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A laboratory experiment where students measure the volume and mass of mineral samples using graduated cylinders and a triple beam balance. The data collected is used to determine the density of the minerals by plotting mass and volume on a graph and finding the slope of the best-fit line.
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In this laboratory you will have the opportunity to apply your measuring skills in gathering data, processing it, and interpreting the results. For this experiment you will: 1) measure the volume and mass of samples of minerals, 2) plot the data on a graph, and 3) determine the slope of the line that represents the density of the minerals.
On each of the 100mL and 250 mL graduated cylinders there are markings (graduations) that indicate the volumes along the length of the cylinder. Notice there are two sets of graduations on each cylinder, a graduation for larger volumes and smaller volumes.
are in increments of 1 mL and the larger graduations are in increments of 10 mL.
are in increments of 2 mL and the larger graduations are in increments of 20 mL.
Numbers that express measurements always contain one or more digits we are certain of, plus one that is estimated. All of these digits, the certain ones and the estimated one, are considered to be reasonably reliable, and are called significant figures. For example, the readings of 36.0 mL for both graduated cylinders above each contain three significant figures, the first two of which are certain, and the last of which is estimated.
When the meniscus of the liquid lies somewhere in between graduations, the volume of liquid must be estimated. As a rule, the volumes between the smallest graduations can be further graduated into 10 parts so that the accuracy of the 100 mL graduated cylinder can be estimated to the nearest 0.1 mL and the 250 mL cylinder can be estimated to the nearest 0.2 mL.
Therefore the liquid in the 100 mL graduated cylinder could be recorded as 43.4 or 43.5 or 43.6 mL and the liquid in the 250 mL graduated cylinder could be recorded as 92.8 or 93.0 or 93.2 mL.
Partially fill each of the two graduated cylinders with water and determine the volumes. To do this, place the cylinder on the table and stoop down so your eye is level with the water level. You will notice that the water looks curved in the cylinder. To get an accurate reading, read the bottom of the curve ( meniscus ). Record the volumes of the water below and let your instructor check your results.
Volume of water in 100 mL cylinder __________ mL __________ L
Volume of water in 250 mL cylinder __________ mL __________ L
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Mass is a measure of the quantity of material the object contains. Measuring mass is done by comparing the mass of an unknown object to the mass of a known object. A beam balance has known masses (riders) which can be moved along the beams to determine the mass of an unknown object on the pan. Each of the beams has its own graduations. The mass of the unknown object is simply the sum of the readings on all three beams.
To start, move all of the riders to zero (far left.) Notice that the riders for the 100 g and 10 g beams must fit into notches, while the 1 g rider slides between graduations. On the far right of the balance is a zero-scale which indicates when the known masses are equal to the unknown mass. When all of the riders are on zero, the balance arm should be even with the zero-scale indicator. Notice that the 1 g beam is graduated into 0.1 g graduations.
Similar to the graduated cylinder, the masses of objects must be estimated to one more decimal place than the smallest graduation, or 0.01 grams. This is done by making 10 imaginary graduations between these graduations and estimating to the nearest 0.01 g.
Determine the mass of your pencil using the triple-beam balance and record your results below. Have your instructor check your results. Your answer should be recorded to the nearest 0.01 g (13.56 g, for example.)
Mass of pencil = ___________ grams _______________ kilograms
Minerals are solids that form naturally within the earth through the process of crystallization. Minerals differ from one another in a variety of ways, but because minerals have specific chemical and physical compositions, they have uniform consistency and a specific density. This physical property allows us to identify minerals by determing their mass/volume ratios and comparing the results with known values. In this portion of the laboratory the density of two common minerals will be determined from plotting mass and volume data. The identity of the minerals will be determined by comparing the experimental results with a table of known values.
100 mL graduated cylinder. Record this volume in the data table.
second piece to the mass of your first sample of mineral.
mineral into the graduated cylinder. Record the total volume of the first and second sample.
Since the slope of a line is a mathematical relationship, it is not satisfactory to say one line is "quite steep” or "not so steep". It is necessary to know as accurately as possible how much the line is slanted from the horizontal. In order to do this the amount of vertical "Rise" for a given amount of horizontal "Run" of the line must be determined. The slope, therefore, is obtained by constructing a right triangle at any segment of the line, determining the Rise and Run on the vertical and horizontal axes, and then finding the ratio of the Rise to the Run for that segment of the line. If, for example, we find that for any given segment of the line there is a rise of 3 units for every 2 units of horizontal distance, then the slope of the line is 1.5.
The graph below is a best-fit plot of mass and volume data of four samples of a mineral. The slope of the line is determined using two points located on the best-fit line, not data points. The slope of the line (density of the mineral) is the ratio of the mass and volume (M / V).
Volume (mL)
Mass (g) 1 5.8 48. 32.0 105. 50.0 149. ( 65 , 200) 66.4 190.
Change in mass (Y) = 200.00 g – 140 .00 g = 60.00 g
Change in volume (X) = 6 5 .0 mL – 46 .0 mL = 19.0 mL
Slope (Y / X) = 60.00 g / 19.0 mL = 3.16 g / mL
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To determine the volume for 100.00g of the mineral, a set of perpendicular lines that intersect at the best- fit line are drawn. For this mineral, the sample would occupy a volume of 3 2 .0 mL.
Volume (mL)
Mass (g)
Density (g/mL)
Borax 1.7 Pyrite 5. Quartz 2.65 Hematite 5. Talc 2.8 Copper 8. Mica 3.0 Gold 19.