The unit that should be used to measure energy when calculating specific heat capacity is Energy is in Joules ( J ).
The specific heat capacity should be determined in joules per kilogram degree-celsius ( J k g − 1 ∘ C − 1 ).
It is to be supplied for the substance with respect to mass and it increased the temperature.
Hence, The unit that should be used to measure energy when calculating specific heat capacity is Energy is in Joules ( J ).
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The unit used to measure energy when calculating specificheat capacity is the joule (J).
The joule (J), a unit used to quantify energy, is used to calculate specific heat capacity. In the International System of Units (SI), the joule serves as the default unit of energy.
It is described as the quantity of energy that is delivered when one newton of force is exerted across a one-meter distance.
Thus, the quantity of heat energy needed to increase the temperature of a particular substance by a specific amount is measured as specificheat capacity. J/kg°C, or joules per kilogramme per degree Celsius, is the unit of measurement.
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The theories change over time because new information and technology may be developed that influence the theory. Therefore, option B is correct.
As new information and perspectives become available, established theories may be changed or refuted. If a new or modified theory explains all the old theory did and then some, scientists are likely to accept it.
When fresh data emerges that refutes an existing theory, scientific theories can be revised or replaced. All scientific theories are founded on observable, testable data, and they can be changed when new information is found that contradicts the present idea.
When certain features of a hypothesis are refuted by fresh experimental data, a theory might be altered in science.
Thus, option B is correct.
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Theories change over time due to new information, technology, and the perspectives of new generations of scientists.
Theories change over time for several reasons. First, new information and technology may be developed that influence the theory. For example, advancements in experimental methods can provide new information and lead to the refinement or modification of theories. Additionally, theories may change with each new generation of scientists as they bring new perspectives and ideas. It is important to note that theories may or may not be supported by new information, and scientists do not change the definition of theory to have their ideas accepted.
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Answer:
it A
Explanation:
Its a negative ion that hss one less valence electron than a netural bromine atom
Answer:
44,640 ft
Explanation:
assuming the rocket started from rest, then v₀ = 0
2 min = 120 s
Δx = v₀t + 1/2at²
Δx = 0 + 1/2(6.2 ft/s²)(120 s)² = 44,640 ft ≈ 8.45 mi
Answer:
Halogen
0.85294
Explanation:
c = Speed of light =
b = Wien's displacement constant =
T = Temperature
From Wien's law we have
Frequency is given by
For Halogen
Frequency is given by
The maximum frequency is produced by Halogen bulbs which is closest to the value of
Ratio
The ratio of Incandescent to halogen peak frequency is 0.85294
Answer:
80×5×10=4000J
so therefore, work done on the body is 4000J
Answer:
Billow clouds provide a visible signal to aviation interests of potentially dangerous turbulent sky since they indicate instability in air currents.
Explanation:
Billow clouds are created in regions that are not stable in a meteorological sense. They are frequently present in places with air flows, and have marked vertical shear and weak thermal separation and inversion (colder air stays on top of warmer air). Billow clouds are formed when two air currents of varying speeds meet in the atmosphere. They create a stunning sight that looks like rolling ocean waves. Billow clouds have a very short life span of minutes but they provide a visible signal to aviation interests of potentially dangerous turbulent sky since they indicate instability in air currents, which although may not affect us on the ground but is a concern to aircraft pilots. The turbulence due to the Billow wave is the only logical explanation for the loss of 500 m in altitude of the plane.