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Analyses plan Module 19

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Title: Difference between total analysis, fractionation and species Author: rvogt_lokal Last modified by: rvogt Created Date: 10/8/2004 4:14:13 PM – PowerPoint PPT presentation

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Title: Analyses plan Module 19


1
Analyses planModule 19
  • Major base cations to be determined by ICP-AES
  • Conductivity and temperature
  • H determined using pH electrode
  • Al fractionation
  • Major anions to be determined by IC
  • Use of auto-pipettes
  • Total organic carbon
  • UV and Vis absorption

2
Conductivity
  • Master student lab V160
  • Ecoscan Con5 (Eutech instruments) conductivity
    meter.
  • The instrument is calibrated using 1000 and 1433
    µS calibration solutions
  • The measurements are done for quality control
    purposes in order to compare measured and
    calculated conductivity

3
H determined using pH electrode
  • Analytical Chemistry lab Ø109
  • Thermo Orion model 720 pH-meter with a Blueline
    11-pH electrode.
  • The pH-meter is calibrated with pH 4.00 and
    7.01 buffer solutions

4
Major base cations to be determined by ICP-AES
  • Ca2, Mg2, Na, K
  • Method will be demonstrated in Module 24
  • Appropriate calibration solutions are prepared by
    Masha
  • Conducted by Anne-Marie Skramstad

5
Major anions to be determined by Ion
Chromathograph (IC)
  • Analytical Chemistry lab Ø109
  • Tot-F, Cl-, NO3-, SO42-
  • Principle
  • The sample is injected in a flow of eluent
  • The analyte ions are separated by different
    degree of binding to the active sites on the ion
    exchange material
  • Ions with opposite charge of the analyte is
    exchanged with H or OH-
  • The activity of the analyte is and accompanied H
    or OH- in the eluent stream is measured by means
    of a conductometer
  • Presented by Hege Lynne et al

6
Total organic carbon
  • Analytical chemistry lab Ø 104
  • High temperature (680C) catalytic combustion
    analysis on a Shimadzu TOC-5000A instrument
  • Principle
  • The organic carbon is combusted to CO2 by high
    temperature and catalysis. The amount of CO2
    produced is measured using av IR detector
  • Presented by Hege Lynne et al.
  • Analytes measured may include TC, IC, TOC, NPOC,
    and POC

7
Al fractionation
  • Master student lab V160
  • Method presented as example in Lecture 1 (slide
    15)
  • Download manual from
  • http//folk.uio.no/rvogt/KJM_MEF_4010/

8
QC of data
  • After the analysis the data must be compiled and
    quality controlled by ion balance and agreement
    between measured and calculated conductivity
  • For this purpose you may use the Data compilation
    and QC worksheet available at http//folk.uio.no/
    rvogt/KJM_MEF_4010/

9
Speciesin natural freshwater Central
equilibriums in natural water samples
  • KJM MEF 4010
  • Module 19

10
Inorganic complexes
  • Major cations in natural waters
  • H, Ca2, Mg2, Na, K
  • Common ligands in natural systems
  • OH-, HCO3-, CO32-, Cl-, SO42-, F- organic
    anions
  • In anoxic environment HS- S2-
  • Dominating species in aerobic freshwater at pH 8
    are

11
Hydrolysis
  • In aqueous systems, hydrolysis reactions are
    important
  • Hydrolysis reactions are controlled by H
  • The higher the pH, the stronger the hydrolysis
    of metal cations
  • E.g. Aluminium
  • Al3aq denotes Al(H2O)63

12
Concentrations of dissolved Fe3 speciesTwo
total Fe concentrations, FeT 10-4M and FeT
10-2M
13
Dissolved Organic Matter
  • Low molecular weight (LMW)
  • lt 1000Da (e.g. C32H80O33N5P0.3)
  • E.g.
  • High molecular weight
  • 1000 - gt 100 000Da
  • Humic substance
  • Very complex and coloured substances
  • Enhances weathering
  • The protolyzation of weak organic acids
  • Complexation of Al and Fe
  • Total congruent dissolution

14
Concentrations and activities
15
Activity
  • X?X X
  • X is the activity to X
  • X is the concentration to X
  • ?X is the activity coefficient to X
  • ?X are dimensionless
  • It is determined by
  • The diameter (å) of the hydrated X
  • Its valence (nX)
  • The ionic strength (I)

Not possible to calculate further than I0.1
n1
n2
n3
n4
  • ? ?? when I ? 0 ? ? 1 when Ilt10-5M

Anions cations
16
Debye Huckel (DH) equation
  • For ionic strengths (I) lt 0.1M the ?X can be
    calculated by means of e.g. the Debye Huckel
    equation
  • I lt 0.1
  • I lt 0.005
  • 0.5 0.33 are temperature dependent table
    values
  • Presented values are for 25C
  • åX is a table value for the specie in question
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