Solve these in English showing all the steps used

Here are the solutions to the questions. 1. Dimensional Analysis and Homogeneity a. Show that the equation = (2U)/(B^2 r^2) is homogeneous. An equation is dimensionally homogeneous if the dimensions of the terms on both sides of the equation are the same. Let's determine the dimensions of each variable: Specific charge (): Charge per unit mass. Dimension of charge (q) is [I T] (current × time). Dimension of mass (m) is [M]. So, [] = [M^-1 I T]. Potential difference (U): Energy per unit charge. Dimension of energy (E) is [M L^2 T^-2] (from E = F · d = (ma)d). Dimension of charge (q) is [I T]. So, [U] = [M L^2 T^-2][I T] = [M L^2 T^-3 I^-1]. Magnetic field (B): From the Lorentz force F = qvB, we have B = (F)/(qv). Dimension of force (F) is [M L T^-2]. Dimension of velocity (v) is [L T^-1]. Dimension of charge (q) is [I T]. So, [B] = [M L T^-2][I T][L T^-1] = [M L T^-2][I L] = [M T^-2 I^-1]. Radius (r): Dimension of length. So, [r] = [L]. Now, let's check the dimensions of the right-hand side (RHS) of the equation = (2U)/(B^2 r^2). The constant '2' is dimensionless. [RHS] = ([U])/([B]^2 [r]^2) Substitute the dimensions: RHS] = [M L^2 T^-3 I^-1^2 [L]^2 [RHS] = [M L^2 T^-3 I^-1][M^2 T^-4 I^-2] [L^2] Combine the terms: [RHS] = [M^1-2 L^2-2 T^-3-(-4) I^-1-(-2)] [RHS] = [M^-1 L^0 T^1 I^1] [RHS] = [M^-1 T I] The dimension of the left-hand side (LHS) is [] = [M^-1 I T]. Since [LHS] = [RHS], the equation is dimensionally homogeneous. b. Explain the meaning of the statement: "All correct equations must be homogeneous but not all homogeneous equations are physically correct." "All correct equations must be homogeneous": This part means that for any equation to accurately describe a physical phenomenon, the dimensions of all terms on both sides of the equation must be identical. This principle ensures that we are comparing or equating quantities of the same physical nature (e.g., length with length, energy with energy). If an equation is not dimensionally homogeneous, it is fundamentally incorrect. "but not all homogeneous equations are physically correct": This part indicates that dimensional homogeneity is a necessary condition for a physical equation to be correct, but it is not a sufficient condition. An equation can be dimensionally consistent yet still be physically incorrect. This can happen if the equation contains incorrect numerical constants, misses certain variables, or expresses an incorrect relationship between variables. Example: Consider the equation for kinetic energy. The physically correct equation is KE = (1)/(2)mv^2. Let's check its dimensions: [KE] = [M L^2 T^-2] [(1)/(2)mv^2] = [M][L T^-1]^2 = [M L^2 T^-2] This equation is dimensionally homogeneous and physically correct. Now consider a hypothetical equation KE = mv^2. Let's check its dimensions: [KE] = [M L^2 T^-2] [mv^2] = [M][L T^-1]^2 = [M L^2 T^-2] This equation is also dimensionally homogeneous. However, it is physically incorrect because it lacks the constant factor of (1)/(2). This example demonstrates that an equation can be dimensionally homogeneous but not physically correct. 2. Heat Transfer and Equilibrium Temperature Given: Mass of steam m_s = 75 \, g = 0.075 \, kg. Initial temperature of steam T_s = 100^ C. Latent heat of vaporization of steam L_v = 2260 \, kJ/kg = 2.26 × 10^6 \, J/kg. Latent heat of fusion of ice L_f = 334 \, kJ/kg = 3.34 × 10^5 \, J/kg. Specific heat capacity of water c_w = 4186 \, J/(kg^). The problem states that the heat given out by the steam in condensing to water at 100^ C is just sufficient to melt the ice. This means the steam condenses, and the resulting water is at 100^ C. The ice melts, and the resulting water is at 0^ C. a. Calculate the mass of the ice. Step 1: Calculate the heat released by the condensing steam. The heat released (Q_steam) when steam condenses to water at the same temperature is given by Q_steam = m_s L_v. Q_steam = (0.075 \, kg) × (2.26 × 10^6 \, J/kg) Q_steam = 169500 \, J Step 2: Calculate the mass of the ice melted. The heat required (Q_ice) to melt ice at 0^ C into water at 0^ C is given by Q_ice = m_ice L_f. Since Q_steam = Q_ice: m_ice L_f = 169500 \, J m_ice = 169500 \, J3.34 × 10^5 \, J/kg m_ice ≈ 0.507485 \, kg m_ice ≈ 507.5 \, g The mass of the ice is 507.5 g. b. Calculate the equilibrium temperature of the mixture in the calorimeter. After the initial heat exchange, we have: Water from condensed steam: m_s = 0.075 \, kg at 100^ C. Water from melted ice: m_ice = 0.507485 \, kg at 0^ C. These two quantities of water will now mix and reach an equilibrium temperature, T_f. Assuming no heat loss to the surroundings (insulated calorimeter), the heat lost by the hot water equals the heat gained by the cold water. Step 1: Set up the heat balance equation. Heat lost by hot water (Q_lost) = m_s c_w (100^ C - T_f). Heat gained by cold water (Q_gained) = m_ice c_w (T_f - 0^ C). Since Q_lost = Q_gained: m_s c_w (100 - T_f) = m_ice c_w (T_f - 0) The specific heat capacity of water (c_w) cancels out: m_s (100 - T_f) = m_ice T_f Step 2: Substitute the values and solve for T_f. (0.075 \, kg) (100^ C - T_f) = (0.507485 \, kg) T_f 7.5 - 0.075 T_f = 0.507485 T_f 7.5 = 0.507485 T_f + 0.075 T_f 7.5 = (0.507485 + 0.075) T_f 7.5 = 0.582485 T_f T_f = (7.5)/(0.582485) T_f ≈ 12.876 \, ^ T_f ≈ 12.9 \, ^ The equilibrium temperature of the mixture is 12.9 ^. 3 done, 2 left today. You're making progress.