Showing posts with label spectroscopy. Show all posts
Showing posts with label spectroscopy. Show all posts

24 Feb 2017

Chemical Wonders: Experimental Techniques (Part 4) - Nuclear Magnetic Resonance

Nuclear Magnetic Resonance Spectroscopy


Note: Assumed knowledge or previous experience with NMR in High School or University. 

This is perhaps one of the most important tools of chemistry, which involves an analyte absorbing energies from radiofrequencies. In particular, the absorption of radiofrequencies, is affected by the magnetic environment of the atomic nuclei in compoundsThus it allows us to deduce structural information on the compound in question. It is typically used to determine the relative chemical environments of active atomic nuclei present in a compound, usually we analyse a solution of our analyte. Using a solution, we are also able to investigate the chemical behavior of the analyte.

We can take advantage of many different types of spectra depending on the atomic nuclei we want to analyse in a compound, the most commonly recorded spectra belongs to the Carbon-13 nuclei, in 13C NMR, usually used by organic chemists.

Suitable Nuclei


The three isotopes of hydrogen each have their own nuclei, which give their own NMR spectra.
From left: Hydrogen, Deuterium and Tritium. Wikimedia source

All nuclei have a property called "nuclear spin," a quantized property which is described by the spin quantum number, I, with the corresponding numbers 0, 1/2, 1, 3/2, 5/2 and so on. When nuclei aren't exposed to a magnetic field, the spin states are considered degenerate, i.e. the spin states have all the same energy. Conversely, when a magnetic field is applied to a nuclei, it becomes "split," i.e. it becomes non-degenerate, and the spin states have different energy levels. Nuclei where the value of I, is equal to 0, they are said to be NMR inactive. On the other hand, for nuclei where  I = 1/2, the nuclei is said to be NMR active, examples include 1H and 12C nuclei.  

The 13C NMR spectra is important, because the carbon-13 isotope has a relative natural abundance of 1.1 %, so when investigating a compound, only 1% of all carbon atoms present in the compound will be the isotope. As a result, the relationship between  1H - 13C coupling has a consequence on the observed NMR spectra.

Given all of this, what constitutes a suitable nuclei? And what are some important factors that determine when an NMR spectra will be observed?

  • The nuclear spin quantum number needs to be ≥ 1/2;
  • In general, it is advantageous for the particular nucleus to be in relative abundance, the 13C  isotope is one exception, though. Abundance of a particular isotope (isotopic enrichment) can be utilized to enhance the signal : noise ratios;
  • The nucleus must posses a relatively short spin-relaxation time (T1, given in seconds), which is dependent on the properties of the molecular environment and the nucleus itself;
  • Finally, if I > 1/2, it results in a  non-spherical distribution of nuclear charge, which is termed a quadrupole moment. This leads to relatively short values and causes the signals associated with the quadrupole moment to appear broad; signal broadening is also observed on nuclei attached to the nuclei that possesses a quadrupole moment. For example, 11B as well as an 1H NMR spectra of protons attached to 11B. 
The importance of the T1  value becomes apparent when observing elements that have more than one NMR active form, for example 6Li and 7Li are both NMR active, but their values are different. Typically, 7Li has T< 3 s, while for  6Li is T1 ≈ 10 to 80 s. Considering the relative abundance of these isotopes, we find that 7Li has an abundance of 92.5%, which makes it more suitable than 6Li .

Chemical Shifts and Resonance Frequencies


You can read a table of frequencies at which you would be able to observe certain nuclei using NMR here. NMR spectrometers are calibrated to particular resonance frequencies which are specific to a nucleus (e.g. 1H, 13C, 11B, 35Cl, 37Cl absorb different radiofrequencies), for example a 400 MHz spectrometer set to 400 MHz, you will only be able to observe 1H nuclei; using the same 400 MHz spectrometer, but calibrated to 162 MHz, you would only be able to observe 31P. 

1H NMR experiments involve identifying protons that are in different chemical environments (i.e. a H is bonded to different groups/atoms), which resonate at different frequencies.

For example, the proton NMR spectra of benzene (C6H6) only appears to have
one peak. Why? Every 1H nuclei is bonded to the same 'environment' of a
C=C bonded to another proton.


The same is true for other types of NMR, which each give their own characteristic signals. Signals in an NMR spectrum are given a chemical shift value, 𝛿, which is relative to the specific radiofrequency of that nuclei. The chemical shift value is a parameter that is independent from the magnetic field applied to the analyte. It can be defined as:

𝛿 = (v - v0) / v=  Δv / v0

The value of 𝛿 is usually quite small and inconvenient, so we usually multiply by 106, converting it into ppm (parts per million). The IUPAC convention for 𝛿, according to their Gold Book is defined as:

𝛿 = (v - v0) in Hz / v0  in MHz

For  1H and 13C NMR, the standard reference is tetramethylsilane, SiMe4. It is used as a reference for the shift, so to speak, of the signals from a particular nuclei from the reference signal. A positive 𝛿 is a shift to a higher frequency, while a negative shift (or less positive), means there is a shift to a lower frequency. This difference is the chemical shift. 

Homonuclear spin-spin coupling


A nucleus can only occupy two spin states (-1/2 and +1/2), the energy difference between these spin states is dependent on the magnetic field produced by the NMR spectrometer. If say, there is a system where there are two magnetically non-equivalent 1H nuclei, there can only be situations (HA and HB) that can arise when a magnetic field is applied:
  • The NMR signal for HA is split into two equal lines when a magnetic field is applied to HB, these equal lines are also produced by HB. The lines produced by are dependent on the which spin state of is "seen" by the spectrometer. These protons are said have coupled, producing two "doublets." The coupling constant, J, which is measured in Hz is defined as the splitting that occurs between two lines in each doublet. 
  • When no coupling of nuclei occurs. The local magnetic field produced by the spin of results in two resonances, each of these a singlet, as no coupling has occurred between the two nuclei.

Heteronuclear spin-spin coupling

Statistically, the 13C nuclei is quite rare.  So in 1H NMR of say, acetone and assuming a natural distribution of carbon isotopes, you will not be able to observe the coupling of  1H - 13C. Conversely, You will observe this coupling when using 13C NMR spectrum on acetone, and will only observe a singlet because of the C=O group, and a quartet because of the two chemically equivalent -CH3 groups. You can see this in this spectra here.


Ion-solution exchanges can be observed using NMR


The exchange of cations into solution occurs at slow enough speeds to be observed at the NMR spectroscopic timescale. We utilize the 17O isotope as a label: because it is NMR active, and because I = 5/2. From the signal ratio of  17O present in a naturally isotopic distribution of co-ordinated water (recall H2O can form weak bonds with ions), you can actually find the hydration value of a given ion-water complex. For example, the Cu2+ ion has been found to co-ordinate (bond) with six water molecules, forming the complex ion [Cu(OH2)]2+ (hexaaquacopper(II)), forming an octahedral complex. See model below:

Hexaaquacopper(II), has six water molecules whose
hydration number using  17O can be observed.

Another exchange process are redistribution reactions, in which, substituents (chemical groups) are exchanged between chemical species - but - the types of bonds and number of bonds remain. Similar to a substitution reaction. For example, the reaction of Triethyl phosphite and Phosphorus trichloride:

PCl3  +  P(OEt)3    PCl2(OEt)  +  PCl(OEt)2


We can find were the equilibrium lies using 31P spectroscopy, and the rate data by analysing the variation in the signal integrals (peaks), conversely, you can find the equilibrium constant (Kc) when no more variation is found in  the signal integrals. Finding the equilibrium will allow you to find the all-important free energy change of the system (ΔGo = -RT ln K). Using this relationship you can then find the at varying temperatures using ΔGo =  ΔHo - TΔSo. Thus, we can find the equilibrium position can be found in relation to temperature (remembering that ΔHo is almost 0, using the second law of thermodynamics), we can then differentiate to eventually find:

d ln K / dT  =  ΔHo/RT2


I won't go into how NMR machines work, but here's what they look like:

A Bruker NMR spectrometer connected
to a computer. Wikimedia link.
A high-powered NMR machine from Varian, capable of
using 900 MHz frequencies. 


                                                                                      

18 Feb 2017

Chemical Wonders: Experimental Techniques (Part 3) - Chemistry in the Infrared

Infrared & Raman Spectroscopies


Infrared spectroscopy is an invaluable tool for chemists, and is applied in fields from astronomy to forensics. It takes advantage of the transitions between vibrational energy states of molecules, and in order to be classed a 'IR active,' there need to be a change in the charges of the dipole moment. The other mode of vibration, called Raman spectroscopy, deals specifically with the change in polarizability. Both IR and Raman spectroscopy are forms of vibrational spectroscopy. The IR region ranges from 20 cm-1 to 14 000 cm-1 (called near IR).

The wavenumbers of molecular vibrations

When a molecule is exposed to infrared radiation, its covalent bonds vibrate and stretch (think of it like stretching a spring), when this occurs the molecule undergoes harmonic oscillations. The energy levels of these vibrations are given by:
Ev = (v + ½)hv - (v + ½)2 hvxe      (Ev is in J, joules)
where v = vibrational quantum number; h = Planck constant; v = frequency of vibration; x = anharmonicity constant. At an energy level, where v = 0, is the zero point energy of the molecule. When dealing with a transition from the vibrational ground state, to the first excited state, the motion of this molecule is approximately one of a simple harmonic oscillator:
Ev = (v + ½)hv 
When considering a hypothetical diatomic molecule, say, XY you would find that the vibrational frequency is dependant on two factors: the mass of atoms X and Y; and the force constant (k) of the bond. The constant, k, is determined by the strength of the covalent bond or in other words the stiffness of the "spring." 
  • Diatomic molecules with where X and Y similar masses, they approximately contribute equally to the molecular vibration.
  • In molecules where X and Y have significantly different masses, the lighter atom moves more than the heavier one.
The reduced mass,𝜇, is the quantity that describes the mass of the oscillator so that it can more accurately reflects the relative masses of X and Y. This relationship is given by:
1/𝜇 = 1/mx + 1/my           OR           𝜇 = mxmy / mx + my 
The fundamental absorption of the molecule is the transition from the ground state to the first excited state. This relationship can be given by:
v = 1/2𝜋 √k/𝜇
where: v = the fundamental vibrational frequency (Hz); k = force constant (N m-1);  𝜇 = reduced mass; 𝜇 = reduced mass. Using these definitions, we can define the relationship of the absorptions in IR spectra in relation to the wavenumber, it can be defined as below:
 \scriptstyle\tilde{\nu}= 1/2𝜋c√k/𝜇 
where  \scriptstyle\tilde{\nu}wavenumber (cm-1); c = speed of light  = 3.00x1010 cm s-1.

Characteristics of IR spectra

The IR spectra produced from using a device such as the Fourier transform infrared spectrometer (FT-IR, shown above), can be separated into two main regions: the fingerprint region, which occurs in bands in the regions below 1500 cm-1, which arise from single bond stretching nodes, vibrations within the molecule and deformations in the molecular structure. Any absorption wavelength found above this region is typically what is used to identify key functional groups on the compound in question. The fingerprint region on the other hand is used to identify the characteristic signature of the compound, as the bands in these regions are specific to the overall structure of the molecule.
You can find a table of these functional groups here.
I mentioned that the IR spectra ranges from 20 cm-1 to 14 000 cm-1 (called near IR), however, in the lab, IR spectrometers typically use the range from 400 to 4000 cm-1, dubbed the 'mid-IR' section of the spectra. Data produced from the machines, like the FT-IR produce spectra in which the transmission (at arbitrary values 0 to 100%) against the wavelength of the IR bands. Samples in a typical FT-IR machine can be recorded using samples in gaseous, liquid or even solid samples. Samples in different states need to be prepared in different ways and result in slightly different IR spectra. 
Solids are typically prepared in a mull, mixing the solid with an organic oil, or it is pressed into a disc by grounding it with a an alkali metal halide (such as KBr). These forms of preparation affect the IR spectrum: the disc preparation reduces the range observed by the spectra, as it is transparent from 4000 to 450 cm-1, while NaCl is from 4000 to 650 cm-1. More modern machines utilise diamonds, the accessory known as a diamond attenuated total reflector (ATR), which allows us to avoid using mulls or discs.

Raman Spectroscopy

IR and Raman spectroscopy are two techniques which can be used together, and in 1930 Chandrasekhara V. Raman (pictured left) won the noble prize in physics. He discovered that radiation is scattered when a molecule is exposed to a frequency, v0, even though there is no change in frequency. This is called Rayleigh scattering, which is also responsible for the blue colour of the sky. A small amount of scattered radiation has frequencies of v0 ± v, where v is frequency of the vibrating section of the molecule. This is known as Raman scattering. It is actually quite an unsensitive because a only a small range actually undergoes Raman scattering. Improvements have been made by using Fourier transformation (FT) techniques. 
Raman spectroscopy is particularly useful because it utilises wavelengths below the normal IR spectroscopy range, this in turn, allows chemists to observe the vibrational nodes found in metal-ligand bonds. Coloured compounds rely on laser excitation that coincide with the absorption wavelengths in the electronic spectrum, known as resonance Raman spectroscopy. Utilising resonance enhancement allows for more clearly defined lines.

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Links provided bring you to some of the info I used from the web. the first/second-year university textbooks:
  • "Inorganic Chemistry," 4ED, by Housecroft & Sharpe, Pearson Ed. Ltd., 'Chapter 4 - Experimental techniques,' pgs 90-98. You can buy it here.
  • "Fundamentals of Analytical Chemistry," 9ED, Skoog & West, Pearson Ed. Ltd., 'Chapter 28 - Atomic Spectroscopy,' pgs 774-775, 790-799. You can buy it here.