AP Chemistry Review: Unit 1 (Atomic Structure and Properties)
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Summary
Professor Dave provides a detailed review of Unit 1 of the AP Chemistry curriculum, focusing on atomic structure and properties. This segment covers key concepts such as electron configurations, periodic trends, isotopes, ions, and spectroscopy. Starting from the basic structure of atoms and progressing through complex ideas like quantum numbers and periodic trends, this overview aims to simplify the understanding of chemistry's fundamental building blocks, ensuring students are well-prepared for the AP exam.
Highlights
Atomic structure is the foundation of chemistry, including moles, isotopes, and ions 🌟.
Electron configurations are determined by energy levels and filling orders 🎯.
Periodic trends like atomic radius and ionization energy are crucial for understanding chemical behavior 📊.
Spectroscopy techniques provide insights into isotopic and elemental properties 🔍.
Quantum numbers provide a detailed understanding of electron distributions within atoms ⚛️.
Key Takeaways
Understanding atomic structure and properties is crucial for AP Chemistry success 📘.
Valence electrons determine reactivity and are key to periodic table trends 🔍.
Key periodic trends include atomic radius, ionization energy, electron affinity, and electronegativity 📈.
The Aufbau principle and Hund's rule guide electron configuration filling 📜.
Mass spectroscopy helps define isotopic composition and abundance in elements 🔬.
Overview
In this comprehensive review, Professor Dave demystifies the basics of atomic structure and properties, making it user-friendly for AP Chemistry students. From the fundamental concepts like moles and molar mass to more intricate ideas like spectroscopy and periodic trends, this video serves as an ideal study companion.
As students navigate through the video, they will gain insight into how atoms form molecules, how the periodic table is structured and why it’s organized in its particular way. Essential concepts like atomic mass, electron configurations, and chemical bonds are broken down into digestible bits, which students can easily understand and recall.
The video closes with a focus on periodic trends, a crucial concept in chemistry that describes the predictable patterns in element behavior. By the end of this session, students are well-equipped with the crucial knowledge of Unit 1, ready to take on more complex chemical topics in their AP journey.
Chapters
00:00 - 00:30: Introduction: Preparing for AP Chemistry Exam The introduction sets the stage for preparing for the AP Chemistry exam, emphasizing the importance of understanding various terminologies and concepts. Dave Farina indicates the approach to cover all necessary terms and ideas in a condensed format through comprehensive videos, each focusing on one of the nine units covered in the exam. The introduction then transitions into discussing Unit 1, which deals with atomic structure and properties.
00:30 - 01:00: Topics Overview of Unit 1 The chapter covers fundamental chemistry concepts, including moles and molar mass, mass spectroscopy, pure substances and mixtures, electron configurations, photoelectron spectroscopy, periodic trends, valence electrons, and ionic compounds. The focus will be on complex topics as they arise, but reviewing the fundamentals is encouraged.
01:00 - 01:30: Basic Concepts: Atoms and Molecules This chapter introduces the basics of atoms and molecules, starting with a definition of an atom as the smallest unit of an element. The text uses copper as an example, explaining how repeatedly dividing a copper rod eventually leads to the atomic level, where the material still retains its identity as copper. The uniqueness of elements is attributed to their distinct atomic structures, particularly the number of protons present. Furthermore, it touches upon how atoms combine through chemical bonds to form molecules.
02:00 - 03:30: Pure Substances and Mixtures This chapter explains the difference between elements, compounds, and mixtures. Elements can be single atoms or molecules made of the same type of atoms, like diatomic oxygen (O2) and nitrogen (N2). Compounds are formed when atoms of different elements bond together, such as carbon dioxide (CO2) made from one carbon atom and two oxygen atoms, and water (H2O) made from one oxygen atom and two hydrogen atoms.
04:00 - 06:00: Atomic Structure The chapter titled 'Atomic Structure' discusses the concept of pure substances, which can be either elements or compounds. It explains that a pure substance is composed of only one type of particle. For instance, sodium metal is an element and thus a pure substance because it consists solely of sodium atoms. Similarly, water, despite being a compound composed of hydrogen and oxygen elements, is also a pure substance because it consists only of water molecules. The chapter underscores that although a water molecule is composed of more than one type of atom, its identity and properties as a water molecule are consistent.
11:00 - 13:00: Moles, Atomic Mass, and Molar Mass The chapter titled 'Moles, Atomic Mass, and Molar Mass' explains the concept of mixtures and compounds in chemistry. It highlights the differences between them, noting that mixtures consist of different substances with separate identities and properties, whereas compounds are composed of atoms from different elements that form a single molecule with chemical bonds. The chapter details how these compositions determine the macroscopic properties of materials, using water as an example of a compound.
14:30 - 19:00: Compounds, Percent Composition, and Formulas The chapter discusses the concepts of compounds, percent composition, and chemical formulas. It explains the differences between mixtures and compounds, with a focus on homogeneous and heterogeneous mixtures. A homogeneous mixture, such as sucrose dissolved in water, is one in which the substances involved are evenly distributed within the container. This means that any portion of the mixture would look the same if examined closely, with molecules of each substance dispersed uniformly.
19:30 - 25:30: Quantum Numbers and Atomic Orbitals The chapter 'Quantum Numbers and Atomic Orbitals' seems to be about fundamental chemistry concepts, likely elaborating on atomic structure and the distribution of electrons in atoms using quantum mechanics. The excerpt provided contrasts homogeneous and heterogeneous mixtures, using oil and water as examples of a heterogeneous mixture. It suggests that while homogeneous mixtures have a uniform composition, heterogeneous mixtures like oil and water maintain distinct layers that do not mix even at the interface.
26:00 - 28:00: Electron Configurations This chapter provides a summary of the foundational concepts in chemistry, focusing on the classification of matter. It differentiates between pure substances, which include elements and compounds, and mixtures, which can be further classified as homogeneous or heterogeneous based on their uniformity. The chapter sets the stage for discussing atomic structures, emphasizing the arrangement and roles of protons, neutrons, and electrons in forming atoms.
28:30 - 36:30: Periodic Trends This chapter explores the internal structure of an atom, focusing on the relative positions and masses of protons, neutrons, and electrons. It highlights that protons and neutrons, which are located in the nucleus, have approximately the same mass, while electrons, located far from the nucleus, have significantly less mass.
39:00 - 39:30: Conclusion and Transition to Unit 2 In this chapter, the fundamental charges of protons and electrons are discussed. Protons carry a positive charge, and electrons carry an equal but negative charge, with each unit of charge being 1.602 x 10⁻¹⁹ coulombs. Neutrons are neutral as they have no charge. The identity of an element is defined by the number of protons in its nucleus, illustrated through the example of carbon, which always has six protons. The chapter transitions towards the next unit, suggesting further exploration of atomic structure and properties.
AP Chemistry Review: Unit 1 (Atomic Structure and Properties) Transcription
00:00 - 00:30 Hey everyone, Dave Farina here. To get ready
for the AP chemistry exam, we’re going to have to understand a lot of different terminology
and concepts, and be able to answer fairly complicated questions about them. Because
there are so many terms and concepts to know, let’s go through them all together in as condensed
a format as possible, with one comprehensive video for each of the nine units the exam will cover.
Unit 1 is on atomic structure and properties, so
00:30 - 01:00 these will be all the very basics. We will discuss
moles and molar mass, mass spectroscopy, pure substances and mixtures, electron configurations,
photoelectron spectroscopy, periodic trends, valence electrons, and ionic compounds.
We will be focusing on the more complicated topics as they arise but it will be a good
idea to quickly review the fundamentals, so let’s start with an abbreviated
version of some basic concepts.
01:00 - 01:30 An atom is the smallest unit of an element, which
are these things we see on the periodic table, such as copper. If we cut a copper rod in half,
we get two smaller copper rods. We can continue doing this many times until we finally reach the
tiniest thing that could be considered copper, and that’s a copper atom. Every element is made
of a different type of atom which means it has a different number of protons inside, and
if we were to break apart this copper atom, we wouldn’t have copper anymore.
Atoms join together via chemical
01:30 - 02:00 bonds to form molecules. Sometimes molecules can
be considered elements, if they are comprised of only one type of atom, like diatomic oxygen and
nitrogen. But when atoms of more than one element come together to form a molecule, we would call
this a compound. One carbon atom and two oxygen atoms makes carbon dioxide. One oxygen atom
and two hydrogen atoms makes a water molecule.
02:00 - 02:30 A pure substance can be an element or compound.
If we have a block of sodium metal, which is an element, that’s a pure substance, because it
is made of just one thing, sodium atoms. If we have a sample of water, which is a compound,
that’s a pure substance, because it is also made of just one thing, water molecules. Each
water molecule has more than one element in it, hydrogen and oxygen, but it is still a water
molecule, and the properties of water molecules
02:30 - 03:00 are what determine the macroscopic properties
of water. When we put more than one element or compound together, we get a mixture. Notice that
we have two different substances in this mixture, with totally separate identities and properties.
So a compound is a combination of atoms of different elements to form a single molecule,
where all the atoms are chemically bound, like with water. But with a mixture, we have substances
that are totally different elements or compounds,
03:00 - 03:30 simply mixed together in the same space.
Mixtures can be either homogeneous or heterogeneous. A homogeneous mixture involves
substances that, when mixed together, are distributed evenly in the container. For example,
sucrose dissolved in water. When you put sugar in water and stir, it will disperse evenly within
the water, such that if you were to zoom in on any portion of this mixture, it would look exactly the
same, with sugar and water molecules moving around
03:30 - 04:00 one another. By contrast, a heterogeneous mixture
will not have its components spread out evenly, so every section will not look the same. An
example of this is a mixture of oil and water. We can clearly see that they will form distinct
layers, such that if we zoom in on one part, we see only oil. If we zoom in on another
part, we see only water. And if we zoom in at the interface, we see oil and water
molecules up against each other but not mixing.
04:00 - 04:30 So to summarize, we have pure substances and
mixtures. A pure substance can be either an element or a compound. A mixture is
made when more than one type of pure substance is mixed together, and this can
be either homogeneous or heterogeneous. Next we are going to want to review atomic
structure, that is the arrangement of protons, neutrons, and electrons to form atoms,
and the parameters they determine.
04:30 - 05:00 Looking inside an atom, the protons and neutrons
sit in the nucleus, with the electrons existing far away from the nucleus. The proton and neutron
have roughly the same mass, about 1.67 x 10-24 grams, which is a trillionth of a trillionth
of a gram, while the electron has nearly 2,000 times less mass than that, at around 9.1 x
10-28 grams. And in terms of electric charge,
05:00 - 05:30 the proton and electron each hold the fundamental
unit of charge, which is 1.602 x 10-19 coulombs, though for the proton that will be positive,
and for the electron it will be negative. The neutron is neutral meaning it has no charge.
Each element is defined by the number of protons in its nucleus. For example, a carbon atom has
six protons in its nucleus. Every carbon atom in the universe has six protons in its nucleus,
and every atom that does not have six protons is
05:30 - 06:00 not carbon. This is fundamentally how we define
carbon. So carbon has an atomic number of six, because the atomic number of an atom is equal
to the number of protons in its nucleus. Every element has its own unique atomic number, and
therefore characteristic number of protons. The mass number of an atom is equal to the
sum of the numbers of protons and neutrons, since each nucleon has a mass of approximately
one atomic mass unit. However, although every
06:00 - 06:30 element has a particular atomic number,
elements do not have a specific mass number, because unlike the number of protons, the number
of neutrons in the nucleus can vary for any given element. For example, carbon typically has six
neutrons, which combined with the six protons will produce a mass number of 12. But it can also
have seven neutrons, for a mass number of 13,
06:30 - 07:00 or eight neutrons, for a mass number of 14. Atoms
of a given element with different numbers of neutrons are called isotopes of a given element,
so carbon atoms will always have six protons, but different isotopes of carbon can have six,
seven, or eight neutrons, which correspond to different mass numbers. The atomic mass of an
element, which is the other number on each block of the periodic table, is the average of all the
naturally-occurring isotopes of that element with
07:00 - 07:30 respect to their relative abundance. So it’s
essentially the average mass of an atom of that element. Most carbon is carbon-12, with a little
bit of carbon-13, and trace amounts of carbon-14, therefore the average mass of all carbon
atoms will be just a tiny bit above 12, as this equation determines. We just multiply
each mass number by a fraction of one representing
07:30 - 08:00 that isotope’s relative abundance, and add them
all together. This can be done for any element. Finally, since protons are positively charged
and electrons are negatively charged, a neutral atom will have the same number of protons and
electrons. If an atom gains electrons, it will become negatively charged, because the number of
negatively charged particles will outnumber the positively charged ones. And if an atom loses
electrons, it will become positively charged,
08:00 - 08:30 because the number of positively charged
particles will outnumber the negatively charged ones. When an atom is not electrically
neutral, it is called an ion, either a cation or anion if positive or negative, respectively.
With both isotopes and ions understood, we can understand how the masses of existing isotopes
and their relative abundances can be determined for any element using a technique called mass
spectroscopy. This instrument takes a sample,
08:30 - 09:00 vaporizes it, ionizes it, and sends it through a
tube where it is subjected to an external magnetic field. The particles then have their paths
deflected by a degree that depends on their mass to charge ratio, and this information is received
when they collide with a detector. A mass spectrum displays this mass to charge ratio, which for
ions with a singular charge is essentially just atomic mass, against their relative abundance. So
with a spectrum like this we can clearly see the
09:00 - 09:30 naturally-occurring isotopes for this particular
element with their respective mass numbers on the horizontal axis, and their relative abundances on
the vertical axis. This is how this information was initially determined for every element.
To quickly summarize, the atomic number of an atom is equal to the number of protons in the nucleus.
The mass number of an atom is equal to the number
09:30 - 10:00 of protons plus the number of neutrons in the
nucleus. This means that we can calculate the number of neutrons in any atom by finding the mass
number minus the atomic number. And the electrical charge on an atom is the number of protons minus
the number of electrons. We can report these values using something called a nuclide symbol.
These consist of the chemical symbol for the element, with the atomic number in subscript to
the left, the mass number in superscript to the
10:00 - 10:30 left, and the charge in superscript to the right.
We will have to interpret these nuclide symbols, so just remember the definitions of these terms
and where they go. For example, look at this nuclide symbol for magnesium. We see 12 down
here, which means 12 protons, which is actually slightly redundant, because every magnesium atom
in the universe must have 12 protons to qualify as a magnesium atom. Then we see 24 up here,
which means there must be 12 neutrons, since
10:30 - 11:00 12 plus 12 is 24. And then this plus two charge
means the atom has lost two electrons compared to the neutral atom, which leaves 10 electrons.
With the submicroscopic structure of the atom understood, we need to be able to talk about
matter on the macroscopic level, as well. This is hard, since molecules are way too small to see,
and macroscopic amounts of a substance contain an unbelievable number of molecules. That’s
why we came up with the concept of the mole.
11:00 - 11:30 A mole is just a word that describes a number,
like the way a dozen means 12. But it is a very large number that allows us to convert
between atomic mass and grams. For example, carbon weighs on average about 12 atomic mass
units. According to the definition of a mole, a mole of carbon atoms will therefore weigh 12
grams. This demonstrates how the mole is our
11:30 - 12:00 way of converting between atomic mass units
and grams, so that we can discuss molecules in terms of numbers, but have that number be so
large that it represents a quantity that we can see with our eyes and do chemistry with. In other
words, this way we can weigh out matter in grams and do chemistry with it, but still be talking
about numbers of molecules and thus respect the ratios in which these molecules react. The number
of items in a mole is called Avogadro’s number,
12:00 - 12:30 which is equal to 6.022 x 1023, which is nearly a
trillion trillion. So that’s precisely the number of carbon atoms in 12 grams of carbon, because
one carbon atom weighs 12 atomic mass units. The mass of one mole of a substance is
called the molar mass. Elements will have a molar mass equal to their atomic mass
but in grams per mole instead of atomic mass units. Compounds will also have a molar mass,
and it will be equal to their molecular mass,
12:30 - 13:00 so to find the molar mass of a compound we simply
add up the atomic masses of all the atoms in the molecule, and then we express that number in
grams per mole instead of atomic mass units. It should be very easy to convert between grams
and moles for any compound. Let’s say we want to know the number of moles in 28.35 grams of
glycine. We can simply find the molecular mass
13:00 - 13:30 by adding up the atomic masses of all the atoms
in the molecule. Using the molecular formula of C2H5O2N, we get two times twelve for the two
carbons, five times one for the hydrogens, two times sixteen for the two oxygens, and
fourteen for the lone nitrogen. Adding those values up will give us a mass of 75, which
if expressed in atomic mass units will be the molecular mass, but if expressed in grams
per mole it will represent the molar mass,
13:30 - 14:00 or the mass contained in one mole of glycine
molecules. Then we convert our mass into moles. We will multiply our gram value by this conversion
factor, putting moles on the top and grams on the bottom so that grams cancel, and doing the
arithmetic we will get 0.38 moles of glycine. We can go the other way as well, from moles to
grams. Let’s say we are looking at vitamin C,
14:00 - 14:30 which has the molecular formula C6H8O6. Say
we have 1.42 x 10-4 moles, but we need this in grams. Once again, adding up the atomic
masses of all the atoms in the molecule, we can get a molar mass of 176 grams per mole. If
we multiply our value in moles by this conversion factor, we can see that moles cancel, and we
will get an answer of 0.025 grams of vitamin C.
14:30 - 15:00 With moles understood, we can start to better
understand compounds and their compositions, as well as how these compositions
can be determined. This will involve discussing empirical and molecular formulas.
The percent composition of a compound is the percent of the molecular mass that is represented
by each element in a compound. This is easy to calculate if we know the molecular formula of a
compound, because we can then know the molecular
15:00 - 15:30 mass. If we know the molecular mass, we can just
find the fraction of the molecular mass that is contributed by each element. Let’s say we want
to know the percent composition of ammonia. We know that ammonia has a molecular mass of 17
atomic mass units, because the nitrogen atom has a mass of 14 atomic mass units, and each
hydrogen atom has a mass of 1 atomic mass unit, for a total of 17. We can simply calculate the
mass of each element present in the compound
15:30 - 16:00 over the total mass of the compound to get
the percent composition of the compound. If one nitrogen atom is 14, then 14 over 17 will give
us 0.82, which times 100 gives us 82%. This means that the nitrogen atom in ammonia represents 82%
of the mass of the molecule. The three hydrogen atoms have a total mass of 3, and 3 over 17 gives
us 0.18. Multiplying by 100, that gives us 18%,
16:00 - 16:30 so hydrogen represents 18% of the mass of the
molecule. And 82% plus 18% does add up to 100%, so these calculations do make sense.
This line of thinking is actually a great way to determine the molecular formula of an
unknown compound. We can do this by first figuring out the empirical formula of a compound, which
is the lowest whole number ratio of the number
16:30 - 17:00 of atoms of different elements in a compound.
Let’s say we combusted an unknown hydrocarbon, which is a compound consisting of only carbon
and hydrogen, and collected the resulting carbon dioxide and water. After performing some basic
calculations, we determine that there was 1.71 grams of carbon and 0.287 grams of hydrogen in the
initial sample. Since these values are in grams, they do not tell us anything about the empirical
formula, because every element has a different
17:00 - 17:30 mass. Instead, we must convert these to moles
to make sense of a numerical ratio. We can use the molar masses of each element to convert to
moles. 1.71 grams of carbon times 1 mole over 12.01 grams gives us 0.142 moles of carbon atoms
in the original sample. Doing the same thing for hydrogen, 0.287 grams of hydrogen times 1 mole
over 1.008 grams gives us 0.284 moles of hydrogen
17:30 - 18:00 atoms in the original sample. Let’s divide both
of these numbers by the smaller number so that we can try to get a whole number ratio. 0.142 over
0.142 gives us 1, and 0.284 over 0.142 gives us 2, or a 1 to 2 ratio. So we can see from these
calculations that there must have been twice as many hydrogen atoms as carbon atoms
in the sample. This makes the empirical
18:00 - 18:30 formula for the unknown substance, CH2. We must
realize that this is not the molecular formula, which tells us the actual number of atoms of each
element in the compound. The compound could have many more than one carbon atom, but however many
carbon atoms are in the compound, there must be twice as many hydrogen atoms. At any rate, we
can perform a calculation like this for any compound containing any combination of elements,
we just use the molar mass of each element and
18:30 - 19:00 convert the mass into moles to find the molar
ratios, and therefore the empirical formula. We can also get the molecular formula if we have
the molecular mass of the compound, which we can get through mass spectrometry. In such a case,
we would just find out how many multiples of the formula unit are required to get a total
mass equivalent to the molecular mass. Given the previous example with an empirical formula of
CH2, let’s say that we knew the molecular mass was
19:00 - 19:30 42. The mass of CH2 is 14, 12 from carbon and two
from hydrogen, and 42 divided by 14 is three, so we just multiply the formula unit by three to get
C3H6, and that must be the molecular formula, as it obeys the ratio of the empirical formula, and
has a mass that is equal to the molecular mass.
19:30 - 20:00 With empirical and molecular formulas
understood, we have to dive back into the atom and learn more about electrons.
Precisely how are these distributed within an atom? This will be important to understand
in order to discuss chemical reactions. Again, atoms contain both protons and electrons,
and these have opposite charge, which means they are attracted to one another. This attraction
is described mathematically by Coulomb’s law, which says that the force between two charged
particles is proportional to the product of their
20:00 - 20:30 charges divided by the square of the distance
between them. If opposite charges this will be an attraction, if the same charge it will be
a repulsion. Greater magnitude of charge means greater force, and closer together means greater
force, while farther away means lesser force. Electrons themselves reside in things called
atomic orbitals, or three-dimensional regions of probability surrounding the nucleus where an
electron can be found, and there are different
20:30 - 21:00 kinds of quantum numbers which will describe
these orbitals. The first quantum number is the principal quantum number n. This refers to
the energy level or the shell that the electron resides in. A higher n value means a higher
energy and further away from the nucleus. The next number will be the angular momentum quantum
number, L. This can have any value from 0 to n-1, meaning if n is 1, L is 0. If n is 2, L can be
0 or 1, and so forth. L will define the type
21:00 - 21:30 of orbital the electron is in. An L value of 0
corresponds to s orbitals. Those are spherical, and they increase in radius as n increases. If
L is 1, we are discussing p orbitals, which are lobes that extend on each of the X, Y, and Z
axes. If L is 2, we are looking at d orbitals,
21:30 - 22:00 which look a bit stranger. S, p and d are the
most important ones for our purposes. Next, we have the magnetic quantum number, m sub L.
This can be anywhere from –L to L, so if L is 2, and we are discussing d orbitals, L can be -2,
-1, 0, 1, or 2. This is why there are five d orbitals per energy level, because there are five
possibilities for m sub L and each one corresponds
22:00 - 22:30 to an individual orbital. For precisely the
same reason, there are three p orbitals per energy level, with m sub L values of -1, 0, and 1,
and there is only one s orbital per energy level, with an m sub L value of zero. Lastly, there is
the spin quantum number, m sub s. This will be positive one half or negative one half, and
since a maximum of two electrons can fit in any atomic orbital, each pair will receive
opposite spin values, which we can call spin
22:30 - 23:00 up or spin down. The key thing to understand is
that the n value describes a shell of electrons, and the L value describes a subshell. So there
is an n = 3 shell, and within that there is a 3s subshell, and a 3p subshell, and a 3d subshell.
Then m sub L describes an individual orbital within a subshell, and m sub s differentiates
between the two electrons within an orbital.
23:00 - 23:30 Now we need to understand how electrons
fill up these orbitals. As n increases, the energy of the orbital increases, as we are
moving farther away from the nucleus, so Coulomb’s law says the attraction to the nucleus will
decrease. We should also know that within a shell the energy increases from s to p to d orbitals.
So 1s is the lowest energy orbital, then 2s,
23:30 - 24:00 2p, 3s, 3p, and so forth. But this pattern isn’t
followed precisely when we get to larger atoms, the first deviation being that the 3d orbitals
are higher in energy than the 4s. Looking at this diagram, we can see the precise order of the
orbitals in terms of increasing energy. Since a system will always want to be at the lowest energy
possible, this is the order, from bottom to top,
24:00 - 24:30 that an atom will arrange its electrons. This
order in which the orbitals are filled is called the Aufbau principle. Additionally there is
Hund’s rule, which says that when looking at a set of degenerate orbitals, which means orbitals of
the same energy, as a set of p orbitals or a set of d orbitals will always be, we must place one
electron in each orbital first before doubling them up. So for these p orbitals, each one gets
a spin up electron first, and then we start
24:30 - 25:00 generating pairs by placing spin down electrons.
Each electron within an atom must be assigned an orbital, and the specific arrangement of
electrons amongst the orbitals within an atom is called the electron configuration
of the atom. Many properties of an element will depend on its electron configuration, so
let’s make sure we understand these as well. The convention for reporting an electron
configuration is to list all the types of orbitals that are occupied along with a number to indicate
the occupancy of those particular orbitals. Each
25:00 - 25:30 item in an electron configuration should have the
n value, followed by the letter that corresponds to the type of orbital, and a superscript that
describes the number of electrons contained in that subshell. So this would be read 2p4, which
refers to a total of 4 electrons that exist in the 2p orbitals. Let’s make sure we understand that
neither of these two numbers is telling us how
25:30 - 26:00 many orbitals are being described, as that number
is implied, since each energy level contains 1 s orbital, 3 p orbitals, and 5 d orbitals.
So when assigning an electron configuration we are starting with the lowest energy orbital,
the 1s, and building up to the higher energy orbitals according to the Aufbau principle and
Hund’s rule, until all the electrons are assigned to an orbital. A convenient way to follow the
Aufbau principle is to simply know what sections
26:00 - 26:30 on the periodic table correspond to which
subshells. Looking at the periodic table now, we must understand that each period, or
row on the table, represents a shell, or a particular n value. The first row
is n = 1, then n = 2, and so forth. Then, we must know that this section containing groups
1 and 2 is called the s block. This section is the p block. The transition metals are the d block,
and the lanthanides and actinides are the f block,
26:30 - 27:00 though we won’t be too concerned with f orbitals
here. The only trick is that the d block is always one behind the period number in terms of principal
quantum number. For example we can see that in the 4th period it’s actually the 3d orbitals that
follow the 4s. If we can internalize this way of looking at the periodic table, then the Aufbau
principle reveals itself as we simply read left to right and up to down on the table. Starting
at the top left corner, the order would be 1s,
27:00 - 27:30 2s, 2p, 3s, 3p, 4s, 3d, 4p, and so forth, which
is precisely the order dictated by the Aufbau principle. This will make it much easier for us
to assign electron configurations to any atom. We should now be able to assign the electron
configuration of any element. This is easy to do if we simply look at where an element sits on
the periodic table, and list off the subshells
27:30 - 28:00 that the element will utilize by going left to
right and up to down on the table until we get to the element in question. Take chlorine for
example. In order to get to chlorine, let’s start up at the top left corner, and read off the
subshells. 1s will be full, so 1s2. Same with 2s, so 2s2 and 2p6 from period 2. Then 3s2, and
when we get to the 3p orbitals, we count 1,
28:00 - 28:30 2, 3, 4, 5 to get to chlorine. 3p5. That gives
us 1s22s22p63s23p5 as the electron configuration for chlorine. This makes perfect sense, as
neutral chlorine has 17 electrons to place, and this is the lowest energy configuration
for the distribution of these 17 electrons. With electron configuration understood, we
can begin to truly understand the structure
28:30 - 29:00 of the periodic table, and why elements are
arranged in the groups as they are. Let’s take a closer look at the periodic table
and see what else we can learn from it. Looking at the table now, we can see rows called
periods and columns called groups, and elements will be in the same group because they have
similar electron configurations. Specifically, they have the same number of valence electrons,
which are the electrons in the outermost shell.
29:00 - 29:30 In group 1, all the configurations end in s1. In
group 2, they end in s2. You can see that in every group, the electron configurations end the same
way as the other elements in that group. So as we move forward and learn about the periodic table,
it is the number of valence electrons that will determine the reactivity and properties of any
particular element, as the valence electrons are the ones that are available to do chemistry. Those
electrons that are not in the outermost shell,
29:30 - 30:00 and are therefore not valence electrons, are
called core electrons. These are the ones in the inner shells, which do not participate
in chemistry. So most elements have many core electrons, and just a few valence electrons,
particularly as we get lower on the table. We must comprehend a set of periodic trends,
meaning properties that atoms possess which change in a predictably periodic way as we move in some
direction along the table. The first property we will look at is the atomic radius. It’s difficult
to measure the radius of a lone atom, so the
30:00 - 30:30 convention is to tabulate lists of covalent radii,
which are defined as one half the distance between the nuclei of two identical atoms that are bonded
to each other. This should be roughly the same as the radius of the atom outside of the context
of a chemical bond as well. When we examine various covalent radii, we notice that the radius
will increase as we go down the periodic table. This is because when we go down a row on the
table, we are increasing the n value by 1,
30:30 - 31:00 thus adding a shell and placing the valence
electrons farther away from the nucleus. This makes the atom larger, as well as its covalent
radius. Then moving horizontally, as we move to the right along a period, the covalent radius will
decrease slightly. This may seem counterintuitive, as the addition of electrons doesn’t seem like
it should result in a smaller radius, but we must realize that as we move to the right we are
also adding protons, given that the atomic number
31:00 - 31:30 is increasing, and the more protons there are
in the nucleus, the greater the electromagnetic attraction that will pull the electrons in the
existing shells a bit closer to the nucleus. There are a few deviations to this trend, particularly
if we were to examine the transition elements of a particular period, but in general, atomic
radius will decrease as we move through a period. So radius increases going down and left,
and decreases going up and right on the table.
31:30 - 32:00 So that covers covalent radii, which essentially
refer to the size of an atom. But what happens to this radius when an element loses or gains
electrons to become an ion? Any change in the number of electrons should affect the radius
in some way. As it happens, any time an atom loses an electron, the remaining valence electrons
will still feel the same effective nuclear charge, but distributed amongst fewer electrons,
so it will cause the radius to contract. This means that any cation has a smaller ionic
radius than the covalent radius of the neutral
32:00 - 32:30 atom. This difference can be dramatic if all the
valence electrons are lost, since this will result in the removal of an entire shell, dropping
down to the shell below. But if an atom gains electrons, the effective nuclear charge will be
distributed amongst more electrons than before, and there will be additional electron
repulsion amongst the valence electrons, which results in an expansion of the radius. We
can see a concrete example with aluminum. If all
32:30 - 33:00 three valence electrons are lost, it will lose
its entire valence shell, and therefore will have a dramatically reduced radius. Sulfur on the
other hand, when it becomes the sulfide ion, the two additional electrons will cause the
radius to increase quite a bit, since there are no additional protons to pull the electrons,
just more electrons that will push the radius out. We might sometimes compare isoelectronic
species. These are atoms and ions that have
33:00 - 33:30 the same electron configuration. For example,
let’s look at the different species that can exhibit the electron configuration 1s22s22p6.
We can see that beyond just neon, a number of different ions can have this configuration if the
corresponding neutral atoms gain or lose a certain number of electrons. When comparing isoelectronic
species, the radius will decrease as the atomic number increases. This is because they will all
experience the same amount of electron repulsion,
33:30 - 34:00 since they have the same number of electrons,
but as we add more protons to the nucleus, this pulls the electrons closer to the nucleus.
Next let’s look at ionization energy. This is defined as the energy required to remove the
outermost electron from an atom in the gas phase and in its ground state configuration. The higher
the ionization energy, the more difficult it is to remove the electron, which tells us something
about the atomic radius of the atom as well as
34:00 - 34:30 the effective nuclear charge felt by the electron.
Each element will have a first ionization energy, which is the energy required to generate the
1+ cation, and they will also have successive ionization energies, like the second ionization
energy, to go from 1+ to 2+, and so forth. Each ionization energy will be larger than the last,
because it will get harder and harder to remove electrons the more positive the ion becomes, as
each ionization is a further destabilization.
34:30 - 35:00 The electron that is removed will always be the
outermost electron. As the atom gets larger, the outermost electron gets farther away
from the nucleus, and therefore becomes easier to remove. Every time we add a shell,
we are moving further away from the nucleus, so ionization energy decreases as we move down the
periodic table. Since atomic radius also decreases going to the right within a period, we can expect
the ionization energy to increase at the same
35:00 - 35:30 time. As we go, we are adding protons, contracting
the radius, and holding electrons more tightly, so they are harder to remove. That means in
general, while atomic radius increases down and left, ionization energy will increase up and
right, precisely the opposite of the radius trend. That means helium is the most difficult element
to ionize, with a single shell that is totally full and close to the nucleus, while francium is
the easiest, with a lone electron in an outermost
35:30 - 36:00 shell that is very far from the nucleus.
The energies of the electrons in an atom can be determined by photoelectron spectroscopy.
With this type of spectrum, the energy required to remove an electron from a particular subshell
is shown on the horizontal axis, and then the vertical axis tells us how many of those electrons
are in that subshell. Further to the left means a greater binding energy which means
electrons that are closer to the nucleus, starting
36:00 - 36:30 with the 1s electrons. Then moving to the right
they get lower in energy and farther from the nucleus. When we see these spectra we should be
able to recognize which peak corresponds to whch subshell based on its position on the horizontal
axis, and also state how many electrons are in each subshell based on the height of the peak.
We also want to learn about electron affinity. This is precisely the reverse concept of
ionization energy, it is the energy change
36:30 - 37:00 involved with adding an electron to a neutral
atom in the gas phase, thus forming a negatively charged ion. This process could absorb energy
or release energy, depending on the element, and a negative electron affinity will mean that the
process is actually favorable for a given element. Looking at this table, we can see that the
trend is similar to the ionization energy trend, since the harder it is to remove an electron,
or the higher the effective nuclear charge,
37:00 - 37:30 the easier it is to add an electron, and thus a
greater electron affinity. This is why elements like fluorine and chlorine have very large
electron affinities, as gaining an electron will endow them with noble gas electron configuration,
which is a very stable situation. So in general, electron affinity increases going up and
right on the table, with some exceptions. Noble gases do not follow this trend, as with
a full shell of electrons, it is typically
37:30 - 38:00 not favorable to add another electron, so we
discount them when considering this property. And finally, let’s examine electronegativity.
Electronegativity is a measure of how well an atom can attract electron density towards
itself, which is measured by looking at the way electrons are shared in chemical bonds. The more
strongly it can attract electrons, the greater its electronegativity. Electronegativity will
depend on atomic radius, since a smaller atom with a greater effective nuclear charge will attract
electrons more strongly, so the electronegativity
38:00 - 38:30 trend will be the same as the ionization energy
trend, it will increase going up and right on the periodic table. Fluorine will have the
greatest electronegativity, and francium will have the lowest. Again, we will exclude the noble
gases from this trend, as with their full valence shells, they are not likely to share electrons,
making electronegativity meaningless for those elements. There is a common point of confusion
that we should make abundantly clear. We must
38:30 - 39:00 make the distinction between electronegativity and
electron affinity, because the latter involves an actual ionization and an associated energy change
that is measurable. The former just describes a relative calculation of how well an atom attracts
the electrons in a bond, which does not involve any transformation, and it is listed on an
arbitrary relative scale from zero to four. And
39:00 - 39:30 so to put it all together, atomic radius increases
going down and left on the table, while ionization energy, electron affinity, and electronegativity
all increase going up and right on the table. And that concludes a review of Unit 1. I’ll
see you over in Unit 2 for more chemistry.