139855
A physical quantity \(Q\) is related to four independent observables \(\alpha, \beta, \mathrm{c}\) and \(\mathrm{d}\) as \(\mathrm{Q}=\frac{\alpha^{3} \beta^{2}}{\sqrt{\mathrm{cd}}}\)
The percentage error of measurement is \(\alpha, \beta, c\) and \(d\) respectively are \(1 \% 3 \% 4 \%\) and \(2 \%\) The percentage error in the quantity \(Q\) is then
139857 The following observations were taken for determining surface tension \(T\) of water by capillary method, Diameter of capillary, d \(=1.25 \times 10^{-2} \mathrm{~m}\), Rise of water, \(h=1.45 \times 10^{-2} \mathrm{~m}\). Using \(g=9.80 \mathrm{~m} / \mathrm{s}^{2}\) and the simplified relation \(\mathrm{T}=\frac{\text { rhg }}{2} \times 10^{3} \mathrm{~N} / \mathrm{m}\), the possible error in surface tension is closest to
139855
A physical quantity \(Q\) is related to four independent observables \(\alpha, \beta, \mathrm{c}\) and \(\mathrm{d}\) as \(\mathrm{Q}=\frac{\alpha^{3} \beta^{2}}{\sqrt{\mathrm{cd}}}\)
The percentage error of measurement is \(\alpha, \beta, c\) and \(d\) respectively are \(1 \% 3 \% 4 \%\) and \(2 \%\) The percentage error in the quantity \(Q\) is then
139857 The following observations were taken for determining surface tension \(T\) of water by capillary method, Diameter of capillary, d \(=1.25 \times 10^{-2} \mathrm{~m}\), Rise of water, \(h=1.45 \times 10^{-2} \mathrm{~m}\). Using \(g=9.80 \mathrm{~m} / \mathrm{s}^{2}\) and the simplified relation \(\mathrm{T}=\frac{\text { rhg }}{2} \times 10^{3} \mathrm{~N} / \mathrm{m}\), the possible error in surface tension is closest to
139855
A physical quantity \(Q\) is related to four independent observables \(\alpha, \beta, \mathrm{c}\) and \(\mathrm{d}\) as \(\mathrm{Q}=\frac{\alpha^{3} \beta^{2}}{\sqrt{\mathrm{cd}}}\)
The percentage error of measurement is \(\alpha, \beta, c\) and \(d\) respectively are \(1 \% 3 \% 4 \%\) and \(2 \%\) The percentage error in the quantity \(Q\) is then
139857 The following observations were taken for determining surface tension \(T\) of water by capillary method, Diameter of capillary, d \(=1.25 \times 10^{-2} \mathrm{~m}\), Rise of water, \(h=1.45 \times 10^{-2} \mathrm{~m}\). Using \(g=9.80 \mathrm{~m} / \mathrm{s}^{2}\) and the simplified relation \(\mathrm{T}=\frac{\text { rhg }}{2} \times 10^{3} \mathrm{~N} / \mathrm{m}\), the possible error in surface tension is closest to
139855
A physical quantity \(Q\) is related to four independent observables \(\alpha, \beta, \mathrm{c}\) and \(\mathrm{d}\) as \(\mathrm{Q}=\frac{\alpha^{3} \beta^{2}}{\sqrt{\mathrm{cd}}}\)
The percentage error of measurement is \(\alpha, \beta, c\) and \(d\) respectively are \(1 \% 3 \% 4 \%\) and \(2 \%\) The percentage error in the quantity \(Q\) is then
139857 The following observations were taken for determining surface tension \(T\) of water by capillary method, Diameter of capillary, d \(=1.25 \times 10^{-2} \mathrm{~m}\), Rise of water, \(h=1.45 \times 10^{-2} \mathrm{~m}\). Using \(g=9.80 \mathrm{~m} / \mathrm{s}^{2}\) and the simplified relation \(\mathrm{T}=\frac{\text { rhg }}{2} \times 10^{3} \mathrm{~N} / \mathrm{m}\), the possible error in surface tension is closest to
139855
A physical quantity \(Q\) is related to four independent observables \(\alpha, \beta, \mathrm{c}\) and \(\mathrm{d}\) as \(\mathrm{Q}=\frac{\alpha^{3} \beta^{2}}{\sqrt{\mathrm{cd}}}\)
The percentage error of measurement is \(\alpha, \beta, c\) and \(d\) respectively are \(1 \% 3 \% 4 \%\) and \(2 \%\) The percentage error in the quantity \(Q\) is then
139857 The following observations were taken for determining surface tension \(T\) of water by capillary method, Diameter of capillary, d \(=1.25 \times 10^{-2} \mathrm{~m}\), Rise of water, \(h=1.45 \times 10^{-2} \mathrm{~m}\). Using \(g=9.80 \mathrm{~m} / \mathrm{s}^{2}\) and the simplified relation \(\mathrm{T}=\frac{\text { rhg }}{2} \times 10^{3} \mathrm{~N} / \mathrm{m}\), the possible error in surface tension is closest to