a person has far points of 7.5 m from the right eye and 5.8 m from the left eye. write a prescription for the refractive power of (a) right and (b) left corrective contact lenses.

It takes her approximately 1.43 seconds to reach a speed of 2.00 m/s. The calculation is done using the equation v = u + at, where v is the final velocity (2.00 m/s), u is the initial velocity (0 m/s), a is the acceleration (1.40 m/s²), and t is the time taken.

Given that the initial velocity (u) is 0 m/s and the acceleration (a) is 1.40 m/s², we can use the equation v = u + at to find the time taken (t) to reach a speed of 2.00 m/s.

2.00 m/s = 0 m/s + (1.40 m/s²) * t

Simplifying the equation:

2.00 m/s = 1.40 m/s² * t

Dividing both sides of the equation by 1.40 m/s²:

t = 2.00 m/s / 1.40 m/s² ≈ 1.43 seconds

Therefore, it takes approximately 1.43 seconds for the commuter to reach a speed of 2.00 m/s.

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The blackbody object that peaks at 1,000 nm (just outside the visible spectrum) would appear invisible to the human eye. The answer is b.

The visible spectrum for humans ranges from approximately 400 nm (violet) to 700 nm (red). A blackbody object's perceived color depends on its temperature and the wavelength at which it emits the most radiation. The peak wavelength of the radiation emitted by an object decreases as its temperature increases according to Wien's displacement law.

In this case, a blackbody object that peaks at 1,000 nm has a temperature of approximately 2,897 K. This is outside the range of temperatures that produce visible light.

Therefore, the object would not appear to have any color to the human eye. Instead, it would appear as a dark object, absorbing most of the visible light that strikes it. Hence, b is the right option.

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If the Fed wants to lower the federal funds rate, it should buy government securities in the open market. This will increase the amount of money available in the banking system, leading to a decrease in the federal funds rate.

Selling government securities in the open market would have the opposite effect and raise the federal funds rate. Increasing the reserve ratio would require banks to hold more reserves and would also raise the federal funds rate. Increasing the discount rate would make borrowing from the Fed more expensive, which could indirectly increase the federal funds rate.

If the Fed wants to lower the federal funds rate, it should d. buy government securities in the open market.

By purchasing government securities, the Fed increases the supply of money in the economy. This results in a lower federal funds rate as banks have more funds available for lending, leading to increased demand for loans and lower borrowing costs.

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The change in energy (in joules) of the hot water due to the heat transfer when it is placed in contact with the cold water and allowed to reach equilibrium is -15,464 J.

The change in energy (in joules) of the hot water due to the heat transfer when it is placed in contact with the cold water and allowed to reach equilibrium can be calculated using the equation

Q = mcΔT

Where Q is the heat transferred, m is the mass of the water, c is the specific heat capacity of water, and ΔT is the change in temperature of the water.

For the hot water

m = 1.00 kg

c = 4,186 J/(kg·°C) (specific heat capacity of water)

ΔT = 41.5°C - Teq

Where Teq is the equilibrium temperature of the two bodies.

For the cold water

m = 1.00 kg

c = 4,186 J/(kg·°C) (specific heat capacity of water)

ΔT = Teq - 21°C

Because the heat transfer is from the hot water to the cold water, the magnitude of the heat transferred will be the same for both bodies. Therefore

mcΔT = mcΔT

(1.00 kg)(4,186 J/(kg·°C))(41.5°C - Teq) = (1.00 kg)(4,186 J/(kg·°C))(Teq - 21°C)

Simplifying this equation, we get

83.7 J/°C = Teq - 21°C + Teq - 41.5°C

Combining like terms, we get

2Teq - 62.5°C = 83.7 J/°C

Solving for Teq, we get

Teq = (83.7 J/°C + 62.5°C)/2

Teq = 73.1°C

Therefore, the change in energy (in joules) of the hot water due to the heat transfer when it is placed in contact with the cold water and allowed to reach equilibrium is

Qh = mcΔT = (1.00 kg)(4,186 J/(kg·°C))(41.5°C - 73.1°C) = -15,464 J

(Note that the negative sign indicates that the hot water loses energy, as expected.)

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Based on the terms and information provided, here is a breakdown of the properties for asteroids and Kuiper Belt Objects (KBOs):

1. Vesta: This is a property of asteroids, as Vesta is one of the largest asteroids in the asteroid belt between Mars and Jupiter.

2. Similar in composition to comets (mostly rock and metals): This is a property of asteroids, as they are primarily composed of rock and metals, whereas KBOs are mostly composed of ices.

3. Majority are small bodies: This is a property of both asteroids and KBOs, as both types of objects consist of numerous small celestial bodies.

4. Mostly reside in a belt between Mars and Jupiter: This is a property of asteroids, as the asteroid belt is located between the orbits of Mars and Jupiter.

5. Mostly reside in a belt extending 20 AU beyond the orbit of Neptune: This is a property of KBOs, as the Kuiper Belt extends from about 30 to 50 AU from the Sun.

6. Pluto: This is a property of KBOs, as Pluto is considered a dwarf planet and is located within the Kuiper Belt.

7. Similarities to some moons: This is a property of both asteroids and KBOs, as both types of objects can have characteristics and compositions similar to certain moons in our solar system.
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The largest allowable length of the aluminum bar ab would be determined by the maximum length that maintains the required diameter for each centric load magnitude.

To determine the largest allowable length of the aluminum bar ab for a centric load of magnitude (a) 150 kn, (b) 90 kn, (c) 25 kn using aluminum alloy 2014-t6, we need to use the formula for the maximum allowable stress:
σ = P / A
Where σ is the maximum allowable stress, P is the centric load magnitude, and A is the cross-sectional area of the aluminum bar.
For aluminum alloy 2014-t6, the maximum allowable stress is 324 MPa.
(a) For a centric load of 150 kn, the cross-sectional area required would be:
A = P / σ = (150,000 N) / (324 MPa) = 463.0 mm^2
Using the formula for the area of a circle, we can determine the diameter of the required aluminum bar:
A = πd^2 / 4
d = √(4A / π) = √(4(463.0 mm^2) / π) = 24.3 mm
Therefore, the largest allowable length of the aluminum bar ab would be determined by the maximum length that maintains a diameter of 24.3 mm.
(b) For a centric load of 90 kn, the required diameter would be:
d = √(4(90,000 N) / π(324 MPa)) = 19.8 mm
(c) For a centric load of 25 kn, the required diameter would be:
d = √(4(25,000 N) / π(324 MPa)) = 12.1 mm

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In Part A, the electron's speed is given as 4.00 km/s and the force acting on it due to the electric field is 5.50×10−15N. To find the acceleration produced by this force,

we can use the equation F = ma, where F is the force, m is the mass of the electron, and a is the acceleration. As the mass of the electron is very small,

we can use the equation a = F/m. Therefore, the acceleration produced by this force in Part A is:

a = F/m = (5.50×10−15N) / (9.11×10−31kg) = 6.04×10^15 m/s^2

In Part B, the force acting on the electron is parallel to its velocity. This means that the force does not change the direction of the electron's motion, but only its speed.

As the electron is moving with a constant velocity, we can assume that its acceleration is zero. This means that the force acting on the electron must be balanced by another force,

such as a magnetic force, that prevents the electron from changing its direction of motion. Therefore, the acceleration produced by the force in Part B is zero.

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If two concave lenses, each with f = -17 cm, are separated by 8.5 cm. An object is placed 35 cm in front of one of the lenses, then a) The final image distance is -23.2 cm. b) The magnification of the final image is 1.6.

a) We can use the thin lens equation to find the image distance and magnification for each lens separately, and then use the lensmaker's formula to combine the two lenses.

For each lens, the thin lens equation is:

1/f = 1/do + 1/di

where f is the focal length, do is the object distance, and di is the image distance.

Plugging in f = -17 cm and do = 35 cm, we get:

1/-17 cm = 1/35 cm + 1/di1

Solving for di1, we get:

di1 = -23.3 cm

The magnification for each lens is:

m1 = -di1/do = -(-23.3 cm)/35 cm = 0.67

Using the lensmaker's formula, we can find the combined focal length of the two lenses:

1/f = (n-1)(1/R1 - 1/R2 + (n-1)d/(nR1R2))

where n is the index of refraction, R1 and R2 are the radii of curvature of the two lens surfaces, and d is the thickness of the lens.

Since the two lenses are identical, we have R1 = R2 = -17 cm and d = 8.5 cm. Also, for simplicity, we can assume that the index of refraction is 1.

Plugging in these values, we get:

1/f = -2/R1 + d/R1²

Solving for f, we get:

f = -17.0 cm

So the combined focal length is still -17 cm.

We can now use the thin lens equation again, with f = -17 cm and di1 = -23.3 cm as the object distance for the second lens:

1/-17 cm = 1/-23.3 cm + 1/di2

Solving for di2, we get:

di2 = -13.8 cm

The magnification for the second lens is:

m2 = -di2/di1 = -(-13.8 cm)/(-23.3 cm) = 0.59

b) To find the total magnification, we multiply the individual magnifications:

m = m1 × m2 = 0.67 × 0.59 = 1.6

So the final image is upright and magnified, and its distance from the second lens is -13.8 cm, which means its distance from the first lens is:

di = di1 + d1 + di2 = -23.3 cm + 8.5 cm - 13.8 cm = -28.6 cm

Since the object is on the same side of the first lens as the final image, the image distance is negative, which means the image is virtual and on the same side of the lens as the object.

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Using AC current in an electromagnet affects the compass by causing it to oscillate or rapidly change direction.

This is because AC current alternates its direction of flow periodically. When the current flows through the electromagnet, it generates a magnetic field that changes direction along with the alternating current. As a result, the compass needle, which is sensitive to magnetic fields, will continuously change its direction in response to the fluctuating magnetic field created by the electromagnet.

In contrast to DC current, which produces a steady magnetic field, AC current creates a constantly changing magnetic field due to the alternating nature of the current. When an electromagnet is powered by AC current, its magnetic field will continuously change direction, causing the compass needle to rapidly change direction as well. This occurs because the compass needle aligns itself with the magnetic field generated by the electromagnet. The rapidly changing magnetic field can make it difficult to obtain a stable reading from the compass, as the needle will not settle in one direction.

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The speed of the wave on the string can be calculated by multiplying the frequency (60.00 Hz) with the wavelength (2.00 cm), which gives us a result of 120 cm/s.

To further explain, the speed of a wave is defined as the distance traveled by a wave per unit time. In this case, we have a frequency of 60.00 Hz, which means that the wave produces 60 cycles per second. The wavelength, on the other hand, is the distance between two consecutive points of the wave that are in phase with each other. So, with a wavelength of 2.00 cm, we know that the distance between two consecutive points that are in phase is 2.00 cm.

By multiplying these two values, we get the speed of the wave on the string, which is 120 cm/s. This means that the wave travels at a speed of 120 cm per second along the length of the string.

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To express the rate of climb of a mountain trail with no units, you can simply state it as a ratio or fraction: 1/8.33. This means that for every 8.33 units traveled horizontally, the trail ascends 1 unit vertically.

The rate of climb of 120 meters per kilometer can be expressed with no units as a ratio or fraction: 1/8.33. This ratio signifies that for every 8.33 units traveled horizontally (in any unit of distance), the trail ascends 1 unit vertically (in any unit of elevation). By removing the specific units (meters per kilometer), we create a dimensionless quantity that can be used universally. This allows for easier comparison and understanding of the rate of climb, regardless of the specific units used to measure distance and elevation.

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The energy absorbed by 30.0 g of water in heating it from 0.0°C to 100.0°C is 12.7 kJ. Changing the rate at which heat is added from 50 J/s to 100 J/s does not affect this calculation since the energy required to raise the temperature of a substance is independent of the rate at which it is added.

In more detail, the energy absorbed in heating a substance is given by the equation Q = mCΔT, where Q is the energy absorbed, m is the mass of the substance, C is the specific heat capacity of the substance, and ΔT is the change in temperature. For water, the specific heat capacity is 4.18 J/g°C. Therefore, the energy absorbed in heating 30.0 g of water from 0.0°C to 100.0°C is:

Q = (30.0 g)(4.18 J/g°C)(100.0°C - 0.0°C) = 12,540 J = 12.7 kJ

Changing the rate at which heat is added, such as from 50 J/s to 100 J/s, does not affect the amount of energy required to raise the temperature of the water since the energy required is dependent only on the mass, specific heat capacity, and temperature change of the substance, and is independent of the rate at which it is added.

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In which direction is the centripetal acceleration directed on a particle that is moving along a circular trajectory?

Centripetal acceleration is always directed towards the center of the circular path in which the particle is moving. This inward direction ensures that

the particle constantly changes its velocity as it moves along the circular trajectory, even if its speed remains constant.

The centripetal acceleration is responsible for maintaining the particle's circular motion by continuously altering its direction.

To further understand this concept, consider these steps:

1. As the particle moves along the circular path, it has both a linear velocity (tangential to the circle) and an angular velocity (change in angle per unit time).

2. The centripetal force, acting perpendicular to the linear velocity, is responsible for the change in direction of the particle as it moves.

3. The centripetal acceleration is the result of this centripetal force acting on the particle. It is given by the formula: a_c = (v^2) / r, where a_c is the centripetal acceleration,

v is the linear velocity, and r is the radius of the circular path.

4. Since the centripetal acceleration is always directed towards the center of the circle, it ensures that the particle remains in its circular trajectory.

In conclusion, the centripetal acceleration is directed towards the center of the circular path in which a particle moves.

This inward direction enables the particle to maintain its circular motion by continuously adjusting its velocity.

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If r is a primitive root modulo m, then its inverse r(bar) is also a primitive root modulo m.

Let's assume that r is a primitive root modulo m. This means that the set of residues generated by r modulo m is a complete residue system, i.e., it covers all the numbers from 1 to [tex]m^{-1[/tex].

Now, let's consider the inverse of r, denoted as r(bar). By definition, r(bar) is the number such that:

r × r(bar) ≡ 1 (mod m).

To show that r(bar) is also a primitive root modulo m, we need to prove that the set of residues generated by r(bar) modulo m is also a complete residue system.

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To find the particle's speed, we can use the de Broglie wavelength equation:

λ = h/p

where λ is the de Broglie wavelength, h is Planck's constant, and p is the momentum of the particle. We can rearrange this equation to solve for the momentum:

p = h/λ

Now we can use the momentum and the mass of the particle to find its speed:

v = p/m

where v is the speed and m is the mass.

Plugging in the given values, we get:

p = (6.626 x 10^-34 J s)/(7.25 x 10^-12 m) = 9.13 x 10^-23 kg m/s

v = (9.13 x 10^-23 kg m/s)/(6.68 x 10^-27 kg) = 1.37 x 10^4 m/s

Therefore, the particle's speed is 1.37 x 10^4 m/s.

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The car stereo's sound waves transfer energy to the particles in the window, causing them to vibrate and resulting in the vibrations of the window. This phenomenon demonstrates the interaction between sound waves, particles, vibration, and energy.

When music is played through a car stereo, it generates sound waves that travel through the air as a series of compressions and rarefactions. These sound waves consist of alternating high-pressure regions (compressions) and low-pressure regions (rarefactions). As the sound waves reach the window, they encounter the particles present in the window's material.

The sound waves transfer their energy to these particles as they collide with them. This energy causes the particles to vibrate rapidly. The vibrations of the particles are then transmitted to the window, causing it to vibrate as well. The vibrations in the window create oscillations in the air on the other side of the window, which can be perceived as sound by our ears.

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According to the kinetic molecular theory of gases, the volume of the gas particles, which can be atoms or molecules, is considered to be negligible compared to the volume of the container that they occupy. The gas particles are assumed to be point masses.

This assumption is based on the fact that at normal temperatures and pressures, the space between gas particles is much larger than the size of the particles themselves. Therefore, the particles can be treated as point masses without significantly affecting the overall behavior of the gas.

The kinetic molecular theory of gases provides a useful framework for understanding the behavior of gases at the molecular level, and helps to explain many of the observed properties of gases, such as their pressure, volume, temperature, and the relationships between them, such as the ideal gas law.

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The answer is C.) it will take approximately 600 days for the sample to contain 1.25×1011 radioactive nuclei.


The half-life of the radioactive material is 200 days, which means that after 200 days, half of the original nuclei will have decayed. So, after another 200 days (a total of 400 days), half of the remaining nuclei will have decayed, leaving 1/4 of the original nuclei.

We can set up an equation to solve for the time it will take for the sample to contain 1.25×1011 radioactive nuclei:

1×1012 * (1/2)^(t/200) = 1.25×1011

Where t is the number of days.

Simplifying this equation, we can divide both sides by 1×1012 and take the logarithm of both sides:

(1/2)^(t/200) = 1.25×10^-1

t/200 = log(1.25×10^-1) / log(1/2)

t/200 = 3

t = 600

Therefore, it will take 600 days for the sample to contain 1.25×1011 radioactive nuclei.

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Answer:

The surface a drawing is created on is called support

The center of Lake Superior is depressed by 5.2 meters due to the centrifugal force at a radius of 162 km and a latitude of 47°.

When a body rotates, objects on its surface are subject to centrifugal force which causes them to move away from the center.

In this case, Lake Superior is assumed to be at rest with respect to Earth and a circle of radius 162 km at a latitude of 47° is drawn around it.

Using the formula for centrifugal force, the depth that the center of the lake is depressed with respect to the shore is calculated to be 5.2 meters.

This means that the water at the center of Lake Superior is pushed outwards due to the centrifugal force, causing it to be shallower than the shore.

Understanding the effects of centrifugal force is important in many areas of science and engineering.

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The proton needs to be fired toward the lead target with an initial kinetic energy of 25.2 MeV.

To impact a lead of accelerators nucleus with 20 MeV of kinetic energy, a proton must be fired at the nucleus with a specific amount of initial kinetic energy. In this case, the required initial kinetic energy is 25.2 MeV.

To understand why this is the case, it's important to consider the nature of the nuclear reactions that occur when a proton impacts a nucleus. In order for the proton to penetrate the nucleus, it must have enough kinetic energy to overcome the electrostatic repulsion between the positively charged proton and the positively charged nucleus. This kinetic energy is determined by the velocity of the proton as it approaches the nucleus.

The specific amount of initial kinetic energy required to achieve the desired kinetic energy of the proton upon impact depends on a number of factors, including the mass of the target nucleus and the desired kinetic energy of the proton upon impact.

In this case, the 207 Pb nucleus is relatively heavy, which means that the proton must be fired with a higher initial kinetic energy in order to achieve the desired kinetic energy upon impact. The exact value of 25.2 MeV is calculated based on the mass of the lead nucleus and the desired kinetic energy of the proton upon impact.

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Answer:

12×8=848

Explanation:

repell forces

(a) 64.7° is the acceptance angle (in degrees) for the oil immersion objective

(b) 30° is the acceptance angle (in degrees) for the air immersion objective.

Part (a): The acceptance angle for the oil immersion objective can be calculated using the formula α1 = sin⁻¹(NA1/n), where NA1 is the numerical aperture of the objective and n is the refractive index of the medium between the specimen and the objective. Here, NA1 = 1.40 and n = 1.51 (refractive index of oil). Substituting these values, we get α1 = sin⁻¹(1.40/1.51) = 64.7°.
Part (b): The acceptance angle for the air immersion objective can be calculated using the formula α2 = sin⁻¹(NA2/n), where NA2 is the numerical aperture of the objective and n is the refractive index of the medium between the specimen and the objective. Here, NA2 = 0.5 and n = 1 (refractive index of air). Substituting these values, we get α2 = sin⁻¹(0.5/1) = 30°.
In summary, the acceptance angle for the oil immersion objective is 64.7°, while the acceptance angle for the air immersion objective is 30°. This difference in acceptance angle is due to the fact that oil has a higher refractive index than air, which allows for greater light refraction and therefore a larger acceptance angle.

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(a) The work necessary to bring a 101 kg object to a height of 992 km above the surface of the Earth is 986 MJ. (b) The extra work needed to launch the object into circular orbit at a height of 992 km above the surface of the Earth is 458 MJ.

To bring an object to a height of 992 km above the surface of the Earth, we need to do work against the force of gravity. The work done is given by the formula;

W = mgh

where W is work done, m is mass of the object, g is acceleration due to gravity, and h is the height above the surface of the Earth.

Using the given values, we have;

m = 101 kg

g = 9.81 m/s²

h = 992 km = 992,000 m

W = (101 kg)(9.81 m/s²)(992,000 m) = 9.86 × 10¹¹ J

Converting J to MJ, we get;

W = 986 MJ

Therefore, the work necessary to bring a 101 kg object to a height of 992 km above the surface of the Earth is 986 MJ.

To launch the object into circular orbit at this height, we need to do additional work to overcome the gravitational potential energy and give it the necessary kinetic energy to maintain circular orbit. The extra work done is given by the formula;

W = (1/2)mv² - GMm/r

where W is work done, m is mass of the object, v is velocity of the object in circular orbit, G is gravitational constant, M is the mass of the Earth, and r is the distance between the object and the center of the Earth.

We can find the velocity of the object using the formula:

v = √(GM/r)

where √ is the square root symbol. Substituting the given values, we have;

v = √[(6.67 × 10⁻¹¹ N·m²/kg²)(5.97 × 10²⁴ kg)/(6,371 km + 992 km)] = 7,657 m/s

Substituting the values into the formula for work, we have;

W = (1/2)(101 kg)(7,657 m/s)² - (6.67 × 10⁻¹¹ N·m²/kg²)(5.97 × 10²⁴ kg)(101 kg)/(6,371 km + 992 km)

W = 4.58 × 10¹¹ J

Converting J to the required units, we get;

W = 458 MJ

Therefore, the extra work needed to launch the object into circular orbit at a height of 992 km above the surface of the Earth is 458 MJ.

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--The given question is incomplete, the complete question is

"(a) Calculate the work (in MJ) necessary to bring a 101 kg object to a height of 992 km above the surface of the Earth.__ MJ (b) Calculate the extra work (in MJ) needed to launch the object into circular orbit at this height of 992 km above the surface of the Earth .__MJ."--

Stock exchanges and over-the-counter (OTC) markets are two common ways investors can trade securities. Stock exchanges are centralized marketplaces where buyers and sellers come together to trade stocks, bonds, and other securities. The most well-known exchanges include the New York Stock Exchange (NYSE) and the NASDAQ.

Trading on a stock exchange is typically more formal and regulated than trading on an OTC market. OTC markets, on the other hand, are decentralized and allow for more informal trading between individuals and institutions. Examples of OTC markets include the OTC Bulletin Board (OTCBB) and the Pink Sheets. Both types of markets offer opportunities for investors to buy and sell securities, but they differ in their structure and regulation.

Your question is: "Stock exchanges and over-the-counter markets where investors can trade their securities with others are known as?"

My answer: Stock exchanges and over-the-counter (OTC) markets are known as secondary markets. In these markets, investors can trade their securities, such as stocks and bonds, with other investors. Secondary markets provide liquidity, price discovery, and risk management opportunities for investors. The trading process typically involves a buyer and a seller, with the assistance of brokers and market makers. Examples of stock exchanges include the New York Stock Exchange (NYSE) and the London Stock Exchange (LSE), while OTC markets include the OTC Bulletin Board (OTCBB) and the Pink Sheets.

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Converting to Cartesian coordinates is one way to find alternate descriptions for (r,0) (-1,π) in polar coordinates.

When looking for alternate descriptions for the polar coordinates (r,0) (-1,π), converting them to Cartesian coordinates is one way to do it.

However, a better method is to remember the steps to graph a point in polar coordinates.

If r is greater than zero, start along the positive z-axis, and if r is less than zero, start along the negative z-axis.

Then, rotate counterclockwise if θ is greater than zero, and rotate clockwise if θ is less than zero.

By following these steps, alternate descriptions for (r,0) (-1,π) in polar coordinates can be determined without having to convert them to Cartesian coordinates.

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To do this, let's recall the rules for graphing polar coordinates:

1. If r > 0, start along the positive z-axis.
2. If r < 0, start along the negative z-axis.
3. If θ > 0, rotate counterclockwise.
4. If θ < 0, rotate clockwise.

Now, let's examine the given points:

(r, θ) = (-1, π): The starting point is (-1, π), which has a negative r-value and θ equal to π.

(r, θ) = (1, 2π): Since the r-value is positive and θ = 2π, the point would start on the positive z-axis and make a full rotation. This results in the same position as (-1, π).

(r, θ) = (-1, 2π): This point has a negative r-value and θ = 2π. Since a full rotation is made, this point ends up in the same position as (-1, π).

Thus, the alternate descriptions for the polar coordinates (-1, π) are:

1. (r, θ) = (1, 2π)
2. (r, θ) = (-1, 2π)

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The approximate measurement for the angle of the 14th minimum in this diffraction pattern is 58.6 degrees.

We can use the single-slit diffraction formula to find the angle of the 14th minimum in this diffraction pattern. The formula is:

sin θ = mλ / b

where θ is the angle of the minimum, m is the order of the minimum (m = 1 for the first minimum, m = 2 for the second minimum, and so on), λ is the wavelength of the light, and b is the width of the slit.

Given:

m = 14 (order of the minimum)

λ = (unknown)

b = (unknown)

mλ for the 4th minimum = 5.9

We can find the wavelength of the light by using the known value of mλ for the fourth minimum:

sin θ4 = mλ / b

sin θ4 = (4λ) / b

λ = (b sin θ4) / 4

λ = (b sin (tan[tex]^(-1)[/tex](5.9 / 4))) / 4

λ = (b * 0.988) / 4

λ = 0.247b

Now we can use the value of λ to find the angle of the 14th minimum:

sin θ14 = mλ / b

sin θ14 = (14λ) / b

sin θ14 = 3.43λ / b

sin θ14 = 3.43(0.247b) / b

sin θ14 = 0.847

θ14 = sin[tex]^(-1)[/tex](0.847)

θ14 ≈ 58.6 degrees

Therefore, the angle of the 14th minimum in this diffraction pattern is approximately 58.6 degrees.

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Increasing the displacement of a vibrating particle in a mechanical wave from the equilibrium position will increase amplitude. The correct option is C.

The amplitude of a mechanical wave increases with the movement of a vibrating particle from its equilibrium point.

The largest distance a particle can travel from its rest position is known as amplitude, which reveals the wave's energy and intensity.

The wave's wavelength, frequency, or phase velocity are unaffected by this amplitude shift.

The wave's strength and total magnitude are therefore improved by raising the particle's displacement without changing the wave's fundamental properties, such as frequency or speed.

Thus, the correct option is C.

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Your question seems incomplete, the probable complete question is:

Increasing the displacement of a vibrating particle in a mechanical wave from the equilibrium position will increase:

A) Wavelength

B) Frequency

C) Amplitude

D) Phase velocity

Paper must be heated to a specific temperature (234°C) to begin reacting with oxygen because it needs enough energy to break down its complex structure and start the chemical reaction of combustion. Heating the paper over a flame provides the necessary energy to initiate this process.

Once the paper reaches its ignition temperature, the heat from the combustion reaction will continue to sustain the fire. Additionally, the heat causes the cellulose fibers in the paper to release volatile gases, which then ignite and contribute to the flame. Without sufficient heat, the paper would not reach its ignition temperature and would not begin to burn.

The paper must be heated to 234°C to start burning because that is its ignition temperature. At this temperature, the paper begins to react with oxygen, leading to combustion. Heating the paper to this point provides the necessary energy for the chemical reaction between the paper's molecules and the oxygen in the air. The flame acts as a heat source to raise the paper's temperature to its ignition point, allowing the burning process to commence.

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a) Eo = 1.46 x 10^-34 J

b) TE = 0.94 K, Eo >> TE

c) N0 = 68, chemical potential is close to Eo, N1 = 12

d) TE = 2.97 x 10^-8 K, Eo > TE, N0 >> N1

Explanation to the above short answers are written below,

a) The energy of the ground state Eo can be calculated using the formula:
Eo = (h^2 / 8πmV)^(1/3),
where h is the Planck's constant,
m is the mass of a Rb 87 atom, and
V is the volume of the box.

b) The Einstein temperature TE can be calculated using the formula:
TE = (h^2 / 2πmkB)^(1/2),
where kB is the Boltzmann constant.
Eo is much greater than TE, indicating that Bose-Einstein condensation is not likely to occur.

c) At T = 0.9TE, the number of atoms in the ground state N0 can be calculated using the formula:
N0 = [1 - (T / TE)^(3/2)]N,
where N is the total number of atoms.

The chemical potential μ is close to Eo, and the number of atoms in each of the first excited states (threefold-degenerate) can be calculated using the formula:
N1 = [g1exp(-(E1 - μ) / kBT)] / [1 + g1exp(-(E1 - μ) / kBT)],
where E1 is the energy of the first excited state, and
g1 is the degeneracy factor of the first excited state.

d) For 106 atoms in the same volume, TE is smaller than Eo, indicating that Bose-Einstein condensation is more likely to occur.

At T = 0.9TE, the number of atoms in the ground state N0 is much greater than the number of atoms in the first excited states N1, due to the larger number of atoms in the sample.

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