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    This article was downloaded by: [114.79.28.90]On: 04 October 2014, At: 17:48Publisher: Taylor & FrancisInforma Ltd Registered in England and Wales Registered Number: 1072954Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK

    Soil Science and Plant NutritionPublication details, including instructions for authors andsubscription information:

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    Determination of Total Boron in

    Soil by the Curcumin-Acetic Acid

    Method After Extraction with 2-

    Ethyl-1,3-HexanediolHidekazu Yamada

    a& Tomoo Hattori

    a

    aDepartment of Agricultural Chemistry. Faculty of

    Agriculture , Kyoto Prefectural University , Shimogamo ,

    Kyoto , 606 , Japan

    Published online: 30 Oct 2012.

    To cite this article:Hidekazu Yamada & Tomoo Hattori (1986) Determination of Total Boron

    in Soil by the Curcumin-Acetic Acid Method After Extraction with 2-Ethyl-1,3-Hexanediol, SoilScience and Plant Nutrition, 32:1, 135-139, DOI: 10.1080/00380768.1986.10557487

    To link to this article: http://dx.doi.org/10.1080/00380768.1986.10557487

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    Short Communication

    oil Set. Plant Nutr., 3 1), 135-139, 1986

    DETERMINATION OF TOTAL BORON

    IN

    SOIL BY

    THE CURCUMIN-ACETIC ACID METHOD AFTER

    EXTRACTION WITH 2-ETHYL-l,3-HEXANEDIOL

    Hidekazu Y M D and Tomoo HATTORI

    Department o Agricultural Chemistry. Faculty o Agriculture.

    Kyoto Prefectural University. Shimogamo. Kyoto, 606 Japan

    Received February 12, 1985

    The curcumin-acetic acid method after extraction of boron into chloroform or

    methyl isobutyl ketone with 2-ethyl-I,3-hexanediol EHD) has been used for the deter

    mination of boron in fertilizers

    1)

    and foods 2). The extraction with EHD is so

    selective

    to

    boron that it appears to be a suitable procedure for the separation of boron

    from the solution of soil digests. The curcumin-acetic acid method is based on the

    fact that boron in the organic phase reacts with curcumin in an acetic acid-concen

    trated sulfuric acid medium, and this method

    is

    simpler than the conventional curcumin

    method that requires evaporation

    to

    dryness

    of

    the reagents.

    To apply this technique to the determination of boron in soil

    we

    evaluated several

    analytical conditions for the extraction of boron and color development in the cur

    cumin-acetic acid method.

    Experimental

    J Chemicals and reagents.

    Extracting solvent: dissolve

    200

    ml of EHD into

    chloroform, dilute to 1,000 ml with chloroform. Curcumin-acetic acid solution: dis

    solve 0.5 g of curcumin into

    250

    ml of hot glacial acetic acid 60-70C) in a polyethylene

    bottle. This reagent solution stored in a dark polyethylene bottle

    is

    stable for

    at

    least

    2 months. Standard boron solution: dissolve 2.858 g of boric acid HallOs) in water,

    dilute

    to

    500 mI.

    This stock solution contains I mg

    of

    boron per ml and

    is

    diluted

    to prepare the working solutions before use.

    2 Apparatus.

    Absorbance was read with a Hitachi

    100 60

    type spectrophotom

    eter using 1 cm glass cells. Phase separating filter paper, Whatman IPS, was used

    for the separation of the aqueous and organic phases.

    3 Procedure.

    Fuse 0.2 g of fine-powdered soil sample with I.S g of sodium

    peroxide,

    Na

    2

    0

    2

    , in a

    35

    ml nickel crucible for

    20

    min in an electric furnace

    at

    550C.

    Cool and place the crucible in a

    100

    ml polytetrafluoroethylene PTFE, Tefion) beaker,

    and add 5 ml of water in the crucible. Place a polyethylene-made watch glass on the

    Key Words: boron, 2-ethyl-l,3-hexanediol, curcumin.

    135

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    136 H. YAMADA and T. HATTORI

    beaker and allow to stand for 30 min to digest the melted product. Transfer the cru

    cible contents into the PTFE beaker. Wash the crucible several times with water and

    add the washings to the beaker. Acidify the solution in the beaker by gradual addition

    o

    approximately 4 ml

    o

    1 2)H

    2

    SO, and heat the beaker on a hot plate. After

    cooling, transfer the solution in the PTFE beaker into the 50 ml polyethylene bottle

    with a narrow mouth and dilute it to

    25 mt

    with water. Add 4

    ml o

    extracting solvent

    in the bottle and shake it for 3 min. Filter the contents in the bottle with a phase

    separating filter paper to separate the organic phase from the aqueous phase. To 1

    ml o the filtrate (organic phase) add 1 ml o curcumin-acetic acid solution and 0.25

    ml o concentrated sulfuric acid. Allow the mixture to stand for 30 min with occa

    sional shaking and dilute it to 50 ml with 95 ethanol. After 30 min, measure the

    absorbance at 550 nm with reagent blank as a reference, and determine the concentra

    tion o boron with reference to a calibration curve prepared at the same time.

    esults and dis ussion

    Elemental analysis o soils necessitates their decomposition into soluble forms by

    acid digestion

    or

    fusion with various fiuxes. As boron volatilizes easily from the acidic

    aqueous solution upon heating, alkali fusion is suitable for boron analysis o soil.

    Alkali fusion with sodium peroxide as a fusion fiux was chosen. Soil sample could be

    completely decomposed with the addition o an amount o sodium peroxide o more

    than six times the weight

    o

    the soil sample. A larger flux/sample ratio

    is

    desirable

    so that both the temperature and time o fusion can be kept to a minimum. But when

    sodium peroxide was added in excess, the amount o sulfuric acid to acidify the solu

    tion after fusion increased and the corrosion

    o

    the nickel crucible was accelerated.

    Therefore, 1.5 g o sodium peroxide was mixed with 200 mg o soil and the mixture

    was fused for 20 min at

    550C.

    Extraction conditions o boron with EHD and conditions for color development

    o

    the boron-curcumin complex in an acetic acid-concentrated sulfuric acid medium

    were also studied. The results obtained generally agreed well with the results reported

    by

    AOAZZI

    3)

    and by

    UENO

    and

    TODA

    (1);

    thus, this paper described a

    few

    improve

    ments in the method.

    t

    is well known that a small amount o water contaminating the organic phase

    affects the color development

    o

    the boron-curcumin complex: with only 50 ,ul

    o

    water

    present in 1

    ml o

    organic phase, the absorbance was about 85

    o

    that without water

    in the organic phase. To remove the interference from water, the filtration through

    a dry filter paper or the addition o a drying agent, such as sodium sulfate anhydride

    or propionic anhydride, has been tested. But when a phase separating filter paper

    was used, the phase separation and the dehydration

    o

    the organic phase could be

    achieved at the same time.

    The volume ratio

    o

    an aqueous to an organic phase is

    o

    importance in solvent

    extraction, because the recovery by extraction

    is

    closely related to the value o the

    ratio. A higher ratio is desirable as a means of concentrating boron, hence lowering

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    Determination of Boron in Soil

    .

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    138

    H. YAMADA and T. HATTORI

    Table 1. Reproducibility and recovery of added boron with the proposed method.

    Sample Sample taken (g)

    Soil A 0.200

    0.200

    SoilB

    0.100

    O

    100

    Boron added

    (Jlg)

    as B

    in the form

    of

    HaBOs

    o

    5.0

    o

    5.0

    Boron found Jlg)

    7.36, 7.18, 7.04, 7.48

    X=7.27 36.3 ppm in soil)

    S=0.194, CV=2.67%

    12. 1,

    12.3,

    12. 1,

    12.2

    X=12.2

    S=0.0957, CV=0.79%

    Recovery=98.3%

    2.14, 2.20, 2.24, 2.36

    X=2.24

    (22.4 ppm in soil)

    S=0.0929, CV=4.16%

    7.24, 7.12

    X=7.18 Recovery=98.9%

    X

    mean; S, standard deviation; CV, coefficient of variation. Soil A: collected from the plow layer

    of

    a paddy field

    at

    Kyoto Prefectural University. Soil B: collected from the surface

    of

    virgin land formed

    on serpentinite

    at

    Ooe-cho in Kyoto Prefecture.

    Table 2. Analytical results

    of

    boron in reference samples.

    Boron concentration Mean

    Reported value (4, 5

    (ppm)

    (ppm)

    (ppm)

    eference sample

    Soil SO-I 20.9, 24.1, 22.6

    22.5

    204

    SO-3

    29.7,

    28.9,25.9

    28.2

    227

    SO-4

    44.7, 47.9, 46.0

    46.2

    4310

    Rock

    JB-1

    8.8, 10.1, 10.9

    9.9

    JO-l

    5.9,

    6.5,

    6.0

    6.1 8.2*

    Arithmetic mean

    of

    reported values (5).

    (basalt) and JG- (granodiorite) from the Geological Survey of Japan were determined

    to evaluate the accuracy of the method. The boron contents obtained in this study

    were in good agreement with the reported values

    4, 5)

    for the reference samples (Table

    2).

    REFERENCES

    1) UENO, Y. and TODA, T., Determination

    of

    boron in fertilizer by using curcumin-acetic acid,

    iken

    Kaiho 29, 14-20 1976) (in Japanese)

    2)

    FUKUI,

    S.,

    HIRAYAMA,

    T.,

    NOHARA,

    M.,

    KOBAYASHI, K., KAWAMURA,

    T.,

    IWAIDA,

    M., lTo, Y.,

    OOAWA, S., KAKIUCHI, Y.,

    YAMAZAKI,

    H., and ONO, N., Colorimetric determination of boric acid

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    Determination of Boron in Soil

    139

    n

    food by chelate extraction with 2-ethyl-l,3-hexanediol

    and

    by using protonated curcumin,

    isei

    Kagaku,

    29, 323-328 1983) in Japanese)

    J

    AOAZZI E.J., Extraction flame photometric determination

    of

    boron,

    Anal. Chem.,

    39, 233-235 1967)

    4) STEaM, H.P. Certified reference materials,

    CANMET

    Canada Centre

    of

    Mineral andEnergy Tech

    nology) Report 80-6E 1980)

    S

    ANoo,

    A. KURASAWA

    H

    OHMORI,

    T., and TAKEOA E., 1974 compilation

    of

    data on the

    OSJ

    geochemical reference samples JG-l granodiorite

    and

    JB-l basalt,

    Geochem. J.

    8, 175-192 1974)

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