02138020/CAPE/MS 2016 CARIBBEAN EXAMINATlONS COUNCIL CARIBBEAN ADVANCED PROFICIENCY EXAMINATIONS@ PHYSICS UNITl_PAPER02 FINAI, MARK SCHEME MAY/JUNE 2016 'z- o2t3ao2o/cAPE/Ms 2016 PHYS ICS UNITl_PAPER02 MARK SCHEME Question 1 S.O:3.1,3.2,3.3,3.8 t,K (a) (i) a 5 (ii (b) ) (i) KC xs Acceleration is the rate of change of velocity oR a : dvldt oR change of velocity divided by elapsed ti:me Unit: m s-' Both definition and unit correct (1) The Newton's Second Law: . External Unba-l-anced force ,/ (resultant) (1) . Produces an accel-erat'ion (rate of change of momentum) directly proportionaf to the magnitude of the unbalanced force in the di'rection of the unbalanced force (1) . E=ma (1) Graph - See Page 3 AI1 7 Points correct Plot: 5-6Pointscorrect Lalce]. (1) Sca].e (1) Best ].ine (1) t2t (1) 1 (ii) (iii) The reaction time of the driver (1) Strai-ght line feature beyond 0'5s OR bet 0.5 & 3.5s constant non-zero giadient (1) oR The slope of the graph between 0'5 & 3. 5s OR (iv) Distance travelled : A-rea under graph (1) (1) (Area of rectangle) + (Area of triangle) : (15 , 0.5) + (l' 15 ' 3) (1) i 1 SOI 2 4 : 7.5 + 22.5 : 30 m (1) [acce1>t al.so area of TraPezium] Eota]. 15 marks 6 4 5 -3- o2t38O2O/capn/us 2Ore PHYSICS UNIT1-PAPER02 MARK SCHEME Questi-on 1 cont'd ISca]-e il-l-: I r - on x-axis on y-axis I :r l. 4 2 : cm q 1.O sec 96=2m-r I.ll'.1 i :l t Labef Scale Plot Best line 16 i i (1) (f) {2) (1) ;14 5 d 0) , !) 8Lz IO 8 :\ \ 6 4 i--, \i \: 0.o o.o r.o 2.O 3.O Tine (s) rl 4.0 -4- o2L3gO2O/cAPE/Ms 2016 PHYSICS UNITl-PAPER02 MARK SCHEME Question 2 S.o: 2.3, 2.5,2.7,2.9 uI( (a) (i) 7.6 mm (Read off from Figure (ii 1B0o oR rI radians (accept antiphase or ) liii 1 equi val ent ) (1) 1 V = f). (1) 1 SOI :15x0.8:12ms-1(1) (b) (c) 1 between X and Y = 0o oR radians (accept "in Phase") (1) 0 (i) Phase difference (j-i) iii Antinode - Point of maximum displacement/amPlitude (1 ) Nod; - point of zero displacement/amplitude : 2 (1) Number of antinodes in Figure 3 (i) Graph - See Page ( xs KC 1) (1) (1) 5 points correct (2) 6 -.7 points correct (1) A11 Plot Lalce]- (1) Scale (1); Best line(1) (ii ) Gradient in wavel-ength) / (Change rn = (Change wave speed) (0.4s - o.oo) / G7 .s - 0.00) o.oL2 (1) Frequency : L / (gradi-ent of Plot) = - L/ oa o .oL2 2 a * (1) (Accept al so a Total 15 rnarks corr ect consistent with pl ot of v vs )' al ong 6 ana 5 4 ysl s q }2L3AO2O /CAPE,/MS 201 6 PHYS ICS UNITl-PAPER02 MARK SCHEME Questi-on 2 conL'd liil: - Scale: Labcl r - axis 2 cm =5 m s-r - y - axis 4 cm =O.1m l: ..: :1.:....:l:.. I I :l ;.,.1 o.5 ,-.1.--l t- ( I ) Plot a1I Points eortect (2) Best Line ( 1 ) -- -_:1 I r ; ,,( i ) i / o.4 i t E Ii t-:- _ - 1l tn c o o I 6 o.3 / f' o.2 / { { / I L { I .,1: o.1 ) - -, i . i., -f- -f o 5 10 t5 20 2s wave speed v/m s-l 30 3s 40 -5- o 2L38O2O /cAPE/Msl 201 6 PHYSTCS UNITl_PAPER02 MARK SCHEME Question 3 S.O: 6.6, 6-9, 6.10, 6.11 t,K (a) xs Extension is directly proportional to the applied force oR F = -kx (1) (accePt F = kx) (i) Provided that the elas ti-clProPortional not exceeded (1) (second mark cErll only be awarded if correct) ( KC l-irn-it is first is Hang a known mass from Lhe spring and measure the ext.ension. (1) ii) Record mass and corresponding extension (1) Repeat for 4 (rinim-rm) additional masses (1) use PloL a graph of weight versus extension and (1) k constant'. spring tf'" the graph to determit'L (accept aver age of f i ve( or mre) det ermi nat i ons ) Hang unknown werght from the spring and measure .oti"=po*ding extension, x (1) (b) (i) }vq Determj-ne the welght of the rock using mass(1) the and hence deternrine : Area under graph work done in extending spring (1) sor area (nethod f or : a.rea of A + area of rectangle + area between of curved Portion under AB and uPPermost side squares ) (c :ount AB recLangle under +(Lx B) + counting of squares (1) :(a,rbxh) sor Calcu]-a tl the area O.O29, 33) + (0 016 , 33) + 49 squares (1) 1 1 1 sor converting squares to q+ergy^ (5 x o.oo5)/25 : o 000lJ 1 = (1) "qlr"r" So 49 squares = 49 x 0'0001 = o. o4eJ Final cal culation and answer : 0.48 J + 0.53 J +0.049J=1 i^7.d (1) 06 + 0.02J (any suitable,/acctrrate method used to arrive at ttre final ans!iler within ttre tolerance range will earn 4 rtarks) (ii 6 Inel-astrc deformation: 1 1 -'7 - 02L38020 /CAPE,/MS 2O1 6 PHYSICS UNITl-PAPER02 MARK SCHEME a applied Load > elastic Li-rtrit (1) Therefore causes per:manent deformation (1) Total 15 marks 5 4 6 -B- o2L38O 20 /CAPE,/MS 2016 ICS PHYS UNIT1_PAPER02 MARK SCHEME Questi-on 4 UK (a) dr (1) Upward force, on l-ower surface (1) (mrst rention pressure in order to get both of the first 2 rmrks) Upthrust is the upward force minus the dovmward force (1) L{hen upthrust is less than weight of obiect; obiect will sink (1) trdhen upthrust is egual to the weight of ob3ect' the oblect will float (1) (b) KC Downward force, on upper surface due to pressure at Weight of water collected : 0'25 N (1) (i) (ii Mass ) of HzO : 0- 0- H2O 000025 (1) m3 1000 t of 1 025 kg 1000 kglm3 5w: l'. vo1 . of H2o = m= 0.025: Volume 5 : volume of stone : o.ooo025 Density of stone : (mass of sLone) / stone) = m3 (1) 3 (volume of (0.1), / (0. 000025) 4000 kqm " (1) same in The vol-ume of the liqurd displaced is the and water both cases (when ornament is immersed in (1) when immersed in corn oil) ' (c) (i) (ri ) (rii) than Upthrust on ornament due to corn oil is less (1) that due to water OR corn oi-I is fess dense than water N wt. of corn o-i1 displaced : (2'7 '1'87)N = 0'23 .. mass of corn oi-I displaced = 0'023 kq (1) : (80 - 50) cm' Volume of corn oil displaced = 30 cm3 : 3Ox1O-6 (1) 1 1 I m3 1 xs -9- o2t3ao 20 /cAPE/Msi 2O1 6 PHYSICS UNITl-PAPER02 MARK SCHE},IE .'. Densi'ty of (r) corn oil : Mass of corn oil : 0.023 = '761 kg m ' 30"10-u Vof . of corn oi-], (comect units in order to obtain both rnarks) Alternative Of r 2 C wei-ght of corn oj-1 d-isplaced = (2'7 1.87) = 0-23N (1) of corn oil displaced = (80 - 50) cm3 : 30x (1) 10-6 m3 3] below if presented in kgcm ans. [accept Volume DensitY of corn oi:l of corn oil x g) (lieight of corn oil) : '76'1 kgm-3 (1) ans (unit must be stated to earn unit mark) S.O: 4.L, 4-2 / (VoI' (1) unit 10 5 - 10- o2l38O2O /CAPE,/MS 2O1 6 PHYSICS UNITl_PAPER02 MARK SCHEME Question 5 (rnathod rm:st be practically feasible to earn ANY of the first 5 m^arks) Any suitable experiment to prove Snell's ExamPle: - (a) Diagram UK KC T'aw (2t 1. A clearly labelled diagram showing (i) glass b1ock, (ii) norma;I, (iii) incident ray' (iv) refracted ray (v) emergent ray, (vi)angIe of .incidence, i, (vii) angle of refraction, r ' Sheet of, PaPef Normal- - 2 - (subtract 1 mark for everl'rnissing conqponent) (sr:btract 1 mark for conqglete J-isting of apparatus but no t{i agram) l2l Procedure trace' ray obtaining of method Credible Credible method of obtaining i and r. 4 Indicate at least 4 repet'itions of 2 &' 3 (subtract 1 mark for onrission of any steps) 5 (1) Precaution accuracy the Any sensible step taken Lo improve of the resul-ts. Anal vsis & Interpretation 5. Pfot a graph of sin i versus sin r (b) (i) '7 (1) 't. A straight line passing through the ori:gin verifies Snell's Law : (1) (sin i/sin r) = constant medium into parti-cular one from for lrght travelling another (1) sPeed of light in bl-ock A : Speed of light iq air Refractrve index of A 2 3r1o8 : L.67 x 1o-8 m'-t (1) 1.8 XS - 11- o2t3so2o /cAPE,/Ms 201 PHYSICS UNIT.l _ PAPER 02 MARK SCHEME Questi-on 5 cont'd (j-i) (1) fonmrla Sin 72 : 1-B Sin 0 Sin 0 = sin (72) /l.B : 0.53 (1) substn & = O = 30o ans (ful I mrks f or exact ans\4er : 31 9 degrees; even if appr ox' deni ed (1) for:rtr]-a Sin O. : rr2/\1 (1)su.bstn & ans = 1.40 .'. 0" = 51" 1-BO (Accept exact ans \,1er : 51. 05 de gr ees ) At AC boundary 0 i (angle of incidence) : 22 + O a ) (iii) (iv) (22 + 30"\ 2 1 = 52o (1) angle of 51" at AC I 52' is greater than the critical j-s internalJ-y totally light and therefore the (1) AC. at reflected Tota1 15 marks I 7 6 -72PHYS 02L3AO2O/cAPE/Ms 2016 ICS UNITl_PAPER02 MARK SCHEME Question 6 S.O: 3-2| 3.3t 3.1 t,K (a) short wavelength radiation (mainly visible) passes through the earth atmosphere (1) KC enters and This j-s absorbed bY the earth (land c sea) and wa-rms them up (1) The warm land and sea then re-radiates outwards ' (1) is longer wavelength IR radiation The re-radiated radiation (1) A portion of the outgoing IR radiation is trapped' by the greenhouse gases in the atmosphere' (1) 6 This traPPed radiation causes the temPerature of the earLh's atmosPhere to j-ncrease' (1) (b) Area of glass window : L x (2. B (1) B 2.0): 4.8 m2 1 2 KA AE t (1) , Ax 0.03 m (1) (unit conversion) AX =-0 96 ) x 4-B x (35 - 26) /0-03 (1) 1382 J s-t (1) (c) Heat inPut into room to cause 3"c rise in temperature: 2 AT (1) 5.7 x 10s, C 3 1.?'106J(1) Time required for this temperature rl-se 1. 7,106 1382 2 (1) : 1,230 seconds = 20.5 minutes (1) xs