA. lobbins, H. Tillander Council of Management: C.R. Cavey, T.]. Davidson, N.W. Decks, R.R. Harding, I. Thomson, V.P. Watson Members' Council: Aj. Allnutt, P. Dwyer-Hickey, R. fuller, l. Greatwood. B. jackson, J. Kessler, j. Monnickendam, L. Music, l.B. Nelson, P.G. Read, R. Shepherd, C.H. VVinter Branch Chairmen: Midlands - C.M. Green, North West - I. Knight, Scottish - B. jackson Examiners: A.j. Allnutt, M.Sc., Ph.D., leA, S.M. Anderson, B.Se. (Hons), I-CA, L. Bartlett, 13.Se, .'vI.phil., I-G/\' DCi\, E.M. Bruton, FGA, DC/\, c.~. Cavey, FGA, S. Coelho, B.Se, I-G,\' DGt\, Prof. A.T. Collins, B.Sc, Ph.D, A.G. Good, FGA, f1GA, Cj.E. Halt B.Sc. (Hons), FGr\, G.M. Howe, FG,'\, oo-, G.H. jones, B.Se, PhD., FCA, M. Newton, B.Se, D.PhiL, H.L. Plumb, B.Sc., ICA, DCA, R.D. Ross, B.5e, I-GA, DGA, P..A.. Sadler, 13.5c., IGA, DCA, E. Stern, I'GA, DC/\, Prof. I. -
Let Us Enjoy Our Leisure Through Recreational Games 4
Let us enjoy our leisure 4 through recreational games Activities such as running, jumping, throwing, creeping, hanging, etc. are movements which help to maintain the body in an active, healthy, energetic and happy state. Games can be categorized into three main groups such as; minor games, leadup games, and organized games. When you have studied this lesson you would, be able to create and play new games, and spend your leisure time happily and enjoyably. Also you would be able to gain some knowledge about organized games. Let us understand the need for sports activities The bell rang for the school interval. Menuka and his friends ran happily to the ground after enjoying their meal of chickpeas and cowpea brought in their lunch boxes from home. “What are we playing today?” asked Raman. “Let’s play Breaking seven stones” answered Mohamed. “We don’t have a ball to play Breaking seven stones. So let’s play chase 62 For Free Distribution. 63 and catch.” suggested Menuka. “Fine, let’s count to find the catcher. 10, 20, 30, 40……,” counted Ravi keeping his friends in a circle. Menuka and his friends played till the interval was over. Figure 4.1- Students engaging in different recreational games. Can you remember such games that you play when you get together with your friends? You would have seen such games being played during the interval or at the sports meet. All these games help to keep our body active and in good shape. Relaxation for your mind after being engrossed in educational activities could be achieved by indulging in a game or sport. -
A New Beryllium Silicate Mineral Species from Mont Saint-Hilaire, Quebec
193 The Canadian Mineralogist Vol. 47, pp. 193-204 (2009) DOI : 10.3749/canmin.47.1.193 BUSSYITE-(Ce), A NEW BERYLLIUM SILICATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC JOEL D. GRICE§, RALPH ROWE AN D GLENN POIRIER Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ALLEN PRATT CANMET, Mining and Mineral Sciences Laboratories, 555 Booth Street, Ottawa, Ontario K1A 0G1, Canada JAMES FRANCIS Surface Science Western, University Western Ontario, London, Ontario N6A 5B7, Canada ABS tr A ct Bussyite-(Ce), ideally (Ce,REE,Ca)3(Na,H2O)6MnSi9Be5(O,OH)30(F,OH)4, a new mineral species, was found in the Mont Saint-Hilaire quarry, Quebec. The crystals are transparent to translucent, pale pinkish orange in color, with a white streak and vitreous luster. Bladed crystals are prismatic, having forms {111} and {101}; they are elongate on [101], up to 10 mm in length. Associated minerals include aegirine, albite, analcime, ancylite-(Ce), calcite, catapleiite, gonnardite, hydrotalcite, kupletskite, leucophanite, microcline, nenadkevichite, polylithionite, serandite and sphalerite. Bussyite-(Ce) is monoclinic, space group C2/c, with unit-cell parameters refined from powder-diffraction data: a 11.654(3), b 13.916(3), c 16.583(4) Å, b 95.86(2)°, V 3 2675.4(8) Å and Z = 4. Electron-microprobe and secondary-ion mass spectrometric analyses give the average and ranges: Na2O 7.63 (9.40–6.62), K2O 0.05 (0.13–0.0), BeO 8.33 (SIMS), CaO 5.35 (5.95–4.17), MgO 0.03 (0.11–0.00), MnO 2.49 (3.00–1.71), Al2O3 0.82 (1.54–0.39), Y2O3 1.97 (2.68–1.51), La2O3 2.65 (3.11–2.16), Ce2O3 9.77 (11.22 –8.15), Pr2O3 1.23 (1.49 –0.74), Nd2O3 4.54 (5.13–3.91), Sm2O3 0.99 (1.25–0.68), Eu2O3 0.010 (0.25–0.0), Gd2O3 1.03 (1.23–0.81), SiO2 38.66 (39.94–37.66), ThO2 3.31 (4.59–2.12), F 3.67 (6.39–2.54), S 0.03 (0.08–0), H2O 4.12 (determined from crystal-structure analysis), for a total of 95.21 wt.%. -
Combined Single-Crystal X-Ray and Neutron Powder Diffraction Structure
American Mineralogist, Volume 95, pages 519–526, 2010 Combined single-crystal X-ray and neutron powder diffraction structure analysis exemplified through full structure determinations of framework and layer beryllate minerals JENNIFER A. ARMSTRONG ,1 HENRIK FRIIS,2 ALEX A NDR A LIEB ,1,* ADRI A N A. FINC H ,2 A ND MA RK T. WELLER 1,† 1School of Chemistry, University of Southampton, Highfield, Southampton, Hampshire SO17 1BJ, U.K. 2School of Geography and Geosciences, Irvine Building, University of St. Andrews, North Street, St. Andrews, Fife KY16 9AL, U.K. ABSTR A CT Structural analysis, using neutron powder diffraction (NPD) data on small quantities (<300 mg) and in combination with single-crystal X-ray diffraction (SXD) data, has been employed to determine accurately the position of hydrogen and other light atoms in three rare beryllate minerals, namely bavenite, leifite/IMA 2007-017, and nabesite. For bavenite, leifite/IMA 2007-017, and nabesite, sig- nificant differences in the distribution of H, as compared to the literature using SXD analysis alone, have been found. The benefits of NPD data, even with small quantities of H-containing materials, and, more generally, in applying a combined SXD-NPD method to structure analysis of minerals are discussed, with reference to the quality of the crystallographic information obtained. Keywords: Hydrogen, beryllium, minerals, powder neutron diffraction INTRODUCTION lower cation charge, Be2+ vs. Si4+. Thus, a bridging or terminal Information on crystal structure of minerals, including the O forming part of a Beϕ4 tetrahedron is under-bonded compared localization of light atoms such as H and Be, is of considerable to the equivalent Siφ4 unit leading to the prevalence of Be-OH importance because it allows a better understanding of the min- and Be-F in beryllate minerals (Hawthorne and Huminicki eral behavior under natural conditions. -
Stability of Na–Be Minerals in Late-Magmatic Fluids of the Ilímaussaq Alkaline Complex, South Greenland
Stability of Na–Be minerals in late-magmatic fluids of the Ilímaussaq alkaline complex, South Greenland Gregor Markl Various Na-bearing Be silicates occur in late-stage veins and in alkaline rocks metasomatised by late-magmatic fluids of the Ilímaussaq alkaline complex in South Greenland. First, chkalovite crys- tallised with sodalite around 600°C at 1 kbar. Late-magmatic assemblages formed between 400 and 200°C and replaced chkalovite or grew in later veins from an H2O-rich fluid. This fluid is also recorded in secondary fluid inclusions in most Ilímaussaq nepheline syenites. The late assem- blages comprise chkalovite + ussingite, tugtupite + analcime ± albite, epididymite + albite, bertrandite ± beryllite + analcime, and sphaerobertrandite + albite or analcime(?). Quantitative phase diagrams involving minerals of the Na–Al–Si–O–H–Cl system and various Be minerals show that tugtupite co-exists at 400°C only with very Na-rich or very alkalic fluids [log 2 (a /a ) > 6–8; log (a 2+/(a ) ) > –3]. The abundance of Na-rich minerals and of the NaOH-bear- Na+ H+ Be H+ ing silicate ussingite indicates the importance of both of these parameters. Water activity and silica activity in these fluids were in the range 0.7–1 and 0.05–0.3, and XNaCl in a binary hydrous fluid was below 0.2 at 400°C. As bertrandite is only stable at < 220°C at 1 kbar, the rare formation of epididymite, eudidymite, bertrandite and sphaerobertrandite by chkalovite-consuming reactions occurred at still lower temperatures and possibly involved fluids of higher silica activity. Institut für Mineralogie, Petrologie und Geochemie, Eberhard-Karls-Universität, Wilhelmstrasse 56, D-72074 Tübingen, Germany. -
7 Congresso Internacional De Jogos Desportivos
Motriz, Rio Claro, v.25, Issue Special, 2019 DOI: http://dx.doi.org/10.1590/S1980-65742019SI7congress 7o CONGRESSO INTERNACIONAL DE JOGOS DESPORTIVOS ALEXANDRE IGOR ARARIPE MEDEIROS MÁRIO ANTÔNIO DE MOURA SIMIM Rua EuclídesOnófre de Souza, 880 Casa 1 - Lagoa Sapiranga (Coité) Fortaleza – CE | Fone: 85 9.9991-4199 | 85 9.9755-6043 | www.gestaomix.com.br IDENTIFICAÇÃO 7o Congresso Internacional de Jogos Desportivos: Transdisciplinaridade e Multiprofissionalidade nos Jogos Desportivos: Possibilidades de Intervenção profissional Presidente de Honra Prof. Dr. Fernando Tavares – FADEUP – Porto – Portugal Coordenadores Gerais do Congresso Prof. Dr. Adriano César Carneiro Loureiro – UECE – Fortaleza – CE Prof. Esp. Ailton Silva Oliveira – Diretor Presidente – Gestão Mix Sports Business Prof. Dr. Alexandre Igor Araripe Medeiros – IEFES/UFC – Fortaleza – CE Prof. Esp. João Antônio da Silva Neto – APEFICE – Fortaleza – CE Prof. Esp. Jorge Henrique Monteiro – CREF 5 – Fortaleza – CE Prof. Esp. Renne Mazza - APEFICE – Fortaleza – CE Prof. Ms. Ralciney Márcio Carvalho Barbosa – UNIFOR – Fortaleza – CE Comissão Científica: Prof. Dr. Alcides José Scaglia – UNICAMP – Campinas - SP Prof. Dr. Alexandre Igor Araripe Medeiros – IEFES/UFC – Fortaleza - CE Prof. Dr. André Igor Fonteles – UNIFOR – Fortaleza - CE Prof. Dr. Antonio Carlos Gomes – COB Prof. Dr. Cláudio de Oliveira Assumpção – IEFES/UFC – Fortaleza - CE Profª Drª. Doralice Orrigo da Cunha – Grupo de Estudo Unifor - Fortaleza - CE Prof. Dr. Fernando Tavares – FADEUP – Porto-Portugal Prof. Dr. Gilmário Ricarte Batista – UFPB – João Pessoa – Paraíba Profª. Drª. Isabel Mesquita – FADEUP – Porto-Portugal Prof. Dr. João Cláudio Braga Pereira Machado - UFAM – Manaus - AM Prof. Dr. José Afonso Neves – FADEUP – Porto - Portugal Prof. Ms. José Flávio Alencar Filho – UNIFOR – Fortaleza - CE Prof. -
Alphabetical List
LIST L - MINERALS - ALPHABETICAL LIST Specific mineral Group name Specific mineral Group name acanthite sulfides asbolite oxides accessory minerals astrophyllite chain silicates actinolite clinoamphibole atacamite chlorides adamite arsenates augite clinopyroxene adularia alkali feldspar austinite arsenates aegirine clinopyroxene autunite phosphates aegirine-augite clinopyroxene awaruite alloys aenigmatite aenigmatite group axinite group sorosilicates aeschynite niobates azurite carbonates agate silica minerals babingtonite rhodonite group aikinite sulfides baddeleyite oxides akaganeite oxides barbosalite phosphates akermanite melilite group barite sulfates alabandite sulfides barium feldspar feldspar group alabaster barium silicates silicates albite plagioclase barylite sorosilicates alexandrite oxides bassanite sulfates allanite epidote group bastnaesite carbonates and fluorides alloclasite sulfides bavenite chain silicates allophane clay minerals bayerite oxides almandine garnet group beidellite clay minerals alpha quartz silica minerals beraunite phosphates alstonite carbonates berndtite sulfides altaite tellurides berryite sulfosalts alum sulfates berthierine serpentine group aluminum hydroxides oxides bertrandite sorosilicates aluminum oxides oxides beryl ring silicates alumohydrocalcite carbonates betafite niobates and tantalates alunite sulfates betekhtinite sulfides amazonite alkali feldspar beudantite arsenates and sulfates amber organic minerals bideauxite chlorides and fluorides amblygonite phosphates biotite mica group amethyst -
Annapurna Challenge
Annapurna Challenge Supporting Girlguiding Hampshire West’s 2017 Expedition to Nepal and women’s health in Nepal. Annapurna Challenge Members of Girlguiding Hampshire We will be taking basic medical supplies West are visiting Nepal in April 2017 to with us to give to local Nepalese women trek the Annapurna trail. Thank you who have no access to even the most for supporting us through this basic of health care. challenge. Contents This challenge consists of five sections, one for each colour in the Nepalese prayer flags, and is suitable for Rainbows, Brownies, Guides and the Senior Section (not forgetting the Trefoil Guild) Units should complete one challenge from each section to gain the badge. Ideas are themed around Nepal and its culture. Please feel free to adapt the challenges to suit the girls in your units. We hope you enjoy our challenge and thank you showing an interest. Nepalese Culture Go Outdoors Crafts Games Have a go at this Appendices Badge Order Form Nepalese Culture 1. Try some Nepalese food - Cook or try the national dish Dal Bhat - Or use the traditional ingredients of rice, lentils and curried vegetables to make your own dish. - Try eating with no cutlery using just your right hand (your left hand is thought to be unclean) - Have a tasting evening of Nepalese food. (See appendix for recipe suggestions) 2. Visit a Nepalese Restaurant 3. Make Nepalese Prayer Flags - Prayer flags are often seen flying from temples in Nepal – have a go at making your own – colour in our template or make your own from scraps of material, perhaps decorate with fabric pens or try other techniques. -
TELYUSHENKOITE Csna6[Be2(Si,A1,Zn)18O39F2] — a NEW CESIUM MINERAL of the LEIFITE GROUP Atali A
New data on minerals. M.: 2003. Volume 38 5 UDC 549.657.42 TELYUSHENKOITE CsNa6[Be2(Si,A1,Zn)18O39F2] — A NEW CESIUM MINERAL OF THE LEIFITE GROUP Atali A. Agakhanov Fersman Mineralogical Museum Russian Academy of Sciences, Moscow, Russia Leonid A. Pautov Fersman Mineralogical Museum Russian Academy of Sciences, Moscow, Russia Dmitriy I. Belakovskiy Fersman Mineralogical Museum Russian Academy of Sciences, Moscow, Russia Elena V. Sokolova Department of Geological Sciences, University of Manitoba, Winnipeg, Canada Frank C. Hawthorne Department of Geological Sciences, University of Manitoba, Winnipeg, Canada A new mineral, telyushenkoite, was discovered in the DaraiPioz alkaline massif (Tajikistan). It occurs as white or colorless vitreous equant anhedral grains up to 2cm wide in coarsegrained boulders of reedmergnerite associated with microcline, polylithionite, shibkovite and pectolite. The mineral has distinct cleavage, Mohs 2 3 hardness = 6, VHN100 = 714(696737) kg/mm , Dmeas. = 2.73(1), Dcalc. = 2.73g/cm . In transmitted light, telyushenkoite is colorless and transparent. It is uniaxial positive, ω = 1.526(2), ε = 1.531(2). Singlecrystal Xray study indicates trigonal symmetry, space group P3m1, a = 14.3770(8), c = 4.8786(3) Å, V = 873.2(1) Å3, Z = 1. The strongest lines in the powderdiffraction pattern are [d(I,hkl)]: 12.47(7,010), 6.226(35,020), 4.709(21,120), 4.149(50,030), 3.456(40,130), 3.387(75,121), 3.161(100,031), 2.456 (30,231). The chemical compo- sition (electron microprobe, BeO by colorimetry) is SiO2 64.32, Al2O3 7.26, BeO 3.53, ZnO 1.71, Na2O 13.53, K2O 0.47, Cs2O 6.76, Rb2O 6.76, F 2.84, O = F 1.20, total 99.37 wt.%, corresponding to (Cs0.69Na0.31K0.14Rb0.02)1.16Na6.00 [Be2.04(Si15.46Al2.06Zn0.30)17.82O38.84F2.16]. -
A Specific Gravity Index for Minerats
A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).