Question: I need help with writing a code to solve these using python. Thank you. Data is given below. Here are the data for co2Cp.csv that

I need help with writing a code to solve these using python. Thank you. Data is given below.

I need help with writing a code to solve these using python.Thank you. Data is given below. Here are the data for "co2Cp.csv"

Here are the data for "co2Cp.csv" that you can paste in excel. Thanks.

T (Kelvin) Cp (J/mol K)
298.15 37.129
300 37.221
400 41.325
500 44.627
600 47.321
700 49.564
800 51.434
900 52.999
1000 54.308
1100 55.409
1200 56.342
1300 57.137
1400 57.802
1500 58.379
1600 58.886
1700 59.317
1800 59.701
1900 60.049
2000 60.35
2100 60.622
2200 60.865
2300 61.086
2400 61.287
2500 61.471
2600 61.647
2700 61.802
2800 61.952
2900 62.095
3000 62.229
3100 62.347
3200 62.462
3300 62.573
3400 62.681
3500 62.785
3600 62.884
3700 62.98
3800 63.074
3900 63.166
4000 63.254
4100 63.341
4200 63.426
4300 63.509
4400 63.588
4500 63.667
4600 63.745
4700 63.823
4800 63.893
4900 63.968
5000 64.046
5100 64.128
5200 64.22
5300 64.312
5400 64.404
5500 64.496
5600 64.588
5700 64.68
5800 64.772
5900 64.865
6000 64.957

Heat capacity (C) is a property of a substance defined as: dQ C= d where Q is heat per unit mole, and T is absolute temperature. For substances with small heat capacities (like metals), small flows of heat result in large temperature changes. Large heat flows result in relatively small temperature changes for substances with large heat capacity (like liquid water, for example). The constant pressure heat capacity (Cp) is defined as: Q Cp = OT P Cp is a useful thermodynamic property that has been carefully measured for numerous gases and liquids. The temperature dependence of Cp is typically modeled with a Shomate Equation, a polynomial of the form: Cp = A + BT + CT2 + DT3 + ET-2 R where R is the ideal gas constant and T is absolute temperature. A, B, C, D and E are adjustable parameters found through least squares fitting to experimental data. Notice that the dimensions of R (energy/mole/degree) are the same as that for Cp, so the ratio Cp/R provides a dimensionless Shomate equation. Problem 4 The data file "co2Cp.csv" contains values for Cp of carbon dioxide measured at various temperatures at a fixed pressure of 1 bar. The first column is the measured heat capacity in units of Joules/mole/Kelvin. The second column is the absolute temperature in Kelvin. The Shomate equation does not fit carbon dioxide over the entire temperature range as it did for methane in the previous problem. The proposed solution is to divide the data into two temperature ranges: (1) T1200 K, then fit the Shomate equation to each of the two temperature ranges. Calculate the root mean square percent error in predicting Cp/R when using a single Shomate equation fit over the entire temperature range compared to that obtained by splitting into two temperature ranges and fitting each range separately. The root mean square percent error is defined as: 1/2 error i=1 RMSE = 11 where n is the number of data points over the entire temperature range. The perecent error (called "error" here) is defined for each data point as described above In [ ]: N Problem 5 Using data from the previous problem, plot the percent error in predicted Cp/R values obtained by fitting a single equation over the entire temperature range compared to that obtained by splitting the data into two ranges for fitting. In [ ]: Heat capacity (C) is a property of a substance defined as: dQ C= d where Q is heat per unit mole, and T is absolute temperature. For substances with small heat capacities (like metals), small flows of heat result in large temperature changes. Large heat flows result in relatively small temperature changes for substances with large heat capacity (like liquid water, for example). The constant pressure heat capacity (Cp) is defined as: Q Cp = OT P Cp is a useful thermodynamic property that has been carefully measured for numerous gases and liquids. The temperature dependence of Cp is typically modeled with a Shomate Equation, a polynomial of the form: Cp = A + BT + CT2 + DT3 + ET-2 R where R is the ideal gas constant and T is absolute temperature. A, B, C, D and E are adjustable parameters found through least squares fitting to experimental data. Notice that the dimensions of R (energy/mole/degree) are the same as that for Cp, so the ratio Cp/R provides a dimensionless Shomate equation. Problem 4 The data file "co2Cp.csv" contains values for Cp of carbon dioxide measured at various temperatures at a fixed pressure of 1 bar. The first column is the measured heat capacity in units of Joules/mole/Kelvin. The second column is the absolute temperature in Kelvin. The Shomate equation does not fit carbon dioxide over the entire temperature range as it did for methane in the previous problem. The proposed solution is to divide the data into two temperature ranges: (1) T1200 K, then fit the Shomate equation to each of the two temperature ranges. Calculate the root mean square percent error in predicting Cp/R when using a single Shomate equation fit over the entire temperature range compared to that obtained by splitting into two temperature ranges and fitting each range separately. The root mean square percent error is defined as: 1/2 error i=1 RMSE = 11 where n is the number of data points over the entire temperature range. The perecent error (called "error" here) is defined for each data point as described above In [ ]: N Problem 5 Using data from the previous problem, plot the percent error in predicted Cp/R values obtained by fitting a single equation over the entire temperature range compared to that obtained by splitting the data into two ranges for fitting. In [ ]

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