The number of neutrons differs among isotopes

In some elements, the number of neutrons in the atomic nucleus may vary. Different isotopes of the same element have the same number of protons but different numbers of neutrons, as you saw in the story opening this chapter. Many elements have several isotopes. Generally, isotopes are formed when atoms combine and/or release particles (decay). The isotopes of hydrogen shown here have special names, but for most elements their isotopes do not have special names.

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The natural isotopes of carbon, for example, are 12C (six neutrons in the nucleus), 13C (seven neutrons), and 14C (eight neutrons). Note that all three (called carbon-12, carbon-13, and carbon-14) have six protons, so they are all carbon. Most carbon atoms are 12C, about 1.1 percent are 13C, and a tiny fraction are 14C. The carbon atoms that make up complex biological molecules are mostly 12C, but some are 13C. The ratio of 13C:12C varies with location and can be used to identify biological samples whose origin is not known (Investigating Life: Determining Beef Source in Big Macs Using Isotope Analysis). All carbon isotopes have virtually the same chemical reactivity, which is an important property for their use in experimental biology and medicine.

An element’s atomic weight (or relative atomic mass) is equivalent to the average of the mass numbers of a representative sample of atoms of that element, with all the isotopes in their normally occurring proportions. More precisely, an element’s atomic weight is defined as the ratio of the average mass per atom of the element to 1/12 of the mass of an atom of 12C. Because it is a ratio, atomic weight is a dimensionless physical quantity—it is not expressed in units. The atomic weight of hydrogen, taking into account all of its isotopes and their typical abundances, is 1.00794. This number is fractional because it is the average of the contributing masses of all of the isotopes. This definition implies that in any given sample of hydrogen atoms of a particular element found on Earth, the average composition of isotopes will be constant. But as you saw in the opening to this chapter, that is not necessarily so. Some water has more of the heavy O isotopes. So chemists are now listing atomic weights as ranges, for example, H: 1.00784–1.00811.

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investigating life

Determining Beef Source in Big Macs Using Isotope Analysis

experiment

Original Paper: Martinelli, L., G. Nardoto, L. Chesson, F. Rinaldi, J. P. H.B. Ometto, T. Cerling and J. Ehleringer. 2011. Worldwide stable carbon and nitrogen isotopes of Big Mac patties: An example of a truly “glocal” food. Food Chemistry 127: 1712–1718.

The Big Mac hamburger can be purchased in 35,000 outlets in 120 countries. The recipe for the Big Mac is virtually the same everywhere; it is claimed that the burger has the same quality meat and nutritional quality everywhere it is served. To investigate this claim, Lesley Chesson and James Ehleringer at the University of Utah compared the ratio of 13C:12C in Big Mac patties around the world to determine whether the meat had a local or a common source. Beef cattle eat plant food, and carbon atoms from this food end up in meat. In some types of plants, the ratio of 13C:12C is higher than in others. Depending on which type of plants the cattle consume, the beef will also have a different 13C:12C ratio.

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work with the data

The experiment compared the meat in Big Macs served in 25 different countries by measuring the ratio of stable carbon isotopes (13C:12C) in samples of ten beef patties from each country. The hypothesis was based on claims that the beef used in Big Macs comes from a single source, and that the 13C:12C ratio in patties found everywhere should thus be the same. Table A shows the average the 13C:12C ratio for each of the 25 countries. A higher number means more of the rare, stable isotope 13C than of the much more common 12C.

Table A
Country 13C:12C ratioa Country 13C:12C ratio Country 13C:12C ratio
All 15.8 Germany 21.7 Portugal 20.7
Argentina 17.2 Hungary 22.0 Scotland 25.2
Australia 19.4 Indonesia 19.5 Slovakia 21.0
Austria 22.0 Israel 20.4 South Africa 13.0
Brazil 11.1 Japan 11.8 Spain 21.1
Canada 21.6 Malaysia 21.5 Sweden 23.2
China 13.9 Mexico 13.9 Turkey 20.5
England 25.4 Netherlands 20.7 USA 14.5
France 21.8 Paraguay 12.1 Uruguay 16.7

aMeasured in parts per million atoms (× 100).

QUESTIONS

Question 1

Do the average local ratios differ from the 25-country average ratio? What statistical test would you perform to show that the differences between the individual country averages and the all-countries average are significant? (Refer to Appendix B.)

The average local ratios differ from the all-countries average ratio. To test the hypothesis that the ratios are significantly different, a chi-square test could be used.

Question 2

The countries from which the hamburgers were analyzed are in different locations on Earth. One way to compare locations is by geographic latitude. You may recall that in latitude, 0 degrees defines the equator and 90 degrees defines the poles. Table B shows average 13C:12C ratios of Big Mac beef patties from different latitudes. Plot the data on a graph of ratio versus latitude. What can you conclude from these data?

Table B
Latitude 13C:12C ratioa
20°S–20°N 11.4
20°–40°b 15.3
40°–60°b 21.8

aAverage value measured in parts per million atoms (× 100).

b20°S–40°S and 20°N–40°N; 40°S–60°S and 40°N–60°N.

A graph of the data shows an increasing 13C:12C ratio as latitude away from the equator increases. This implies that different plants occur in different regions. Animal feeds used locally tend to be composed of plants grown locally.image

A work with the data exercise that accompanies this figure may be assigned in LaunchPad.

Most isotopes are stable. However, some, called radioisotopes, are unstable and spontaneously give off energy in the form of α (alpha), β (beta), or γ (gamma) radiation from the atomic nucleus. Known as radioactive decay, this release of energy transforms the original atom. The type of transformation varies depending on the radioisotope, but some transformations result in a different number of protons, so that the original atom becomes a different element.

Scientists can detect released radiation from *radioisotopes. For instance, if you feed an earthworm food containing a radioisotope, you can follow the worm’s path through the soil by using a detector called a Geiger counter. Most atoms in living organisms are organized into stable associations called molecules. If a radioisotope is incorporated into a molecule, it acts as a tag or label, allowing a researcher or physician to track the molecule in an experiment or in the body (Figure 2.3).

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Figure 2.3 Tagging the Brain In these images from live persons, a radioactively labeled sugar is used to detect differences between the brain activity of a depressed person (A) and that of a person who is not depressed (B). The more active a brain region is, the more sugar it takes up (shown as orange areas). The brain of the depressed person (left) shows less activity than the brain of the person who is not depressed.

Question

Q: How could this technique be used in the clinic?

The technique could be used to monitor therapy. As therapy progresses and the patient improves, one would expect that the brain region involved would show more activity.

*connect the concepts Radioisotopes are also used to analyze biochemical pathways (see Key Concept 10.3) and to date fossils (see Key Concept 24.1).

Although radioisotopes are useful in research and in medicine, even a low dose of the radiation they emit has the potential to damage molecules and cells. However, these damaging effects are sometimes used to our advantage; for example, the radiation from 60Co (cobalt-60) is used in medicine to kill cancer cells.

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