Potato slices weighing 50 kg is dried from 60% moisture content (wet basis) to 5% moisture content (dry basis). The amount of dried potato slices obtained (in kg) is ............ (Answer in integer)
We are given:
- Initial weight of wet product = 50 kg
- Initial moisture content = 60% (wet basis)
- Final moisture content = 5% (dry basis)
Step 1: Convert initial moisture content from wet basis to dry basis
Moisture content (dry basis) is: \[ MC_{db} = \frac{MC_{wb}}{1 - MC_{wb}} = \frac{0.60}{1 - 0.60} = \frac{0.60}{0.40} = 1.5 \] Step 2: Use drying equation \[ {Final dry weight} = \frac{{Initial wet weight} \times (1 - MC_{wb})}{1 + MC_{db}^{{final}}} \] Here, final moisture content = 5% dry basis = 0.05 \[ {Dry matter in initial sample} = 50 \times (1 - 0.60) = 20 \, {kg} \] Now, dry matter remains constant. So for final dried product: \[ {Final weight} = {dry matter} \times (1 + MC_{db}^{{final}}) = 20 \times (1 + 0.05) = 20 \times 1.05 = 21 \, {kg} \] \[ \boxed{{Final dried weight} = 21 \, {kg}} \]
The \( F_{121} \) value of a known microorganism with \( Z \) value of \( 11^\circ C \) is 2.4 min for 99.9999% inactivation. For a 12D inactivation of the said microorganism at \( 143^\circ C \), the \( F \) value (in min) is .......... (rounded off to 3 decimal places)
Match the following enzymes in Column I with their applications in Column II.
In the figures given below, L and H indicate low and high pressure centers, respectively; PGF, CoF and CeF indicate Pressure Gradient Force, Coriolis Force and Centrifugal Force, respectively; \( V \) is Velocity. [The arrows indicate only the directions but not the magnitudes of the forces and velocity.]
Which of the following is/are the correct representation(s) of the directions of various forces and velocity in the gradient wind balance in the northern hemisphere?
Which of the following is the correct form of the mass divergence form of the continuity equation for a compressible fluid? [In the given equations, \( \rho \) is the density and \( \nabla \) the three-dimensional velocity vector of the fluid.]
[(i)] $\displaystyle \frac{\partial \rho}{\partial t} + \nabla \times (\rho \mathbf{v}) = 0$
[(ii)] $\displaystyle \frac{\partial \rho}{\partial t} + \nabla \cdot (\rho \mathbf{v}) = 0$
[(iii)] $\displaystyle \frac{\partial \mathbf{v}}{\partial t} + \rho \cdot \nabla \mathbf{v} = 0$
[(iv)] $\displaystyle \frac{\partial \rho}{\partial t} + \mathbf{v} \cdot \nabla \rho = 0$
The vertical (depth) profiles for three parameters P1, P2, and P3 in the northern Indian Ocean are given in the figure below. The values along the x-axis are the normalized values of the parameters and y-axis is the depth (m).
Identify the parameters P1, P2, and P3 from the options given below.