Wednesday, March 18, 2020

Measuring the specific heat capacity of water Essays

Measuring the specific heat capacity of water Essays Measuring the specific heat capacity of water Paper Measuring the specific heat capacity of water Paper Introduction The Specific Heat Capacity of any substance can be defined as the amount of energy needed to raise 1kg of the substance by 1i c. Its found by using the following formula: C = Q / (M x ? ?) Where (C) represents the SPHC; (Q) the energy needed or given out in joules; (M) is the mass of the substance calculated in kilograms and ? ? represents the change in temperature in either i C or Kelvin. Aim The aim of the experiment is to determine the Specific Heat Capacity of any liquid, but in our case Water. Hypothesis I think that we will obtain a close number to the exact Specific Heat Capacity known as 4200 J/Kgi C. , though it will not be 100 accurate because some heat will be lost, leading to possible errors in data. I dont think we can insulate 100% with the following calorimeter at school, thus it might gain or release energy causing in-accuracy. Additionally I think that the change of temperature will be constant throughout the experiment, because the amount of energy given will always stay the same. I also believe the temperature will rise proportional to time, this is because as more time is expanded, the molecules receive more heat, according to the Kinetic Theory, the molecules become more active, and start to move rapidly increasing collision rate. Thus more the time, the higher the temperature will be until a certain point. This is the boiling point, and this is when the molecules have reached the maximum point, and are on the point of transforming into another state of form gaseous. Apparatus A Calorimeter A Thermometer A Electric Weighing Scale. A Power Pack d 1. An empty calorimeter is weighed. The liquid under test is then poured in the calorimeter and reweighed. The Mass m of the liquid is found. 2. An immersion heater and a thermometer are placed in the calorimeter 3. The initial temperature ? ? 1 of the liquid is recorded. 4. The liquid is heated for a time t seconds. The stirrer is used to maintain a uniform temperature throughout the liquid. The lid minimizes heat losses by convection. 5. Record the temperature after every two minutes and plot it in the table below. 6. The final temperature ? ? 2 is noted and the changed in temperature ? ? after time t is found7. Record the results in the table below Precautions 1. To properly place the lid, otherwise heat lose might increase, to minimize heat loss as much possible using insulation. 2. To maintain uniform temperature make sure to keep stirring the calorimeter. 3. Make sure to keep constant energy supply by heater 12V. Variables Independent Is the power heating the up the water. This is because if you change the power, then the change in temperature will also change proportionally. So you have to keep it constant throughout, otherwise this might lead to un-reliable data. To manipulate you could change the power, by increasing the current or the volts. So you could change the current from 12V, to 16V, which would change the power. But this has to be done at the start of the experiment, and then kept constant throughout. Dependent This is the change in temperature, as this is dependent on the power supplied to the heater, if changed then the change in temperature will also change. To manipulate, you will have to change the Independent variable. Controlled This is the mass of the water, the time intervals and the power. These have to be kept constant, or otherwise it wont be a fair test. The mass of the water is kept at 0. 425 kg, 120 second time intervals and 12W power supply. To manipulate you could increase the mass by 0. 010 kg, or increase the power supply to 16W, or even increase or decrease the time intervals to either 300 second or 30 seconds. But the changes have to be kept constant otherwise. Results Time / Seconds Temperature / (? ) Change in temperature. E = the power in watts Q = the energy in joules T = time in seconds 12 x 0. joules Now to find the Specific Heat capacity we have to go back to the original formula, and deduce these finding into it. Re-arrange the formula C Conclusion From my calculation and results I have obtained the Specific Heat Capacity of water to be 4320 j/kgi C for this practical. Now I can argue that this is not a 100% accurate experiment as the scientifically defined Specific Heat Capacity of water is found to be 4200 j/kgi C. There is a difference of 1320 j/kgi C, from my results and the initial value; but I used two different ways to calculate the answer. I used the formula, which gives 4320 j/kgi C, but then I also used the gradient which in result gave me a more accurate answer of 4235 j/kgi C. As you can see the gradient gives a much more accurate answer, this is because when you use the method of calculating the sphc, by subtracting the final temperature by the initial temperature, you only base your calculation of two sets of data. This is unreliable, because if one of them proves to be inaccurate, then this impacts the answer proportionally. The gradient method is more accurate, because you are taking the data from the line of best fit, which allows you to predict the value of one variable based on a value of the other; avoiding erroneous sets of data. Using the gradient method I got an answer of 4235j/kgi C, which is very close to the initial value of Specific Heat Capacity of Water. There is a difference of only 35j/kgi C, and a difference of 85j/kgi C from the calculations using the other method. So why isnt my answer identical to the genuine calculation? Well this can be caused by many reasons, one is that the calorimeter partially absorbed some of the heat which in turn meant, that it needed more energy to raise the temperature of the water, as the particles had less energy due to heat loss. Another reason could be because it was insulated 100%, which meant that it lost some heat to the air, which again meant that the particles didnt have as much energy so it needed more. Though this reasons will only slightly affect the answer, as we didnt not perform the experiment at a very high temperature. In my hypothesis I stated that my answer for the specific heat capacity will differ slightly from the original, and I was right, but I also stated that the change in temperature will be constant, and that the temperature will rise uniformly. Theoretically I should be right, but from my results you can see that the change in temperature wasnt constant. This is because I didnt stir, the calorimeter enough and persistently. This would have made the particles in the water move more so the temperature would have then increased. The more stirring that was done could have allowed the temperature to increase at a fully uniform level. And I think that the main reason why my results of the specific heat capacity doesnt exactly equal 4200 j/kgi C. Evaluation I think that I was very close to the precise specific heat capacity of water. With a difference of only 35j/kgi C I think that there are variables, which cannot be controlled 100%. But I think I could have improved this experiment. I think next time I could take a wider range of data, for the temperatures. This means to repeat the experiment numerous times. This will allow me to have more accurate data. Also I think I should keep the stirring of the water more persistent next time. I could either, have a plan of something like, stirring for 2 minutes, and then stopping for an minute etc. Or I could persistently keep on stirring through the whole experiment; this will allow the particles to move around the beaker more, making it a fairer test. Also I could increase the power supplied to the calorimeter, which would allow me to analyze the relationship at higher temperatures, and also more modern equipment. All these factors could be improved next time, hopefully giving me even accurate results. 1 Appendix 1 2 See Graph Show preview only The above preview is unformatted text This student written piece of work is one of many that can be found in our GCSE Electricity and Magnetism section.

Sunday, March 1, 2020

Definition and Examples of Language Change

Definition and Examples of Language Change Language change is the phenomenon by which permanent alterations are made in the features and the use of a language over time. All natural languages change, and language change affects all areas of language use. Types of language change include sound changes, lexical changes, semantic changes, and syntactic changes. The branch of linguistics that is expressly concerned with changes in a language (or in languages) over time is historical linguistics (also known as diachronic linguistics). Examples and Observations For centuries people have speculated about the causes of language change. The problem is not one of thinking up possible causes, but of deciding which to take seriously...Even when we have eliminated the lunatic fringe theories, we are left with an enormous number of possible causes to take into consideration. Part of the problem is that there are several different causative factors at work, not only in language as a whole but also in any one change...We can begin by dividing proposed causes of change into two broad categories. On the one hand, there are external sociolinguistic factors - that is, social factors outside the language system. On the other hand, there are internal psycholinguistic ones - that is, linguistic and psychological factors which reside in the structure of the language and the minds of the speakers.(Jean Aitchison, Language Change: Progress or Decay? 3rd ed. Cambridge University Press, 2001)Words on the Way OutAmidst and amongst are all rather formal, almost affected, now, and are more usually encountered in high-brow writing, less usually in speech. This suggests that these forms are on the way out. They will probably bite the dust, just as betwixt and erst have done...(Kate Burridge, Gift of the Gob: Morsels of English Language History. HarperCollins Australia, 2011) Anthropological Perspective on Language ChangeThere are many factors influencing the rate at which language changes, including the attitudes of the speakers toward borrowing and change. When most members of a speech community value novelty, for example, their language will change more quickly. When most members of a speech community value stability, then their language will change more slowly. When a particular pronunciation or word or grammatical form or turn of phrase is regarded as more desirable, or marks its users as more important or powerful, then it will be adopted and imitated more rapidly than otherwise...The important thing to remember about change is that, as long as people are using a language, that language will undergo some change.(Harriet Joseph Ottenheimer, The Anthropology of Language: An Introduction to Linguistic Anthropology, 2nd ed. Wadsworth, 2009)AÂ  Prescriptivist Perspective on Language ChangeI see no absolute Necessity why any Language would be perpetually changing.(Jonathan Swift, Proposal for Correcting, Improving, and Ascertaining the English Tongue, 1712) Sporadic and Systematic Changes in LanguageChanges in language may be systematic or sporadic. The addition of a vocabulary item to name a new product, for example, is a sporadic change that has little impact on the rest of the lexicon. Even some phonological changes are sporadic. For instance, many speakers of English pronounce the word catch to rhyme with wretch rather than hatch...Systematic changes, as the term suggests, affect an entire system or subsystem of the language... A conditioned systematic change is brought about by context or environment, whether linguistic or extralinguistic. For many speakers of English, the short e vowel (as in bet) has, in some words, been replaced by a short i vowel (as in bit), For these speakers, pin and pen, him and hem are homophones (words pronounced the same). This change is conditioned because it occurs only in the context of a following m or n; pig and peg, hill and hell, middle and meddle are not pronounced alike for these speakers.(C.M. Millward, A Biography of the English Language, 2nd ed. Harcourt Brace, 1996) The Wave Model of Language Change[T]he distribution of regional language features may be viewed as the result of language change through geographical space over time. A change is initiated at one locale at a given point in time and spreads outward from that point in progressive stages so that earlier changes reach the outlying areas later. This model of language change is referred to as the wave model ...(Walt Wolfram and Natalie Schilling-Estes, American English: Dialects and Variation. Blackwell, 1998)Geoffrey Chaucer on Changes in the Forme of SpeecheYe knowe ek that in forme of speeche is chaungeWithinne a thousand yeer, and wordes thoThat hadden pris, now wonder nyce and straungeUs thinketh hem, and yet thei spake hem so,And spedde as wel in love as men now do;Ek for to wynnen love in sondry ages,In sondry londes, sondry ben usages.[You know also that in (the) form of speech (there) is changeWithin a thousand years, and words thenThat had value, now wonderfully curious and stran ge(To) us they seem, and yet they spoke them so,And succeeded as well in love as men now do;Also to win love in sundry ages,In sundry lands, (there) are many usages.](Geoffrey Chaucer, Troilus and Criseyde, late 14th century. Translation by Roger Lass in Phonology and Morphology. A History of the English Language, edited by Richard M. Hogg and David Denison. Cambridge University Press, 2008)