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    SOLID STATE NMR SPECTROSCOPY APPLIED TONATURAL ORGANIC MATTER AND

    ENVIRONMENTAL SAMPLES

    Pellegrino Conte

    Dipartimento di Ingegneria e Tecnologie Agro-Forestali,Universit degli Studi di Palermo

    Contact: [email protected]

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    Definition of Natural Organic Matter (NOM)

    The decomposition of plant, animaland microbial material in soil andwater produces a variety of complex

    organic molecules, collectively callednatural organic matter. Thesecompounds play many importantroles in the environment.

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    Roles of Natural Organic Matter (NOM)

    NOM is ubiquitous in soils, watersand sediments.

    In agriculture, NOM is importantbecause of its positive effects onthe structure, water retentionand nutrient properties of soils.

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    Roles of Natural Organic Matter (NOM)

    NOM also interacts with metal ionsand minerals to form complexes ofwidely differing chemical andbiological nature.

    Solubility, mobility and toxicity ofmany trace metals are stronglycorrelated with the concentration of

    natural organic matter in soil andwater.

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    Roles of Natural Organic Matter (NOM)

    NOM interacts with organicpollutants (i.e. polycyclic aromatic

    hydrocarbons, PAH) to reduce theirenvironmental availability and toxicity

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    Roles of Natural Organic Matter (NOM)

    Natural organic matter createsproblems for the water supplyindustry. It is required its removal inorder to minimize water color andeliminate formation of potentiallyharmful chemical byproducts as aresult of chlorination.

    Through a process called "bio-fouling," natural organic matter is

    also a major culprit in degrading theperformance of membrane filtrationsystems used for water purificationand desalination.

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    Models for studying NOM complexity

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    Nature of Natural Organic Matter (NOM)

    Persistent and universal naturalorganic matter molecules are in theenvironment, they are littleunderstood.

    Natural organic matter has no uniquestructure or composition, cannot becrystallized and is extremely difficultto characterize.

    Structure proposed by Flaig (1960)

    Structure proposed by Stevenson (1982)

    Structureproposed byStein (1997)

    Structure proposed bySchulten (1993)

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    Nature of Natural Organic Matter (NOM)

    Natural Organic Matter is a complexmixture of several different self-

    aggregatingcompounds formingsupramolecular aggregates.

    The size of each molecular systemwithin NOM does not exceed 2000Da.

    The new view (by Piccolo, 2001)

    Weak dispersive forcesare mainlyinvolved in the conformationalstabilization of NOM

    Saccharides

    Peptides

    Alkyl chains

    Aromatic systems

    Cations

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    Importance of NMR in characterizing NOM

    Solid state NMR(CPMAS 13C-NMR)

    Liquid state NMR(13C-NMR)

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    Liquid state 13C-NMR vs Solid state 13C-NMR spectroscopy

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    Hydrophobic core

    Hydrophilic moiety

    Water

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    Conformational analysis of NOM fractions

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    High performance size exclusion profile

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    ppm (t2)

    -200-1000100200300400

    =

    CH

    CH

    CH

    T

    CTHT

    T

    HT

    CT

    HT

    TItI

    )(1

    exp1)(

    exp)(

    1)(1

    1

    1

    1

    0

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    TCH: 1. fast local motionshigh TCH

    values;2. high amount of protonslow TCHvalues

    T1(H):proton spin lattice in therotating frame; fast local motionsshorterT1(H) values. High protonconcentrationfaster spin diffusionwith shorter T

    1(H) values.

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    Quantitative assessment of CPMAS 13C-NMR spectroscopy

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    What does it mean?

    (ppm)

    -40-20020406080100120140160180200220240

    Content of a chemical groupI

    i/I

    ix 100

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    1H 90 pulse

    Hartman-Hahn condition

    Contact time

    Spin diffusion

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    Measurement of1

    H90 pulse

    via CP

    via1

    H

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    Precise measurement of1H 90 pulse by application of a 4 x 90 CP pulse sequence

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    Spectra acquired with:

    1H 90 pulse calibrated on Gly

    1

    H 90 pulse calibrated on Glyand 4 x 90 CP sequence1H 90 pulse calibrated with 4 x90 CP sequence

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    Samples 1H 90 pulse (s) by

    DD (Inversion

    Recoverymeasurement)

    4 x 90 CP sequence

    SDS 3.12 2.83

    CMC 3.02 2.83

    HMB 3.06 2.83

    pepsin 3.11 2.80

    HA1 3.17 2.90

    FA1 3.12 2.88

    UM1 3.04 2.80

    HA2 2.96 2.80

    HA3 2.98 2.84HA4 3.05 2.84

    Between 2 and 6% of signalrecovery is obtained when aquantitative evaluation of CPMAS 13C-NMR spectra isdone after application of thecorrect 1H 90 pulse.

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    The Hartmann-Hahn Condition

    SSIIBB 11 =

    SI=

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    The rotor spin rate is directly related to thestrength of the dipolar interactions

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    Rotor spinning rate: 5kHz

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    Cross polarization

    Cross polarization

    with RAMP on 1H

    Cross polarizationwith RAMP on 13C

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    Effect of spin diffusion (Standard molecules)

    SO4-

    12

    34

    56

    78

    910

    1112

    OH

    O

    OHO

    CH3

    12

    34

    5

    6

    78

    9

    10

    CH3

    CH3

    CH3

    CH3

    CH3

    CH3

    Hexamethylbenzene (HMB)

    Sodium dodecylsulphonate (SDS)

    Ferulic Acid

    12

    3

    4

    5

    O

    OH

    O

    6

    OH

    O

    CH27 O

    O

    O

    *

    *

    n

    Carboxymethylcellulose sodium salt (CMC)

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    Standards Humic substances

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    Solid state NMR in the differentiation of NOM of different origin

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    Solid state NMR in the analyses of bulk soils

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    A Chinese soil

    An Italian soil

    An Australian soil

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    CONCLUSIONS

    1. Solid state NMR spectroscopy is a very powerful tool to analyzehardly soluble natural organic matter

    2. It is the only way to obtain quantitative information on the chemicalnature of NOM

    3. It provides information on the chemical nature of organic matterdirectly in bulk soils

    4. It can be used to study the interactions between NOM and theinorganic moieties of soils as well as the interactions withenvironmental pollutants

    5. Further applications are still possible such as solid state 31P-NMR(for the analyses of phosphorous cycle in the environment), 27Al-and29Si-NMR (for the understanding of amorphous clay minerals)