A crystal of potassium permanganate is placed into a beaker of water. the next day, the solid color is gone, but the water is evenly colored. this is an example of:________

Answers

Answer 1

This is an example of a dissolution process.

When a crystal of potassium permanganate is placed into water, it dissolves and forms a solution. Potassium permanganate is a highly soluble compound in water.

The solid crystal of potassium permanganate initially has a distinct color, which is usually purple or dark violet. However, as it dissolves in water, the solid color disappears, and the water becomes evenly colored. This happens because the potassium permanganate molecules disperse uniformly throughout the water, leading to a homogeneous solution.

In a solution, the solute particles (potassium permanganate molecules) are dispersed and surrounded by the solvent particles (water molecules). The solute particles mix thoroughly with the solvent particles, resulting in a solution that appears uniformly colored.

The disappearance of the solid color and the even distribution of color throughout the water indicate that the crystal of potassium permanganate has undergone dissolution, forming a homogeneous solution.

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Related Questions

you blow across the open mouth of an empty test tube and produce the fundamental standing wave in the 14.0-cmcm-long air column in the test tube, which acts as a stopped pipe. the speed of sound in air is 344 m/sm/s.

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When you blow across the open mouth of an empty test tube, you create a standing wave in the 14.0 cm-long air column inside the tube. This column of air acts as a stopped pipe. The speed of sound in air is given as 344 m/s. the frequency of the fundamental standing wave in the test tube is 614.3 Hz.

To find the frequency of the fundamental standing wave in the test tube, we can use the formula:
frequency = speed of sound / wavelength

Since the test tube is acting as a stopped pipe, we know that the length of the air column is equal to a quarter of the wavelength of the fundamental standing wave.
So, the wavelength of the fundamental standing wave in the test tube is four times the length of the air column, which is 4 * 14.0 cm = 56.0 cm.

Now, we can substitute the values into the formula:
frequency = 344 m/s / 56.0 cm

Before we can continue, we need to convert the wavelength from centimeters to meters:
56.0 cm = 0.56 m

Now, we can substitute the values and solve for the frequency:
frequency = 344 m/s / 0.56 m = 614.3 Hz

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Why did it take more generations of complete selection to reduce q from 0.1 to 0.01 (a 0.09 change) compared that for a 0.5 to 0.1 reduction (a larger, 0.4 change)? explain.

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In conclusion, the starting frequency of a trait determines how many generations of complete selection are needed to reduce its frequency. A higher starting frequency allows for a faster reduction, while a lower starting frequency requires more generations for the same amount of change.

The reason it took more generations of complete selection to reduce q from 0.1 to 0.01 compared to reducing it from 0.5 to 0.1 is because of the starting frequencies of q.
When starting with a higher frequency of q, such as 0.5, there is a larger pool of individuals with the desired trait. This means that there are more individuals available for selection and reproduction, which can lead to a faster reduction in the frequency of q.
In contrast, starting with a lower frequency of q, such as 0.1, means that there are fewer individuals with the desired trait. This smaller pool of individuals results in a slower rate of selection and reproduction, leading to a slower reduction in the frequency of q.
To put it simply, it is easier and faster to reduce a trait that is more common in a population compared to one that is less common.
In conclusion, the starting frequency of a trait determines how many generations of complete selection are needed to reduce its frequency. A higher starting frequency allows for a faster reduction, while a lower starting frequency requires more generations for the same amount of change.

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4.45 mol of an ideal gas is expanded from 431 k and an initial pressure of 4.20 bar to a final pressure of 1.90 bar, and cp,m=5r/2. calculate w for the following two cases:

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In both cases, the work done by the gas is 15244.6 J.

To calculate the work done by the gas in the two cases, we need to use the ideal gas law and the equation for work done in an expansion.

The ideal gas law is given by:

PV = nRT

The equation for work done in an expansion is given by:

w = -ΔnRT

Let's calculate the work done in each case.

Case 1:

Initial pressure (P1) = 4.20 bar

Final pressure (P2) = 1.90 bar

Number of moles (n) = 4.45 mol

Temperature (T) = 431 K

To calculate the work done, we need to find the change in moles (Δn):

Δn = n2 - n1

Δn = 0 - 4.45

Δn = -4.45 mol

Substituting the values into the equation for work done:

w = -ΔnRT

w = -(-4.45)(8.314 J/(mol·K))(431 K)

w = 15244.6 J

Therefore, in case 1, the work done by the gas is 15244.6 J.

Case 2:

Initial pressure (P1) = 4.20 bar

Final pressure (P2) = 1.90 bar

Number of moles (n) = 4.45 mol

Temperature (T) = 431 K

To calculate the work done, we need to find the change in moles (Δn):

Δn = n2 - n1

Δn = 0 - 4.45

Δn = -4.45 mol

Substituting the values into the equation for work done:

w = -ΔnRT

w = -(-4.45)(8.314 J/(mol·K))(431 K)

w = 15244.6 J

Therefore, in case 2, the work done by the gas is also 15244.6 J.

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Final answer:

One can calculate work done during isobaric or reversible adiabatic expansion of an ideal gas using thermodynamics principles, the ideal gas law, given values for pressure, volume, and mole quantity, and the specific heat capacity at constant pressure.

Explanation:

This problem is about thermodynamics and ideal gases. It can be solved by utilizing the first law of thermodynamics and the ideal gas law, along with the definition of isobaric, or constant pressure process.

The quantity w represents the work done by or on the system. In thermodynamics, work done by an expansion is generally considered to be negative. First, we need to convert our pressure to the same units as R (the ideal gas constant), which in this case is joules, so 1 bar = 100000 Pa.

The work done (w) during an isobaric process is given by w=-P(delta)V, where delta V is the volume change. Finding V1 is done using the ideal gas law equation PV=nRT. Because the process is isobaric, P, n, and R are all constant, simplifying the equation. Solving it, we then substitute back in the values we determined into the isobaric work equation.

The situation is more complex with cp,m=5r/2, which signifies a reversible adiabatic process. In this case, the work done by the system is described by a more complicated equation, which includes an integration over volume and requires knowledge of calculus.

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the net outward electric flux passing through any closed surface is equal to the net charge enclosed by the surface divided by a constant.

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The net outward electric flux passing through a closed surface is equal to the net charge enclosed by the surface divided by a constant.

According to Gauss's Law, the total electric flux passing through a closed surface is directly proportional to the net charge enclosed by that surface. This relationship is mathematically represented as Φ = q/ε₀, where Φ is the net electric flux, q is the net charge enclosed, and ε₀ is a constant known as the electric constant or permittivity of free space.

The electric flux represents the total number of electric field lines passing through a given surface. When a closed surface encloses a charge, the electric field lines originating from the charge will either enter or exit the surface. The net flux passing through the surface is the algebraic sum of these electric field lines.

Gauss's Law states that the net flux passing through the closed surface is proportional to the net charge enclosed. In other words, the more charge enclosed by the surface, the greater the number of electric field lines passing through the surface. The constant ε₀ in the equation represents the ability of a medium to permit the formation of electric fields. It is a fundamental constant in electromagnetism and has a value of approximately 8.85 x 10⁻¹² C²/N·m².

By dividing the net charge enclosed by the constant ε₀, we obtain the net electric flux passing through the closed surface. This relationship provides a useful tool for calculating electric fields and charges in various scenarios, allowing for a better understanding and analysis of electric phenomena.

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