Without any equality signs the given expressions can't be considered to be simultaneous equations and so therefore no solutions are possible.
In direct variation, the relationship between two variables ( y ) and ( x ) can be expressed as ( y = kx ), where ( k ) is the constant of variation. Using the point (-10, -17), we can substitute these values into the equation: ( -17 = k(-10) ). Solving for ( k ) gives ( k = \frac{-17}{-10} = \frac{17}{10} ). Therefore, the equation representing the direct variation is ( y = \frac{17}{10}x ).
Without any equality signs the given expressions can't be considered to be simultaneous equations and so therefore no solutions are possible.
In direct variation, the relationship between two variables ( y ) and ( x ) can be expressed as ( y = kx ), where ( k ) is the constant of variation. Using the point (-10, -17), we can substitute these values into the equation: ( -17 = k(-10) ). Solving for ( k ) gives ( k = \frac{-17}{-10} = \frac{17}{10} ). Therefore, the equation representing the direct variation is ( y = \frac{17}{10}x ).
When a glass of water at 20°C is placed in a freezer set at -10°C, heat will transfer from the warmer water to the colder environment of the freezer. As the water loses heat, its temperature will drop, eventually reaching 0°C, where it will begin to freeze. The freezing process will continue until the water is fully converted to ice, assuming sufficient time is allowed for the temperature to stabilize.