CHEM10006 Study Guide - Final Guide: Biogeochemical Cycle, Carboxyhemoglobin, Acid Strength

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The pH of pure water depends on temperature
Carbon & life
Carbon in atmosphere largely present as CO
2
Carbon in living systems present in biomolecules
In geosphere present as carbonate minerals & in
sediments
Cycling through biogeochemical cycle: oxidation
state ranges from -4 to +4
CO: odorless, colorless, neutral oxide, product of
incomplete combustion of fossil fuels, triple bond, a
ligand for Fe in myoglobin & haemoglobin, greater
affinity than O
2
: carboxyhemoglobin
CO
2
: colorless, non-toxic, some odour, product of
human respiration and combustion of fossil fuels, a
greenhouse gas, soluble, dissolves to carbonic acid,
determines the pH of natural waters & blood
Acids & Bases
Water undergoes self-ionization which involves the transfer of
a proton from one water molecule to another to produce a
hydroxide ion & hydronium ion
H
2
SO
4
is a stronger acid than other acidic forms
SO
3
has trigonal geometry
Phosphorus
Bones & teeth, DNA/RNA (phosphodiester link), energy
carriers, exists in minerals, allotropes
P
4
O
10
in water creates H
3
PO
4
(phosphoric acid): weak triprotic
acid: dissociates in a stepwise manner, undergoes
polymerization reactions
Gas solubility increases with pressure e.g. O
2
& N
2
Henry’s law: The amount of gas dissolved in a solution is
directly proportional to the pressure of the gas above the
solution: K
H
is the Henry’s law constant (i.e. equilibrium
constant)
As temperature decreases, stability increases due to less
kinetic energy: less escape from a liquid as gas
C
gas
= Molarity of gas in solution
P
gas
= Partial pressure of the gas
Rearranged:
The larger the value of K
H
,
the more soluble the gas
Calculating pH of Weak Acids
Esters
Organic esters: Formed by condensation reactions
between carboxylic acids & alcohols
Phosphate esters: Formed by condensation reactions
between phosphoric acid & alcohols
Energy captured by
photosynthesis stored &
transferred by phosphate
molecules
Energy stored as P-O bonds,
with the forward reaction
catalysed by ATPase
enzymes & reverse by
phosphatase enzymes:
energy released for
metabolic purposes
High charge repulsion in
trophosphase partially
relieved when ATP
hydrolyzed: releases energy
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Document Summary

H 2 so is a stronger acid than other acidic forms. Bones & teeth, dna/rna (phosphodiester link), energy carriers, exists in minerals, allotropes. P o 10 in water creates h 3 po 4 (phosphoric acid): weak triprotic acid: dissociates in a stepwise manner, undergoes polymerization reactions. The ph of pure water depends on temperature. Carbon in atmosphere largely present as co 2. Carbon in living systems present in biomolecules. In geosphere present as carbonate minerals & in sediments. Cycling through biogeochemical cycle: oxidation state ranges from - to + . Co: odorless, colorless, neutral oxide, product of incomplete combustion of fossil fuels, triple bond, a ligand for fe in myoglobin & haemoglobin, greater a(cid:1562)nity than o 2 : carboxyhemoglobin. Co 2 : colorless, non-toxic, some odour, product of human respiration and combustion of fossil fuels, a greenhouse gas, soluble, dissolves to carbonic acid, determines the ph of natural waters & blood.