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Surface Waters Module II D' Orvos

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Title: Surface Waters Module II D' Orvos


1
Surface Waters Module IID. Orvos
2
Phosphorous
  • In contrast to nitrogen, phosphorus in aquatic
    systems has no gaseous form and only one charged
    form (PO4-3). However, the water chemistry of
    phosphorus is complicated by its tendency to
    adsorb onto inorganic particulate matter and its
    incorporation into organisms to form organic
    phosphorus.

3
Phosphorous
  • Phosphorus is not needed large quantities like
    carbon, hydrogen, and nitrogen, but it is often
    the limiting factor for primary production in
    both terrestrial and aquatic environments. This
    occurs for 3 reasons
  • 1. phosphorus containing rocks are often scarce
    so the supply from rock breakdown may be poor.
  • 2. there is no gaseous stage of phosphorus so
    there is no equivalent to nitrogen fixation
  • 3. phosphorus is sufficiently reactive to be
    bound to many types of soil

4
Total P and Lake Productivity
  • lake productivity total P ug/L
  • ultra oligotrophic lt 5
  • oligotrophic 5-10
  • mesotrophic 10-30
  • eutrophic 30-300
  • hypereutrophic gt 300

5
Forms of P
  • 1. dissolved phosphate (PO4 -3)
    orthophosphate, reactive P
  • 2. dissolved total phosphorus orthophosphate
    DOP (see below)
  • 3. particulate phosphorus bacterial, plant and
    animal phosphorus and phosphorus absorbed to
    suspended inorganic particles

6
Forms of P
0.45 u filter
7
Phosphorous
  • Dissolved total P and particulate P must first be
    mineralized by an acid to reactive P before
    measurement.
  • Total phosphorus can be divided into particulate
    (filterable) and dissolved (filtrate) phosphorus.
    The filters are 0.45 µ polymer.
  • Only the orthophosphate can be used directly for
    algal growth, so it is often called reactive
    phosphorus.

8
Phosphorous
  • Relative to total soluble phosphorus there is
    usually much more particulate phosphorus.
    Particulate phosphorus includes phosphorus bound
    in bacteria, plants, and animals as well as
    phosphorus adsorbed to suspended inorganic
    particles such as clays.
  • Sources
  • weathering of rocks
  • particles in air
  • pollution (detergents, fertilizers) leads to
    cultural eutrophication
  • Losses
  • water effluents
  • organisms settle to bottom
  • insect hatches - fish removal
  • precipitates FePO4, MnPO4, Ca3(PO4)2

9
Phosphorous in Surface Water
  • Orthophosphate is lost from the open water by a
    variety of mechanisms but most involve
    precipitation of inorganic solid phosphate phases
    formed by direct precipitation with calcium,
    iron, etc. or sorption onto clay particles.
  • Phosphorus does not normally accumulate in lake
    waters because of rapid loss to the sediments,
    followed by little return of phosphorus in
    oligotrophic lakes and only more or less seasonal
    returns in eutrophic lakes.

10
Measurement of P
  • Phosphate is measured colormetrically with
    ascorbic acid. Total P must be digested via acid
    to convert it to orthophosphate, which is then
    quantified. Ion chromatography is also used.

11
Chlorine
  • Chlorine is a common disinfectant used in
    automated watering systems. At lower
    concentrations it is used to disinfect animal
    drinking water. At higher concentrations,
    chlorine is used to sanitize rack manifolds and
    room distribution piping. A chlorine test kit or
    titrator must be used to measure the
    concentration of chlorine in water.

12
Forms of Chlorine
  • Free Chlorine
  • Combined Chlorine
  • Total Chlorine

13
Free Chlorine
  • Chemistry important in disinfection
  • Free chlorine is defined as the concentration of
    residual chlorine in water present as dissolved
    gas (Cl2), hypochlorous acid (HOCl), and/or
    hypochlorite ion (OCl-). The three forms of free
    chlorine exist together in equilibrium.
  • Cl2 H2O ? HOCl H Cl-
  • HOCl ? H OCl-
  • As the pH falls below 2, the predominant form is
    Cl2. Between pH 2 and 7 the equilibrium is in
    favor of HOCl. At pH 7.4 HOCl and OCl- are about
    equal, while above this increasing proportions of
    OCl- are present.

14
Combined Chlorine
  • Combined chlorine is defined as the residual
    chlorine existing in water in chemical
    combination with ammonia or organic amines which
    can be found in natural or polluted waters.
    Ammonia is sometimes deliberately added to
    chlorinated public water supplies to provide
    inorganic chloramines.
  • Chloramines in presence of organic matter can
    form trihalomethanes. Importance?

15
Total Chlorine
  • Total chlorine is the sum of free and combined
    chlorine. When chlorinating most potable water
    supplies, total chlorine is essentially equal to
    free chlorine since the concentration of ammonia
    or organic nitrogen compounds (needed to form
    combined chlorine) will be very low. When
    chloramines are present in the municipal water
    supply, then total chlorine will be higher than
    free chlorine.

Germicidal strength of different forms of
chlorine in water are ranked as follows HOCl gt
OCl- gt inorganic chloramines gt organic chloramines
16
Biochemical Oxygen Demand
  • Often called biological oxygen demand, although
    that is technically incorrect
  • Abbreviated BOD
  • BOD refers to the amount of oxygen that would be
    consumed if all the organic material in 1 L of
    water (or wastewater or industrial effluent) were
    oxidized by microbes

17
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18
Measuring BOD
  • The first step in measuring BOD is to obtain
    equal volumes of water (or wastewater or
    industrial waste) from the area to be tested and
    dilute each specimen with a known volume of
    buffered distilled water that has been thoroughly
    shaken to insure oxygen saturation. The greater
    the sample BOD, the larger the dilution.

19
Measuring BOD
  • After this, an oxygen meter is used to determine
    the concentration of oxygen within one of the BOD
    bottles. The remaining vial is than sealed and
    placed in darkness and tested five days later.
    BOD is then determined by subtracting the second
    meter reading from the first. Why five days?
  • The range of possible readings can vary
    considerably water from an exceptionally clear
    lake might show a BOD of less than 2 mg/L of
    water. Raw sewage may give readings in the
    hundreds and food processing wastes may be in the
    thousands of mg of BOD
  • Engineers likes pounds of BOD!

20
CBOD and BODu
  • BODu is the ultimate BOD, i.e., the BOD with no
    time restriction placed on the test (although it
    is usually a 30-day test)
  • CBOD or Carbonaceous BOD represents the BOD from
    organic compounds and oxidation of inorganic
    compounds such as ferrous iron and sulfide. Any
    BOD from nitrifying organisms, which consume
    oxygen in the nitrification process of converting
    ammonia to nitrate, is removed by adding a
    nitrification inhibitor. Usually, CBOD BODu in
    most effluents

21
BOD Measurement Use
22
Chemical Oxygen Demand
  • The quantity of oxygen used in biological and
    non-biological oxidation of materials in water a
    measure of water quality. Acid heat are used
    to oxidize the sample.
  • The determination of chemical oxygen demand (COD)
    is used in municipal and industrial laboratories
    to measure the overall level of organic
    contamination in wastewater. The contamination
    level is determined by measuring the equivalent
    amount of oxygen required to oxidize organic
    matter in the sample.
  • BOD/COD ratio the greater the ratio, the more
    oxidizable (biologically treatable) the waste.
    Ratios rarely exceed 0.8-0.9.

23
Oxygen-Reduction Potential
  • The redox potential or oxidation-reduction
    potential (Eh) is the electrical voltage which
    exists between two electrodes, one made of
    hydrogen and the other made of the material under
    study.
  • When oxygen combines with a material chemical
    oxidation has occurred when oxygen is removed
    from a substance chemical reduction has occurred
  • Changes in the redox potential are important only
    in eutrophic conditions or in special limnologic
    environments such as highly reducing acidic bogs.
  • The oxidation state of many metal ions and some
    nutrient compounds are controlled by the amount
    of oxygen present and the associated redox
    potential.

24
Chlorophyll
Seasonal concentrations of chlorphyll a in a New
York lake Orvos et al., 2000.
25
Trace Metals
  • Many metals are present in small amounts. Often
    these are of concern because of source and
    potential effects to humans, plants, and animals.
    Common trace metals include Cu, As, Cd, Hg,
    and Pb. Metals are usually detected with atomic
    absorption spectrometry or ICP.

26
Trace Organics
  • Pesticides, volatile organic compounds (VOCs),
    PCBs, and a multitude of other compounds are
    found in surface waters. Its a whole other
    course of material.
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