Water is combination of:
O hydrogen and olygen
O hellum and oxygen
O oxygen and carbon
O carbon and hydrogen

The statement that "the visible light we see from a flare is only a tiny fraction of the energy it releases" is FALSE.

In fact, visible light makes up a significant portion of the energy released during a flare, along with other forms of electromagnetic radiation such as ultraviolet and X-rays. Your question pertains to identifying the FALSE statement about solar flares. The other FALSE statement is: "Flares originate in the upper part of the corona, in the regions called coronal holes." In reality, flares occur in the Sun's lower atmosphere (chromosphere) and are associated with active regions, not coronal holes.

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A current of 4.21 A is needed to produce a magnetic field of 2.0 × 10−2t within the solenoid with 12 turns per centimeter.

To find the current needed to produce a magnetic field of 2.0 × 10−2t within the solenoid with 12 turns per centimeter, we can use the formula for the magnetic field strength inside a solenoid:

B = μ0 * n * I

Where B is the magnetic field strength, μ0 is the permeability of free space (4π × 10−7 T•m/A), n is the number of turns per unit length (in this case, 12 turns/cm or 120 turns/m), and I is the current flowing through the solenoid.

Rearranging the formula to solve for I, we get:

I = B / (μ0 * n)

Plugging in the values we have, we get:

I = (2.0 × 10−2 T) / (4π × 10−7 T•m/A * 120 turns/m)

I = 4.21 A

Therefore, a current of 4.21 A is needed to produce a magnetic field of 2.0 × 10−2t within the solenoid with 12 turns per centimeter.

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If two populations live very far from each other and are geographically separated, they are different species.

The main effect is that groups will diverge from one another when they are geographically isolated, both in terms of physical appearance and genetic variation.

Reproductive isolation results from these alterations, which might be brought on by genetic drift or natural selection.

The process by which new species emerge is known as speciation. It happens when populations within a species separate and experience reproductive isolation. A period of geographic separation causes groups from an ancestral population to diverge into distinct species in allopatric speciation.

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The mass of water in the pool having a 1.0 m depth at one end to a 3.0 m depth at the other is 144,000 kg.

The average depth of the pool can be calculated as (1.0 m + 3.0 m) / 2 = 2.0 m.

The length and width of the pool are given as 6 m and 12 m, respectively.

To find the volume of the pool, we can use the formula for the volume of a rectangular prism: Volume = Length x Width x Height.

Volume =[tex]6 m * 12 m * 2.0 m[/tex] = 144 m³.

The density of water is approximately 1000 kg/m³.

Therefore, the mass of water in the pool is Mass = Volume x Density = 144 m³ x 1000 kg/m³ = 144,000 kg.

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Main Answer: The mass of a moving electron traveling by you at v = 0.85c is larger than the rest mass of the electron.

Supporting Answer: According to Einstein's theory of special relativity, the mass of a moving object increases as its velocity approaches the speed of light. The formula for the relativistic mass of an object is given by:

m = m0 / sqrt(1 - v^2/c^2)

Where m0 is the rest mass, v is the velocity of the object, and c is the speed of light.

Substituting the given values, we get:

m = 9.11 x 10^-31 kg / sqrt(1 - 0.85^2)

m = 1.84 x 10^-30 kg

Therefore, the mass of a moving electron traveling by you at v = 0.85c is larger than the rest mass of the electron.

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The potential energy of the 5kg cinder block at a 20m scaffolding is 980 Joules.

The potential energy of an object is given by the formula PE = mgh, where m is the mass of the object (5kg), g is the acceleration due to gravity (9.8 m/s²), and h is the height (20m). Plugging in these values, we get PE = 5kg * 9.8 m/s² * 20m = 980 Joules. So, the cinder block has 980 Joules of potential energy due to its position above the ground.

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The magnetic field in the region where the hall probe gives a reading of 2μV for 1.7A of current is 1.78T.

The magnetic field in a region where the hall probe gives a reading of 2μV for 1.7A of current can be calculated as 1.7/2 times the magnetic field in the region where the reading is 1.5μV for 2A of current.

First, we can use the formula B = (V/I)/(1/RH) where B is the magnetic field, V is the voltage reading, I is the current, and RH is the Hall coefficient of the probe.

In the first region, B₁ = (1.5 μV/2A)/(1/RH)

In the second region, B₂ = (2 μV/1.7A)/(1/RH)

We can rearrange the equations to solve for RH and set them equal to each other:

RH = (1.5 μV/2A) / B₁ = (2 μV/1.7A) / B₂

Solving for B₂, we get:

B₂ = (2 μV/1.7A) / [(1.5 μV/2A) / B₁] = 1.78T

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The area is reduced by 1/3, the resistance will increase by a factor of 3. Therefore, the new resistance is 3R * 3 = 9R.

The resistance of a conductor is given by the formula R = ρ (L/A), where ρ is the resistivity, L is the length, and A is the cross-sectional area. Since the volume remains the same, the product of length and area should remain constant. When the length is tripled, the cross-sectional area must be reduced by a factor of 1/3 to maintain the volume. The resistance is inversely proportional to the cross-sectional area, so if the area is reduced by 1/3, the resistance will increase by a factor of 3. Therefore, the new resistance is 3R * 3 = 9R.

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The given statement "Contextual interference is interference introduced into the practice session through the use of massed practice schedule" is FALSE because it introduced into the practice session through the use of varied or random practice schedules, not massed practice schedules.

It is a phenomenon where learning is more challenging due to the mixing of various skills, but it often leads to better long-term retention and skill transfer.

Massed practice, on the other hand, involves repetitive practice of a single skill in a short amount of time without introducing variations, which can sometimes lead to quicker short-term improvements but may not enhance long-term retention as effectively as varied practice schedules.

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The net force acting on a van with a mass of 1500 kg, accelerating at a rate of 3.5 m/s² in the forward direction, needs to be determined.

The net force acting on an object is calculated using Newton's second law of motion, which states that force (F) is equal to mass (m) multiplied by acceleration (a). In this case, the mass of the van is given as 1500 kg, and the acceleration is 3.5 m/s². Plugging these values into the formula, we get:

[tex]F = m * a[/tex]

[tex]F = 1500 kg * 3.5 m/s^2[/tex]

[tex]F = 5250 kg*m/s^2[/tex]

Therefore, the net force acting on the van is 5250 kg⋅m/s². It's important to note that the unit of force is the Newton (N), which can be derived from the unit kg⋅m/s². So, the net force acting on the van is 5250 N.

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The statement given "The vast majority of stars near us would fall to the bottom right on the H-R diagram." is false because the Hertzsprung-Russell (H-R) diagram is a graph that plots stars based on their luminosity (brightness) and temperature.

On the H-R diagram, stars are typically distributed in different regions based on their characteristics. The majority of stars near us would not fall to the bottom right on the H-R diagram. The bottom right region of the diagram is occupied by hot, high-luminosity stars known as "supergiants." However, the vast majority of stars near us are not supergiants but rather belong to other categories such as main sequence stars, red giants, or white dwarfs. Therefore, the statement is false.

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To compare the average density of Betelgeuse with the Sun, given that Betelgeuse has a mass 25 times that of the Sun, we will use the density formula: density = mass/volume, where the volume is that of a sphere.

Step 1: Determine the ratio of the masses.

Since Betelgeuse has a mass 25 times that of the Sun, the mass ratio is 25:1.

Step 2: Find the ratio of the volumes.

For spheres, volume is given by the formula V = (4/3)πr³. To find the ratio of the volumes, we need to find the ratio of the radii cubed. Betelgeuse has a radius approximately 900 times that of the Sun. Therefore, the radius ratio is 900:1.

Step 3: Cube the radius ratio.

Cubing the radius ratio, we get (900³):(1³) = 729,000,000:1. This is the ratio of the volumes.

Step 4: Calculate the density ratio.

Using the mass ratio (25:1) and the volume ratio (729,000,000:1), we can find the density ratio: (density of Betelgeuse)/(density of the Sun) = (25/729,000,000).

Step 5: Simplify the density ratio.

Simplifying the density ratio, we get (1/29,160,000).

So, the average density of Betelgeuse is 1/29,160,000 times the density of the Sun. This means Betelgeuse is much less dense than the Sun.

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The differential Equation of Motion for the center of mass position, using the x-coordinate parallel to the inclined surface is: a = (2/3)g sinθ - (2/3)μg cosθ.

The gravitational force acting on the disk can be split into two components: one perpendicular to the inclined plane, which we'll call N (the normal force), and one parallel to the inclined plane, which we'll call Mg sinθ (where θ is the angle of inclination).

There is also a force of static friction acting on the disk, opposing its motion down the plane. The frictional force can be found as,
f = μN,
where μ is the coefficient of static friction.

Now, let's consider the motion of the disk. Since the disk is rolling without slipping, we can relate the linear velocity v of the center of mass to the angular velocity ω of the disk as,
v = Rω,
where R is the radius of the disk.

The Equation of Motion for the center of mass position can be derived from the sum of forces acting on the disk. We have:
Ma = Mg sinθ - f
where M is the mass of the disk,
a is the acceleration of the center of mass, and
we have used Newton's second law.

To relate the acceleration to the angular velocity, we can use the fact that the tangential acceleration of a point on the rim of the disk is a = Rα, where α is the angular acceleration. We also have the rotational analog of Newton's second law:
Iα = fR
where I is the moment of inertia of the disk about its center of mass.

Substituting the expression for f from above and using the relationship between linear and angular velocity, we get:
Iα = μN R
M(Rα) = Mg sinθ - μN

Substituting α = a/R and I = (1/2)MR^2, we can simplify the equation to:
a = (2/3)g sinθ - (2/3)μg cosθ

This is the differential equation of motion for the center of mass position of the rolling disk on an inclined plane, including a free body diagram.

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The energy required to melt 16.4 g of ice at 0 ⁰C is 5.46 kJ.

To melt 16.4 g of ice at 0 ⁰C, we need to use the formula:

Energy = mass x ΔH fus

Where ΔH fus is the enthalpy of fusion of water, which is 6.01 kJ/mol.

First, we need to convert the mass of ice from grams to moles:

16.4 g / 18.015 g/mol = 0.91 mol

Next, we can calculate the energy required to melt the ice:

Energy = 0.91 mol x 6.01 kJ/mol = 5.46 kJ

Therefore, the energy required to melt 16.4 g of ice at 0 ⁰C is 5.46 kJ.

It's important to include the units in our answer to make it clear what we are measuring. In this case, the units are in kilojoules (kJ).

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The main answer to A) is that box D experiences the largest change in kinetic energy. This is because the change in kinetic energy is directly proportional to the mass of the object and the square of its velocity.

Box D has the largest mass, so it requires more energy to be pushed and moves at a higher velocity than the other boxes. Therefore, it experiences the largest change in kinetic energy.

The main answer to B) is that box C experiences the smallest change in kinetic energy. This is because the change in kinetic energy is directly proportional to the mass of the object and the square of its velocity. Box C has the smallest mass, so it requires less energy to be pushed and moves at a lower velocity than the other boxes. Therefore, it experiences the smallest change in kinetic energy.

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The answer for A 8.0-cm radius disk with a rotational inertia is A. 0.50 m/s^2, which is less than 1 g.

To solve this problem, we can use the equation τ = Iα, where τ is the torque applied, I is the rotational inertia, and α is the angular acceleration.
First, we need to find the angular acceleration. We know that the torque applied is 9.0 N·m and the rotational inertia is 0.12 kg·m^2, so we can plug these values into the equation and solve for α:
τ = Iα
9.0 N·m = 0.12 kg·m^2 α
α = 75 rad/s^2
Next, we need to find the linear acceleration of the mass. We can use the equation a = rα, where a is the linear acceleration, r is the radius of the disk, and α is the angular acceleration we just found:
a = rα
a = 0.08 m × 75 rad/s^2
a = 6.0 m/s^2
Finally, we need to divide the linear acceleration by the acceleration due to gravity to get the answer in terms of g's:
a/g = 6.0 m/s^2 / 9.81 m/s^2 ≈ 0.61 g's

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The initial mass m is approximately 2.2 kg, and the spring constant k is approximately 10.8 N/m.

To solve this problem, we'll use the formula for the period of a spring-block system:

T = 2π√(m/k)

where T is the period, m is the mass, and k is the spring constant. 1)

For the initial mass m, T1 = 3.8 s. So, 3.8 = 2π√(m/k). 2)

For the increased mass (m + 1.8 kg), T2 = 8.6 s.

So, 8.6 = 2π√((m + 1.8)/k).

We have two equations and two unknowns (m and k).

To find m, we can first solve for k in equation 1:

k = (2πm/3.8)².

Now, substitute this expression for k in equation 2:

8.6 = 2π√((m + 1.8)/((2πm/3.8)²))

Solving for m, we get m ≈ 2.2 kg.

Next, find the spring constant k using the expression for k from equation 1:

k ≈ (2π(2.2)/3.8)² ≈ 10.8 N/m.

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Without further information or context, it is impossible to determine the proportions of sand, silt, and clay at point t.

Soil composition can vary greatly depending on location, climate, and geological history. Soil scientists use a variety of methods to determine the proportions of different soil particles, such as texture-by-feel analysis, which involves rubbing soil between fingers to determine the relative proportions of sand, silt, and clay. Other methods include laser diffraction and X-ray diffraction. Understanding the soil composition can help inform land use and management decisions, as different soils have varying water-holding capacities, nutrient availability, and erosion potential. It is important to gather specific information about the location in question to accurately determine soil composition.

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The frequency of revolution of an electron around the nucleus of a hydrogen atom can be determined using the equation: f = (1/2π) * (k*[tex]e^{2}[/tex])/(h*n*m)

Where f is the frequency, k is Coulomb's constant, e is the charge of the electron, h is Planck's constant, n is a quantum number, and m is the mass of the electron. Plugging in the values, we get: f = (1/2π) * (8.988×[tex]10^{9}[/tex] N⋅[tex]m^{2}[/tex]/[tex]C^{2}[/tex]) * (1.602×[tex]10^{-19}[/tex] [tex]C^{2}[/tex]) / (6.626×10^-34 J⋅s) * (n) * (9.109×[tex]10^{-31}[/tex] kg). Simplifying, we get: f = (3.29×[tex]10^{15}[/tex] Hz) / n. Therefore, the frequency of revolution of an electron around the nucleus of a hydrogen atom is inversely proportional to the quantum number n. As the value of n increases, the frequency decreases, and the electron moves farther away from the nucleus. Conversely, as the value of n decreases, the frequency increases, and the electron moves closer to the nucleus. This equation is useful in understanding the behavior of electrons in atoms and helps explain the properties of different elements and their chemical reactions.

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The frequency of revolution of an electron around the nucleus of a hydrogen atom. e is the charge of the electron, m is the mass of the electron, and n is a quantum number is expressed as [tex]f = \frac{1}{2\pi} \sqrt{\frac{ke^2}{mn^3}}[/tex]

The frequency of revolution of an electron around the nucleus of a hydrogen atom can be determined using the following formula:

[tex]f = \frac{1}{2\pi} \sqrt{\frac{ke^2}{mn^3}}[/tex]

Where;

Thus, the frequency of revolution of an electron around the nucleus of a hydrogen atom. e is the charge of the electron, m is the mass of the electron, and n is a quantum number is expressed in terms of  e, m, n, the Planck's constant h, and the Coulomb's constant k.

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A-  the average frequency that will be heard is 461 Hz, b-the beat frequency will be 8 Hz.

For part (a), to find the average frequency that will be heard, we can use the formula:
fave = (f1 + f2) / 2
Plugging in the given values, we get:
fave = (457 Hz + 465 Hz) / 2
fave = 461 Hz

For part (b), the beat frequency is the difference between the two frequencies. We can use the formula:
beat frequency = |f1 - f2|
Plugging in the given values, we get:
beat frequency = |457 Hz - 465 Hz|
beat frequency = 8 Hz

This means that the listener will hear a periodic variation in loudness with a frequency of 8 Hz, which is the difference between the two frequencies. This phenomenon is known as beats, and it occurs when two slightly different frequencies are played simultaneously.

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The work done by the gravitational force is negative during the upward motion of the apple as it pops back to the surface of the water.

When the apple is dropped into the water, it initially sinks down due to the force of gravity acting on it. As it reaches the lowest point and starts moving upward, the gravitational force opposes its motion, causing deceleration. During this upward motion, the work done by the gravitational force is negative.

Work is defined as the product of force and displacement, multiplied by the cosine of the angle between them. In this case, the force of gravity and the displacement of the apple are in opposite directions during the upward motion. Since the angle between them is 180 degrees, the cosine of 180 degrees is -1. Therefore, the work done by the gravitational force is negative. It's important to note that during the downward motion of the apple, the work done by the gravitational force is positive, as the force and displacement are in the same direction.

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The rate at which the frictional force on the crate takes energy away from the crate is 160 j/s.

To solve this problem, we need to use the formula:

frictional force = (mass x acceleration)

We know the mass of the crate is 50 kg and it comes to rest in 10 seconds, so the acceleration is:

acceleration = (final velocity - initial velocity) / time
acceleration = (0 - 8) / 10
acceleration = -0.8 m/s^2 (negative because it's slowing down)

Now we can calculate the frictional force:

frictional force = (mass x acceleration)
frictional force = (50 kg) x (-0.8 m/s^2)
frictional force = -40 N (negative because it's opposing the motion)

The rate at which the frictional force takes energy away from the crate is given by the formula:

power = (force x velocity)

We know the force is -40 N (negative because it's opposing the motion) and the initial velocity is 8 m/s. We don't know the final velocity, but we can assume it's close to zero since the crate comes to rest. So we'll use an average velocity of 4 m/s.

power = (force x velocity)
power = (-40 N) x (4 m/s)
power = -160 J/s (negative because it's taking energy away)

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The equation you provided, "line = 25", does not have enough information to determine the slope.

The equation of a line in slope-intercept form is y = mx + b, where m is the slope and b is the y-intercept. The given equation "line = 25" does not have a variable for y or x, so we cannot use the slope-intercept form directly.

Instead, we can think of this equation as a horizontal line that passes through the point (0, 25) on the y-axis. Since a horizontal line has a slope of 0 (the y-values do not change as x-values increase), the slope of the line = 25 is 0. The slope of the line = 25 is 0 (as a decimal, this is 0.000).

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The observed wavelength of light as measured by an Earth observer is 382.3 nm.

This is slightly longer than the emitted wavelength of 374.0 nm, indicating that the star is moving away from us.

This effect, known as redshift, is caused by the Doppler effect and is used by astronomers to measure the motion of stars and galaxies relative to Earth.

The observed wavelength of light, λ', is related to the emitted wavelength of light, λ, and the relative velocity between the source and observer, v, by the formula:
λ' = λ(1 + v/c)
where c is the speed of light in vacuum.

In this case, the star is moving away from the Earth, so v = 2.400 × 108 m/s. The emitted wavelength is λ = 374.0 nm, or 374.0 × 10^-9 m. The speed of light is c = 3.00 × 10^8 m/s.

Plugging these values into the formula, we get:
λ' = λ(1 + v/c) = (374.0 × 10^-9 m)(1 + 2.400 × 10^8 m/s ÷ 3.00 × 10^8 m/s) = 382.3 nm

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The presence of life on Earth by the time the heavy bombardment ended offers evidence to support the hypothesis that life arises relatively easily under the conditions that existed on the early Earth.

The heavy bombardment period on Earth, which lasted from about 4.6 to 3.8 billion years ago, was characterized by intense asteroid and comet impacts that would have had a catastrophic effect on any existing life. However, the fact that life was present on Earth by the time this period ended suggests that life arose relatively easily under the conditions that existed at that time. This indicates that the early Earth must have provided favorable conditions, such as the presence of water and necessary organic molecules, for life to originate and survive despite such a hostile environment.

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If a monopolist is regulated to charge an efficient price, there would be no deadweight loss (DWL) as the price and quantity produced would be the same as in a perfectly competitive market. Therefore, the answer is (a) zero.

In market, the price is equal to the marginal cost (MC) of production, which represents the efficient price.

In a monopoly market, the price is set where marginal revenue (MR) equals marginal cost (MC), which is always higher than the efficient price.

If the regulator sets the price at the efficient level, the monopolist will produce at the same quantity as a perfectly competitive market, and there will be no DWL. Therefore, the answer is (a) zero.

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The transfer function G(s) is stable for the range of K < 0.

To determine the range of K for which the given transfer function G(s) = 3s / (s^4 + 5s^3 + 8s^2 + 3Ks + 9) is stable, we need to use the Routh-Hurwitz stability criterion. The system is stable if all the coefficients in the first column of the Routh array are positive. Here's a step-by-step explanation:

1. Form the characteristic equation by equating the denominator of the transfer function to zero:
s^4 + 5s^3 + 8s^2 + 3Ks + 9 = 0

2. Create the first two rows of the Routh array using the coefficients of the characteristic equation:
Row 1: [1, 8, 9]
Row 2: [5, 3K]

3. Compute the next row (Row 3) by finding the determinants:
Row 3: [(-8 * 3K) / 5, 0] = [(-24K) / 5, 0]

4. To find the range of K that makes the system stable, all the coefficients in the first column should be positive:
1 > 0
5 > 0
(-24K) / 5 > 0

Solving for K in the last inequality:
(-24K) / 5 > 0
K < 0

Thus,K < 0 is the range for stable transfer function G(s).

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The velocity of the fish when it hits the water is 22.3 m/s.

The velocity of the diver is 8.85 m/s.

The height to which the runner’s center of mass is raised during the jump is 0.204 m.

Initial height of the bob is 0.224 m.

1) Speed of the bird, v₁ = 20 m/s

Mass of the fish, m = 2.5 kg

Height of the bird, h₁ = 5 m

The total mechanical energy of the fish before dropping is equal to that after dropping.

Total energy = KE + PE

1/2 mv₁² + mgh₁ = 1/2mv₂² + 0

Multiplying both sides by 2,

v₁² + 2gh₁ = v₂²

Therefore, the velocity of the fish when it hits the water is,

v₂ = √(v₁² + 2gh₁)

v₂ = √(20² + 2 x 9.8 x 5)

v₂ = 22.3 m/s

2) Weight of the diver, W = 740 N

Height from which the board is dropped, h = 10 m

W = mg

Therefore, mass of the diver,

m = W/g

m = 740/9.8

m = 108.82

So, the potential energy of the diver is converted into kinetic energy of the diver.

mgh + 0 = 1/2 mv²

v²= 2gh

Therefore, velocity of the diver is,

v = √2gh

v = √2 x 9.8 x 4

v = 8.85 m/s

3) Velocity of the runner, v = 2 m/s

KE = PE

1/2 mv² = mgh

v²/2 = gh

Therefore, the height to which the runner’s center of mass is raised during the jump is,

h = v²/2g

h = 2²/(2 x 9.8)

h = 0.204 m

4) Speed of the bob, v = 2.2 m/s

Initial height of the bob is,

h = v²/2g

h = (2.2)²/(2 x 9.8)

h = 0.224 m

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When a proton is moved in the direction opposite to an external electric field, the statement that best describes what is happening to the proton in this scenario is "it is moving from high potential to low potential and the electrical potential energy of a system consisting of the proton and the electric field is decreasing."

Potential energy is defined as the energy stored within an object due to its position or configuration. In this case, the proton is moving against the direction of the electric field, which means that it is losing potential energy.

As a result, the electrical energy of the system consisting of the proton and the electric field is also decreasing.

It is important to note that the movement of the proton in this scenario is in opposition to the direction of the electric field, which means that external work is being done on the proton to move it against the field lines.

This work is what causes the decrease in the electrical potential energy of the system.

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When a proton is moved in the opposite direction of an external E-field, it is moving from a region of high electric potential to low electric potential.

The correct statement that describes what is happening to the proton is that it is moving from high potential to low potential, and the electrical potential energy of a system consisting of the proton and the electric field is decreasing. This is because the electric potential energy is proportional to the distance between the proton and the source of the electric field, and moving the proton in the opposite direction of the electric field reduces the distance between them, resulting in a decrease in electric potential energy. In addition, the proton is experiencing a force opposite to the direction of the electric field, which means that the electrical energy of the system is being converted to kinetic energy of the proton. Overall, the movement of the proton in the opposite direction of the electric field results in a decrease in electrical potential energy and an increase in kinetic energy.

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The bulk modulus of the fluid is approximately 2.076 × 10¹² Pa.

To find the bulk modulus of the fluid, we need to use the formula:
Bulk modulus = (change in pressure / (original volume / change in volume))
We are given the initial volume of the fluid as 0.22 m3 and the pressure decrease as 1.7×103pa. We need to convert the change in volume from cm3 to m3, which is 0.18 cm3 = 0.18 × 10^-6 m3.
Bulk modulus = (1.7×103pa / (0.22 m3 / 0.18 × 10^-6 m3))
Bulk modulus = 1.7×103pa / 1.22×10^-4 m3
Bulk modulus = 1.393×10^10 pa
Bulk modulus (B) = -ΔP / (ΔV/V₀)
0.18 cm³ * (1 m/100 cm)³ = 1.8 × 10⁻¹² m³
Now, plug in the values into the formula:
B = -(-1.7 × 10³ Pa) / (1.8 × 10⁻¹² m³ / 0.22 m³)
B = (1.7 × 10³ Pa) / (8.1818 × 10⁻¹²)
Finally, solve for B:
B ≈ 2.076 × 10¹² Pa

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