What You Need and
“Things To Be Aware Of”
You will need: a thermometer, set of scales, calculator (all
as accurate as possible!), a pot, cardboard and a sample of
basalt gravel that you will obtain from GZ. This is more technical
than the average earthcache but if you follow the instructions
closely you will get it right!
General Map of GZ Area: Thanks Google
Earth!
Background
Basalt is an extrusive igneous rock. This means that it has
formed from molten rock erupting out of a volcano rather than
cooling slowly underground. As a result of this relatively rapid
cooling in air it usually has only very small crystals of minerals
(try looking for these with a hand lens at GZ). The Blackhead
quarry area was a peripheral vent of the Dunedin Volcanic Group
which was active 10-13 million years ago.
Basalt - The line is 1cm long: Thanks
University of Otago!
Basalt is the earth's most common igneous rock. Its uses include
construction (basalt building blocks, pavers, bench tops) highways
(as aggregate in asphalt, and volcanic chip highways), statues,
hangi stones and when heated and extruded it can be turned into
stone wool which is a useful insulator.
Stone Wool: Thanks www.woltz.de!
Basalt's use as hangi stones or building blocks stems from its
relatively high specific heat capacity. Materials with a high
specific heat capacity take a long time to heat up - thus a house
made of basalt stays cool well into the summer. They also store a
lot of heat energy (useful in hangis) and take a long time to
release the heat - thus your basalt house releases its heat gained
during the summer well into autumn keeping the house warm.
Your task is to carry out an experiment to calculate the
specific heat capacity of a sample of basalt that you will obtain
from at or near the quarry. It is best to grab a handful of basalt
chips rather than sand or cobbles.
Basalt Gravel
The specific heat capacity of a substance is defined as the
amount of heat required to raise the temperature of 1g of a
substance by 1oC. You can find this out for basalt if
you can put a known amount of heat into a known mass of basalt and
can measure the temperature change.
The formula for heat capacity (C) is:
C = Q / T x m
Where:
C = specific heat capacity. Unit: "joules per gram degree
Celsius" or J/goC
Q = change in amount of heat energy. Unit: joules or J
m = mass. Unit: grams or g
T = change in temperature. Unit: oC
Difficulties arise in putting a measured amount of heat into the
rock and sticking a thermometer onto the side of some basalt gravel
won't exactly give you an accurate reading.
Here is what you will do to overcome that: We know C for water,
can measure its T with a thermometer and find its mass, m easily
with scales. We can rearrange the above formula to make Q the
subject.
Q = m x C x T
So, that is enough to find the amount of heat energy, Q put into
some water.
So, weigh some water (mwater), chuck it a cup. Leave
it for twenty minutes. Take it's temperature
(Twaterstart). Take your stones, weigh them
(mstones), chuck them in a pot of water, let them boil
for ten minutes, no lid. As water boils at 100oC
(Twaterend) then the temperature of the stones
(Tstonestart) is also 100. Say something while you wait
like "bubble, bubble boil and trouble, fire burn and cauldron
bubble" - hey, doesn't that feature in another Dunedin cache? Chuck
the stones in the cup. Put a cardboard lid on (Why? You want the
heat to go into the water not the air). Push the thermometer
through it and watch the thermometer closely. Record the maximum
temperature the water gets to (Twaterend) this is also
the end temperature of the stones (Tstoneend). The
specific heat capacity for water is 4.18 J/goC
(Cwater).
Plug your measured numbers into the following formula to find
out how much heat went into the water and therefore was in the
stones. Becareful of your mathematical order of operations!!
Q = mwater x Cwater x
(Twaterend - Twaterstart)
= ________ x 4.18 x _________
= ________J
Take the calculated heat energy and plug that into the equation
below along with your other measured numbers to find the specific
heat capacity of the basalt.
Cbasalt = Q / ((Tstonestart -
Tstoneend) x mstones) !!do the bits in the
brackets first!!
= _________ J/goC.
Whew! Well done!
I followed this method to get a result within 0.06
J/goC of the assumed specific heat capacity.
Logging
Requirements
GZ is roughly at the highest point of the largest exposed dune
(though this point changes over time) where you will need to go to
complete the tasks below.
0. Preface any email with GC28QY0 Basalt: A Hot Rock! in the
subject line and title and clearly note the question number and
answer. You don't need to wait for a confirmation email to log but
you might be asked for more info if your answers are slim.
1. Email me your calculated Q and Cbasalt.
2. Upload a photo of either the rock sample being taken or the
tests being done.
2010 Stegan’s
EarthCache Masters Programme
Since it is not very feasible for many NZers to easily get more
than two states for the earthcache.org masters programme and
therefore not get past Bronze I’m running my own one on a
number of Earthcaches that I plan to release this year (all things
being equal) with the following points system:
5 points: First to find
3 points: 2nd to find
1 point: Logging a find
1-5 points: Special bonus questions.
Shared points for joint finds.
At the end of 2010, I’ll issue certificates for 1st, 2nd
and 3rd and the first place getter will be awarded a geocoin. If I
feel richer and/or it looks like this is popular I’ll upgrade
the prizes.
Updated information and Leaderboard at: Stegan’s
Earthcache Programme