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Dasar Ilmu Tanah Kemasaman Tanah Dan Masalahnya

Aug 07, 2018

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Dukut Wido
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  • 8/20/2019 Dasar Ilmu Tanah Kemasaman Tanah Dan Masalahnya

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    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    KEMASAMAN TANAH

    &Permasalahannya

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    Soil Acidity:

    auses and Impacts

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    1. Asam KarbonatCarbon dioxide gas from soil air dissolves in

    waterRoot respiration and soil decomposition provideextra CO2

    CO2  !2O !2CO"  !CO"#

      !

    2. Asam#asam dari $etabolism %iologis$icrobes brea& down organic matter' prod(cing

    organicacids s(c) as citric acid' carbox*lic acids andp)enolic acids

    RC!2O!+ O2  !2O RCOO! RCOO#

      !

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    roses#proses engasaman /ana)

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    0. O&sidasi itrogen ,itrication-itrogen memas(&i tana) sebagai !0

    3i(ba) men4adi asam nitrat .

    !0  2O2  !2O !

      !  O"#

    5. O&sidasi S(lp)(r6. Asam#asam dalam air )(4an

    !2SO0  SO02# 2!

    !O"  O"#

      !

    7. lant 8pta&e of Cationslants ex(de ! ions or ta&e (p anions ,eg.SO

    0

    2#- to

    balance o9 cation (pta&eSumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    roses#proses engasaman /ana)

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    Kation ! *ang di4erap pada perm(&aan liatdapat mer(sa& str(&t(r mineral dan melepas&anAl" dalam prosesn*a

    Al(mini(m sangat to&si& bagi &eban*a&an 4enis

    tanaman

    Al memac( )idrolisis !2O

    Al bergab(ng dnegan O!#

    ' meninggal&an !

     dalam lar(tan tana)

    /olerant plants secrete organic acids into t)esoil aro(nd

    t)e root. Organic acids s(c) as ,eg. malate orSumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    /o&sisitas Al.

  • 8/20/2019 Dasar Ilmu Tanah Kemasaman Tanah Dan Masalahnya

    9/23Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    1. Acids are ne(trali:ed in soils wit) available bases

    2. Canadian S)ield severel* a9ected in central and easternCanadaSumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

  • 8/20/2019 Dasar Ilmu Tanah Kemasaman Tanah Dan Masalahnya

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    !  !SO"#

    SO2 SO"sun

    O2!2SO0 ↔2!

      SO02#

    !  O"#

    22; O20O

    !2O

    0O2 2!O"  2!O22O2 22O

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    >fe& p! tana)/er)adap K/K 

    K/K mening&atdengan p!

    &arena=

    ,i- %inding andrelease of ! ions on p!#

    dependentc)argesites

    ,ii-!*drol*sisSumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    ersen Ke4en()an %asa ,K%-

    ? cmol of exc)angeable Ca2 $g2 K  

    a

      cmolc of C>C

    ? 1;; @ persen &e4en()an asam.

    !ote:  Percent acid saturation, though less often cited, is determinedbycmolc Al

    3+ & H+ ions divided by cmolc of CEC. This is actually more

    meaningful, because Ca, g, ! and "a ions are not true bases#

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

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    1. So"ls #"th h"gh cla$ or organ"c content tento ha&e the h"ghest bu'er"ng ca(ac"t$

    2. )h$* +m(ortance o, e-changeable an

    res"ual ac""t$

    Conto) roses en*angga=

    ,i- Al(mini(m )*drol*sis ,in ver* acid soils-

    AlO2  2O → AlO3 

    A"ng more "ons #"ll r"&e the react"on to the le,t.

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    roses#proses en*angga dalam tana)

    d l t )

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    16/23Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    roses#proses en*angga dalam tana)

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    ,ii- rotonation and deprotonation of organic matter

     "ons "ssoc"ate #hen a base "s ae (re&ent"ng( ,rom r"s"ng as much as e-(ecte.

    "ncreases as the  "ons are remo&e "ncreas"ngthe negat"&e charges

    ,iii- p!#dependent c)arge sites in cla*s

    Aga"n a"ng a base "ssoc"ates  "ons ,rom h$ro-$lgrou(s an o-$gen atoms

    ,iv- Cation exc)ange

    As "ons are ae most en u( attracte to negat"&echarge s"tes so that ( changes less than e-(ecte. +, abase "s ae the$ are re(lace b$  "ons or Al "ons,rom e-change s"tes. most e'ect"&e #hen (45.

    ,v- Carbonate dissol(tion and precipitation 6. 7.18

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    roses#proses en*angga dalam tana)

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    "m"ng"me reacts #"th O2 an 2O to (rouce b"carbonate

    O39

    Example:O3

    9  2 → O2  2O

    agO32  22O 2O2↔  a2  2O3

    9  g2  2O39

    •;"carbonate "s reactive wit) exc)angeableandresid(al soil acidit*

    a2

    an g2

     replace !

     and Al"

     on cla*

    H+

     

    Soil Colloid + CaCO3

      Soil Colloid-Ca++  + H2

    O + CO2

      H+

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    PENGAP!AN

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    19/23Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    roses#proses *ang mempengar()i p!tana)

  • 8/20/2019 Dasar Ilmu Tanah Kemasaman Tanah Dan Masalahnya

    20/23Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    >f & ) d ! )

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    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    >fe& engap(ran ter)adap p! tana)

    >f & ! t ) t ) d & d ! d

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    >fe& p! tana) ter)adap &and(ngan !ara dan$i&roba /ana)

    Sumber: classes.uleth.ca/200801/geog3080a/SOILS%20PART%20V%202008.ppt

    t ! t )

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    ,i-$etode at ewarnaCertain organic compo(nds c)angecolo(r inresponse to p!

    3rops of d*e sol(tion can be placed onw)itespot plate ,in contact wit) soil-

    ,ii-$etode otentiometri& 3i9erence between ! ion activit* insoil s(spension and glass electrodegives p!

    Sumber: classes uleth ca/200801/geog3080a/SOILS%20PART%20V%202008 ppt

    enent(an p! tana)