Monday, August 1, 2011
The Phenomenon (Human Reaction to choices)
pH Scale (Real-life Application) -- Continued
Real-Life Application of pH Scale
Thus
pH = -log(3.2 x 10-3)
pH = 2.494
Round up to 2.49
Therefore the pH level of the Lemon Juice is 2.49. We cross-referenced it to several websites and confirmed that the acidity of Lemon juice is 2.49.
http://www.indiacurry.com/chutney/foodphlevel.htm
http://www.everydiet.org/diet/acid-alkaline-diets
http://answers.ask.com/Science/Chemistry/what_is_the_ph_level_of_lemon_juice
Friday, July 29, 2011
Hick's Law
The Weber-Fechner Law
Thursday, July 28, 2011
Logarithms in Psychology (Fitt's Law)
The pH Scale
[H3O+] | pH | [OH-] | Example |
1 X 100 | 0 | 1 X 10-14 | HCl (4%) |
1 X 10-1 | 1 | 1 X 10-13 | Stomach acid |
1 X 10-2 | 2 | 1 X 10-12 | Lemon juice |
1 X 10-3 | 3 | 1 X 10-11 | Vinegar |
1 X 10-4 | 4 | 1 X 10-10 | Soda |
1 X 10-5 | 5 | 1 X 10-9 | Rainwater (unpolluted) |
1 X 10-6 | 6 | 1 X 10-8 | Milk |
1 X 10-7 | 7 | 1 X 10-7 | Pure water |
1 X 10-8 | 8 | 1 X 10-6 | Egg whites |
1 X 10-9 | 9 | 1 X 10-5 | Baking Soda |
1 X 10-10 | 10 | 1 X 10-4 | Ammonia |
1 X 10-11 | 11 | 1 X 10-3 | |
1 X 10-12 | 12 | 1 X 10-2 | Drano® |
1 X 10-13 | 13 | 1 X 10-1 | NaOH (4%) |
1 X 10-14 | 14 | 1 X 100 |
Wednesday, July 27, 2011
The Magic Formulas (Richter Scale)
M = log10 (A / Azero)
A = Azero 10M
Don't understand? We will start with this formula first because it's simpler to understand and because you must be able to understand this formula before moving on to the original formula. (The original formula is derived from a few equations, including the ones we just introduced)
M = log10 (A / Azero)
Definitions:
M is the magnitude
A is the maximum excursion of the seismograph
A0 is the empirical function depending on the epicenter distance
So as the for every 1 unit the magnitude increases, the amplitude increases by a factor of 10. The same 1 unit of increase in magnitude would give you an approximate of 32 times the earthquake's energy! Scary, isn't it?
So, by inserting the variables A and A0, you will get the magnitude of the earthquake and then you can find out the energy of the earthquake.
Now you may ask, "How do we find the epicenter distance?"
During an earthquake, seismic waves are spread spherically out from the hypo-center. You can find the epicenter distance by measuring the time difference on the seismograph and the distance on a travel-time graph at which the P-wave and S-wave have the same separation.
A picture worth a thousand words. So let's let the animation tell you something about the P-wave and the S-wave.
http://upload.wikimedia.org/wikipedia/commons/6/62/Onde_compression_impulsion_1d_30_petit.gif
http://upload.wikimedia.org/wikipedia/commons/6/6d/Onde_cisaillement_impulsion_1d_30_petit.gif
Left to right: P-wave (Primary Wave), S-wave (Secondary Wave)
And you on to the magic formula!
It is the same logic as the previous formulas we have just mentioned. While M is the magnitude and A is the amplitude. There's something new -- δ.δ the epicenter distance of the station, which is where the earthquake takes place. This formula is derived from the previous formulas.
Note: Magnitude greater than 4.6 are strong enough to be recorded b a seismograph. Any figures below 4.6 are not considered strong enough to be considered an earthquake.
And TADAAAA. You have your Richter Scale!
http://en.wikipedia.org/wiki/Epicentral_distance#Epicentral_distance
http://en.wikipedia.org/wiki/P-wave
http://en.wikipedia.org/wiki/S-wave
http://www.vibrationdata.com/earthquakes/magnitude.html
The Richter Scale Chart
Magnitude | Description | Earthquake effects | Frequency of occurrence |
Less than 2.0 | Micro | Micro earthquakes, not felt.[12] | About 8,000 per day |
2.0–2.9 | Minor | Generally not felt, but recorded. | About 1,000 per day |
3.0–3.9 | Often felt, but rarely causes damage. | 49,000 per year (est.) | |
4.0–4.9 | Light | Noticeable shaking of indoor items, rattling noises. Significant damage unlikely. | 6,200 per year (est.) |
5.0–5.9 | Moderate | Can cause major damage to poorly constructed buildings over small regions. At most slight damage to well-designed buildings. | 800 per year |
6.0–6.9 | Strong | Can be destructive in areas up to about 160 kilometres (100 mi) across in populated areas. | 120 per year |
7.0–7.9 | Major | Can cause serious damage over larger areas. | 18 per year |
8.0–8.9 | Great | Can cause serious damage in areas several hundred kilometres across. | 1 per year |
9.0–9.9 | Devastating in areas several thousand kilometres across. | 1 per 20 years | |
10.0+ | Massive | Never recorded, widespread devastation across very large areas; see below for equivalent seismic energy yield. | Extremely rare (Unknown) |
(Based on U.S. Geological Survey documents
http://en.wikipedia.org/wiki/Richter_magnitude_scale
Tuesday, July 26, 2011
The Richter Scale
Magnitude | Ground amplitude (mm) at a distance of 100 km |
0 | 0.00000048 |
1 | 0.0000048 |
2 | 0.000048 |
3 | 0.00048 |
4 | 0.0048 |
5 | 0.048 |
6 | .48 |
7 | 4.8 |
8 | 48 |
9 | 480 |