"#$%&'()*+,-./0, "1
Soil colloids
1*/. 2*..*/34 ,+5 675 8*46 2758/2,..9 ,2:;5 <+,2:*0 *< 4*/.4 =/67 ;5+9 48,.. 4/-5> .544 67,0 & ?8 /0 3/,8565+@ • A52,B45 *< 675/+ 48,.. 4/-5> ,.. 4*/. 2*..*/34 5CD*45 , .,+E5 5C65+0,. 4B+<,25 ,+5, D5+ B0/6 8,44@ • 1*/. 2*..*/34 2,0 ,F+,26 ,03 7*.3 D*4/:;5.9 27,+E53 /*04 3B5 6* 675/+ .,+E5 4B+<,25 ,+5, ,03 05E,:;5 27,+E54@ • G7/4 27,+,265+/4:2 /4 /8D*+6,06 H52,B45 8,09 D*4/:;5.9 27,+E53 /*04 ,+5 D.,06 0B6+/5064@ •
Soil colloids
1*/. 2*..*/34 ,+5 675 8*46 2758/2,..9 ,2:;5 <+,2:*0 *< 4*/.4 =/67 ;5+9 48,.. 4/-5> .544 67,0 & ?8 /0 3/,8565+@ • A52,B45 *< 675/+ 48,.. 4/-5> ,.. 4*/. 2*..*/34 5CD*45 , .,+E5 5C65+0,. 4B+<,25 ,+5, D5+ B0/6 8,44@ • 1*/. 2*..*/34 2,0 ,F+,26 ,03 7*.3 D*4/:;5.9 27,+E53 /*04 3B5 6* 675/+ .,+E5 4B+<,25 ,+5, ,03 05E,:;5 27,+E54@ • G7/4 27,+,265+/4:2 /4 /8D*+6,06 H52,B45 8,09 D*4/:;5.9 27,+E53 /*04 ,+5 D.,06 0B6+/5064@ •
Soil colloids
Crystalline silicate clay
Iron and aluminum oxide
!"#$% '( %')* +'**'),%
Non-crystalline silicate clay
Organic (Humus)
Silicate clay (crystalline and non-crystalline)
1/./2,65 2.,9 2*04/464 8,/0.9 *< :E76.9 H*0353> 4/./2*0 ,03 *C9E50 ,6*84@ • G75 3/I5+50254 H56=550 2+946,../05 ,03 0*0J2+946,../05 4/./2,65 2.,9 /4 675 ,++,0E58506 *< 47556K • L+946,../05 4/./2,65 2.,9M 675/+ 2+946,../05 46+B26B+5 /4 .,95+53 ./N5 D,E54 /0 H**N OP/EB+5 ,Q@ • )*0J2+946,../05 4/./2,65 2.,9M 3* 0*6 5C7/H/6 *+35+53> 2+946,../05 47556 OP/EB+5 HQ@ •
a
R,*./65 O2+946,../05Q The image cannot be displayed. Your computer may not have enough memory to open the image, or the image may have been corrupted. Restart your computer, and then open the file again. If the red x still appears, you may have to delete the image and then insert it again.
b
Basic units of silicate clay •
1/./2,65 2.,9 8/05+,. 2*8D*453 *< 6=* N/034 *
b
-)*)+'. !$/012$,01* 34 -)5 6 78
9*:;).):;<;1=.$%):; 7+/12$,01*34 9*>?=5 @ 7>7A8
Basic units of silicate clay: Sheets
G75 H,4/2 8*.52B.,+ ,03 46+B26B+,. 2*8D*0506 *< 4/./2,65 2.,9@ O,Q " 4/0E.5 656+,753+*0> 2*8D*453 *< , 1/ /*0 4B++*B0353 H9 <*B+ T& ,6*8M ,03 , 4/0E.5 *26,753+*0> /0 =7/27 ,0 ". O*+ UEQ /*0 /4 4B++*B0353 H9 4/C 793+*C9 E+*BD4 *+ T& ,6*84@ OHQ S0 2.,9 2+946,.4 67*B4,034 *< 67545
Basic units of silicate clay: Combined sheets
4B4
C'.< $D#1.,).=
E1'*).)/$5 !"##$%&'() -;$+H/$ 3?'.;'0)**'.)/$8
!"#$ '( %)*)+1/$ +*1"
GD#1.,).= I$0;)+:*)/$ FB4 C'.< $D#1.,).=
J).$<=01).$, ;)+1> K**)/$ L2*'0)/$
Basic units of silicate clay: Combined sheets
12758,:2 3+,=/0E /..B46+,:0E 675 *+E,0/-,:*0 *< 656+,753+,. ,03 *26,753+,. 475564 /0 *05 'K'J69D5 8/05+,. ON,*./0/65Q ,03 <*B+ &K'J69D5 8/05+,.4@
Charges of colloids
V W5+8,0506 27,+E54 • G7+*BE7 /4*8*+D7*B4 4BH4:6B:*0 • U*46.9 /0 &K' 4/./2,65 2.,94 X G58D*+,+9 27,+E54 • G7+*BE7 DY 35D503506 • Z5D503 *0 4*/. DY • S0 'K' 2.,94 ON,*./0/65Q> 7B8B4> ,..*D7,05 ,03 P5[". *C/354 • L7,+E5 +5.,653 6* TYJ E+*BD@
Isomorphous substitution • K%';'0#2':% %:M%H/:H'.K 675 +5D.,258506 *< *05 ,6*8 H9 ,0*675+
=/67*B6 *< 4/8/.,+ 4/-5 /0 , 2+946,. .,\25 =/67*B6 3/4+BD:0E *+ 27,0E/0E 675 2+946,. 46+B26B+5 *< 675 8/05+,. O2,:*0 +5D.,258506 /0 8/05+,.4Q@ • R0*=0 ,4 D5+8,0506 27,+E5 ,03 B0,I52653 H9 4*.B:*0 DY@ • U,]*+ 4*B+25 *< ^;5 27,+E5K +5D.,258506 *< 656+,753+,. 1/ _` ,03 *26,753+,. "._a 2,:*04 =/67 2,:*04 *< .*=5+ 27,+E5@ Substitution of Al3+ with Mg2+ formed one net –ve charge at exchange sites.
• •
W+53*8/0,65.9 /0 675 &K' 8/05+,.4@ T22B+ 3B+/0E 675 <*+8,:*0 *< 67545 8/05+,.4 ,03 B0,I52653 H9 D+54506 50;/+*08506,. 2*03/:*04@
pH dependent • • • • • • •
152*03 4*B+25 *< 27,+E54 /4 ,44*2/,653 =/67 53E5 27,+E5 *< 675 2.,9 8/05+,.4@ G75 bB,0:69 *< ^;5 ,03 _;5 27,+E5 *0 675 53E54 35D5034 *0 4*/. 4*.B:*0 DY@ G5+853 ,4 ;,+/,H.5 *+ DYJ35D503506@ c035+ .*= DY> 675 53E5 /4 _;5 H52,B45 *< 675 5C2544 Y _ /*04 ,44*2/,653 =/67 675 5CD*453 1/JTY ,03 ".JTY E+*BD4@ "4 4*/. 4*.B:*0 DY /02+5,454> 4*85 *< 675 Y_ /4 05B6+,./-53 ,03 675 OJ;5Q 53E5 27,+E5 /02+5,454@ S02+5,4/0E 675 DY ,H*;5 d@e> 2*8D.565 +58*;,. *< Y_ /*04 *0 675 1/JTY ,03 ".JTY E+*BD4> =7/27 /4 8,C/8/-54 675 OJ;5Q 53E5 27,+E5@ 1*/. TU /4 4*B+25 *< DY 35D503506 27,+E5 =/67 675 3/44*2/,:*0 *< Y _ <+*8 2,+H*C9./2 ,2/34 ,03 D750*./2 ,2/34 E+*BD4@ "4 DY /02+5,454> 4*85 *< 67545 /*0 Y_ 05B6+,./-5 ,03 /02+5,4/0E 675 OJ;5Q 4B+<,25 27,+E5@
1:1-type silicate clay
Adjoining sheet
'K'> /03/2,65M ' 1/./2*0 656+,753+,. ,03 ' ,.B8/0/B8 *26,753+,. 47556 O<*+ 5,27 .,95+Q@ • fC,8D.5K R,*./0/65> !"##$%&'()* ,"-.'() ,03 /'-0'()1 • G75 6=* 69D54 *< 47556 ,+5 :E76.9 75.3 6*E5675+ H52,B45 675 ,D/2,. T ,6*8 /0 5,27 656+,753+*0 ,.4* <*+84 675 H*F*8 2*+05+ *< *05 *+ 8*+5 *26,753+*04 /0 675 ,3]*/0/0E 47556@ •
1:1-type silicate clay Layer 1
Y93+*C9. D.,05 /4 5CD*453K ! +58*;,.[,33/:*0,. *< Y_ 2,0 D+*3B25 _ *+ ^ 27,+E54 35D503/0E *0 675 4*/. DY@ ! ".4* H/034 =/67 ,0/*04@ •
g750 675 475564 ,+5 46,2N53 *0 6*D *< *05 ,0*675+> 675 ,3],2506 .,95+4 ,+5 H*B03 6*E5675+ H9 793+*E50 H*03/0E@ • 16+*0E 793+*E50 H*03/0E +54B.64 0* 4=5../0E /0 N,*./0/654 O0*0J5CD,03/0E Layer 2 Hydrogen bonding ,3],2506 .,95+Q@ • R,*./0/65 5C7/H/6 .544 D.,4:2/69> 4:2N/0544> 2*754/*0> 47+/0N,E5> 4=5../0E ,03 7*.3 G75 TYJ *< 675 *26,753+,. 475564 /0 .544 =,65+ 67,0 *675+ 2.,94@ .,95+ & ,+5 ,3],2506 6* 675 H,4,. T J *< 675 656+,753+,. 47556 *< .,95+ '> =7/27 • 'K' 2.,94 ,+5 5,49 6* 2B.:;,65 <*+ <*+8 793+*E50 H*03/0E H56=550 67545 ,E+/2B.6B+5 ,03 4B/6,H.5 <*+ +*,3H53 ,03 6=* .,95+4 O,6 /065+.,95+Q@ HB/.3/0E <*B03,:*04@ •
2:1-type silicate clay (expanding) f,27 .,95+ 2*06,/04 ' *26,753+,. 47556 4,03=/2753 H56=550 & 656+,753+,. 475564
+ 5 9 , . + 5 6 0 S
2:1-type silicate clay (expanding: Smectite group ) 1852:654 7;5 , &K' 46+B26B+5 67,6 5CD*454 , .,95+ *< T ,6*84 ,6 H*67 675 6*D ,03 H*F*8 D.,05 67,6 2*06+/HB654 6* 675 .**45.9 H*B03 ,6 /065+.,95+ O;5+9 =5,N TKT ,03 TK2,:*0 ./0N,E5 H56=550 & .,95+4Q@ • L*88*0 4852:65K U*068*+/..*0/65@ • S065+.,95+ 5CD,04/*0 *22B+4 ,4 Y&T h..4 4D,254 H56=550 .,95+ /0 3+9 2.,9@ • Y,;5 , 7/E7 ,8*B06 *< 05E,:;5 27,+E5 3B5 6* )%';'0#2':% %:M%H/:H'.K – UE&_ *i50 +5D.,254 ".a_ /0 675 *26,753+,. 47556 O+5<5+ 6* 675 05C6 hEB+5Q – ".a_ 4*85:854 +5D.,254 1/`_ /0 675 656+,753+,. 47556 •
?=FN 9*ON
".a_ /0 675 *26,753+,. 47556
-
?=FN 9*ON
".a_ 2*85 *B6 <+*8 2*..*/3> a ^;5 27,+E5 ,6 5C27,0E5 4/65
?=FN
-
9*ON
2:1-type silicate clay (expanding: Vermiculite group )
j5+9 7/E7 05E,:;5 27,+E5> 3B5 6* <+5bB506 4BH4:6B:*0 *< 1/`_ /*04 =/67 ".a_ /0 675 656+,753+,. 475564 O)%';'0#2':% %:M%H/:H'.Q@ • LfL /4 7/E75+ /0 ;5+8/2B../654 67,0 /0 ,09 *675+ 2.,9@ • 1=5../0E *22B+4> HB6 .544 67,0 /0 4852:654 3B5 6* 46+*0E.9 ,34*+H53 Y&T 8*.52B.54> ".J793+*C9. /*04 ,03 2,:*04> =7/27 ,26 8*+5 ,4 H+/3E54 67,0 =53E54@ •
9*ON -)6N
1/`_ /0 675 656+,753+,. 47556
--
9*ON -)6N
1/`_ 2*85 *B6 <+*8 2*..*/3> ` ^;5 27,+E5 ,6 5C27,0E5 4/65
9*ON
-
-)6N
2:1-type silicate clay (non-expanding) FB4"#$ %)*)+1/$ +*1" =0':#
-/0:+/:0$
?)+1 > K**)/$
L2*'0)/
%$G56+,753+,. T26,753+,. G56+,753+,.
G56+,753+,. T26,753+,. G56+,753+,.
G56+,753+,. T26,753+,. G56+,753+,.
K+
Y93+*C/35 G56+,753+,. T26,753+,. G56+,753+,.
-':0+$ '( +210=$
1BH4:6B:*0 *< 1/`_ =/67 ".a_ /0 656+,753+,. 475564
1BH4:6B:*0 *< 1/`_ =/67 ".a_ /0 656+,753+,. 475564
L1H'. ). '+/12$,01* %2$$/%
".
P5 ,03 UE
K./$0*1"$0 %2$$/
G75 4/-5 *< R_ 2,0 h6 /0 H56=550 .,95+4
UEJ*26,753+,. 793+*C/35 475564 /4 4,03=/2753 /0 H56=550 ,3],2506 &K' .,95+4@
16+*0E
16+*0E =/67 YKT H/03/0E
!2$ 1,P1+$./ %2$$/ M).,).=
2:1-type silicate clay (non-expanding: Mica group) f,27 .,95+ 2*06,/04 ' *26,753+,. 47556 4,03=/2753 H56=550 & 656+,753+,. 475564
+ 5 9 , . + 5 6 0 S
R_ /*04 ,+5 :E76.9 75.3 H56=550 .,95+4> 67,6 D+5;506 675 8*;58506 *< =,65+ ,03 2,:*04 /06* 675 4D,25 H56=550 .,95+4@
Nonsilicate colloids (Iron and Aluminium Oxides) • Octahedral sheets: Fe 2+ or Al3+ in the cation positions. • No tetrahedral sheets and no Si. • Lack of isomorphous substitution (little –ve charge) • Small charge (+ or -) due to removal or addition of H + from surface hydroxyl groups. • Non-expansive and relatively little stickness, plasticity and cation absorption. • E.g: gibbsite, goethite, ferrihydrite and hematite.
Structure of gibbsite, an aluminum oxide. Consists of dioctahedral sheets (two octahedral) that are H-H bonded.
Humus (organic matter) • •
• •
•
)*0J2+96,../05 *+E,0/2 4BH46,025@ L*04/464 *< ;5+9 .,+E5 *+E,0/2 8*.52B.54 =/67 E505+,. 2758/2,. 2*8D*4/:*0K `eJkel L> aeJ%el T> aJdl Y ,03 'J%l )@ "26B,. 46+B26B+5 *< 7B8B4 2*..*/34 /4 ;5+9 3/m2B.6@ J;5 *+ _;5 27,+E54 O.,+E5 ^;5 4/654Q /4 35;5.*D ,4 Y_ /*0 ,+5 5/675+ .*46 *+ E,/053 <+*8K – L,+H*C9. E+*BD LTTY – W750*./2 793+*C9. E+*BD – ".2*7*./2 793+*C9. E+*BD YB8B4 2,0 ,34*+H .,+E5 ,8*B064 *< =,65+ 3B5 6* /64 E+5,6 4B+<,25 ,+5, ,03 " D*44/H.5 46+B26B+5 *< 7B8/2 ,2/3> D+/8,+9
Cation exchange capacity (CEC) •
• • •
•
LfL /4 675 /065+27,0E5 H56=550 , 2,:*0 /0 4*.B:*0 ,03 ,0*675+ 2,:*0 *0 675 4B+<,25 *< ,09 05E,:;5.9 27,+E53 8,65+/,. 4B27 ,4 2.,9 *+ *+E,0/2 8,F5+@ S6 85,4B+5 675 ,H/./69 *< 675 4*/. 6* 7*.3 *06* 0B6+/5064 ,03 D+5;506 6758 <+*8 .5,27/0E H59*03 675 +**64@ G75 8*+5 2,:*0 5C27,0E5 2,D,2/69 , 4*/. 7,4> 675 8*+5 ./N5.9 675 4*/. =/.. 7,;5 , 7/E75+ <5+:./69 .5;5.@ G75 2,:*0 5C27,0E5 2,D,2/69 *< , 4*/. /4 4/8D.9 , 85,4B+5 *< 675 bB,0:69 *< 4/654 *0 4*/. 4B+<,254 67,6 2,0 +56,/0 D*4/:;5.9 27,+E53 /*04 H9 5.526+*46,:2 <*+254@ L,:*04 +56,/053 5.526+*46,:2,..9 ,+5 5,4/.9 5C27,0E5,H.5 =/67 *675+ 2,:*04 /0 675 4*/. 4*.B:*0 ,03 ,+5 67B4 +5,3/.9 ,;,/.,H.5 <*+ D.,06 BD6,N5@
Quantifying CEC and AEC 1*/. LfL +5D+545064 675 6*6,. bB,0:69 *< OJQ 4B+<,25 27,+E5 *0 675 8/05+,.4 ,03 TU ,;,/.,H.5 6* ,F+,26 2,:*04 /0 4*.B:*0@ • LfL /4 5CD+54453 ,4 8/./5bB/;,.5064 *< OJQ 27,+E5 D5+ 'ee E *< *;50 3+/53 4*/. O85b['ee EQ *+ 28*. 2[NE@ • ' 8*.5 n k C 'e &a ,6*84> 8*.52B.54> /*04 *+ 2*8D*B034 • fbB/;,.506 =5/E76 [O5b@Q =6 K 8,44 OE+,84Q *< , 4BH46,025 O2,:*0> ,0/*0 *+ 2*8D*B03Q 67,6 =/.. +5,26 =/67 ' E *< Y_ *+ ' 8*.5 Ok C 'e &aQ *< 27,+E54 OE[5bQ@ •
"6*8/2 =5/E76 n E[ k C 'e &a /*04 *+ 8*.52B.54 fbB/;,.506 =5/E76 n E[ k C 'e&a OJQ *+ O_Q 27,+E54 n E[8*.5 27,+E5 n E[5b
' 8*.5 R_ /*04
n k C 'e&a R_ /*04 n k C 'e&a *+ ' 8*.5 O_Q 27,+E54 ,6*8/2 =5/E76 *< R_ n ao E[8*.5 R _ /*04 5bB/;,.506O5bQ =5/E76 *< R_ n ao E[8*.5 O_Q 27,+E54 *+ ao E[5b ' 8*.5 L,&_ /*04
,6*8/2 =5/E76 *< L,&_ 5b@ =5/E76 *< L,&_
n k C 'e&a L,&_ /*04 n& C Ok C 'e &aQ O_Q 27,+E54 n & 8*.5 O_Q 27,+E54 n `e E[8*.5 L, &_/*04 n `e E[& 8*.5 O_Q 27,+E54 n &e E[' 8*.5 O_Q 27,+E5 n &e E[5b g7,6 /4 5b@ =6 *< ".a_ O&d E[8*.5Qp
G75 4*/. LfL /4 46+*0E.9 ,I52653 H9 675 0,6B+5 ,03 ,8*B06 *< 2.,9 8/05+,.4 ,03 TU D+54506 /0 4*/.K • &K' 8/05+,.4 q'K' 8/05+,.4 • Y/E7 4,03 ,03 TU 4*/.4 q 4,039 ,03 .*= TU 4*/.4 • r q /03/2,65 2*06506 8*+5 LfL
•
•
G9D/2,. LfL ;,.B54 <*+ 3/I5+506 4*/. 65C6B+54K -')* /$D/:0$
?$R>4SS =
1,034 O./E76 2*.*+53Q 1,034 O3,+N 2*.*+53Q s*,84 1/.6 .*,84 L.,9 ,03 2.,9 .*,84 T+E,0/2 4*/.4
aJ% 'eJ&e 'eJ'% '%J&% &eJ%e %eJ'ee
•
W+/02/D,.[D+53*8/0,06 2,:*04 * Y_> L,_&> UE_& ,03 R_ – )5B6+,. *+ H,4/2 4*/.4K L, _&> UE_&> R_ ,03 ),_
•
G75 46+50E67 *< 2,:*0 ,34*+D:*0 O.9*6+*D/2 45+/54Q /4 35D5034 *0K – L,:*0 27,+E5 O" 27,+E5> " ,34*+D:*0 46+50E67Q – S< 4/8/.,+ 27,+E5> 3565+8/053 H9 675 4/-5 *+ +,3// *< 793+,653 2,:*04 O# 4/-5[+,3//> " ,34*+D:*0 46+50E67Q
"._a q rY_ q L,_& q UE_& q R_ n )Y`_ q ),_ rY_ /4 B0/bB5 H52,B45 *< /64 ;5+9 48,.. 4/-5 ,03 7/E7 27,+E5 3504/69> 67B4> /64 ,34*+D:*0 46+50E67 H56=550 "._a ,03 L,_&@
Determination of CEC " 2*0;50:*0,. 8567*3 6* 3565+8/05 LfL ;,.B5K )Y`T"2 O,88*0/B8 ,256,65Q 8567*3 HBI5+53 ,6 DY d@e H9 .5,27/0E 8567*3@ • g750 4*/. 4,8D.5 /4 5C6+,2653 =/67 ' ) )Y`T"2> 675 5C27,0E5,H.5 2,:*04 ,+5 +5D.,253 H9 )Y`_ ,03 LfL H52*85 4,6B+,653 =/67 )Y`_@ • G750> 3/I5+506 4,.6 O5EM R&1T`Q /4 055353 6* +5D.,25 )Y `_@ G75 .5,27,65 2*06,/0/0E 675 )Y`_ /4 , 85,4B+5 *< 675 LfL@ •
') )Y`T"2
A,45 2,:*0 ,6 675 5C27,0E5,H.5 4/654 s5,27,65 2*06,/0/0E H,45 4,6B+,:*0
Determination of CEC
Saturated the soil with NH +
Measure exchangeable
Leach NH4+ with K+
Measure CEC (NH4+)
Base saturation (BS) •
A,45 4,6B+,:*0 OlA1QK 675 D5+2506,E5 *< 6*6,. LfL *22BD/53 H9 L,&_> UE&_> R_ ,03 ),_@
•
A,45 4,6B+,:*0K O6*6,. H,454[LfLQ C 'ee
• " lA1> " 675 ,;,/.,H/./69 *< L,&_> UE&_ ,03 R_ 6* D.,06@ • " 4*/. DY> " lA1>
Anion exchange (AEC) • • • • • •
"0/*0 5C27,0E5K ,0/*04 /0 4*/. 4*.B:*04 67,6 ,34*+H53 6* O_Q 27,+E5 4/654 *0 2.,9 8/05+,. 4B+<,254 ,03 TU@ G75 O_Q 27,+E54 ,+5 *0 675 8/05+,. 53E54 ,03 TU@ "0/*0 5C27,0E5 ,.4* *22B+ =/67 TY E+*BD *0 675 793+*C9. 4B+<,25 *< N,*./0/65@ Z/4D.,258506 *< TY /*04 *0 793+*B4 P5 ,03 ". *C/354 D,+:2B.,+.9 /0 7/E7.9 =5,675+53 4*/.4 *< 675 6+*D/24 ,03 4BH6+*D/24@ "fL "> ,4 4*/. DY #@ "fL /0 ,2/3 4*/.4 7/E7 /0 'K' 2.,9 q &K' 2.,9
Y&WT`J q 1T`&J q )TaJ q L.J
Acid and base concept • •
"2/3K " 8*.52B.5 67,6 3*0,654 Y_ 6* 4*85 *675+ 8*.52B.5 /0 =,65+@ A,45K " 8*.52B.5 67,6 ,225D64 Y_ /0 =,65+@ H2O ! H+ + OH-
(weak acid, donate H +)
"F,2754 6* ,0*675+ Y&T 8*.52B.5
H2O + H+ ! H3O+ (weak base, accept H +)
16+*0E ,2/3K 'eel *< 3/44*2/,:*0 *< ,2/3 =750 ,3353 6* =,65+@ • g5,N ,2/3K 'l *+ 4./E76 3/44*2/,:*0 *< ,2/3 =750 ,3353 6* =,65+@ •
HCl ! H+ + Cl- (Strong acid, 100% dissociation) CH3COOH ! CH3COO- (Weak acid, 1% dissociation)
Soil pH
1*/. DYK 3565+8/0,:*0 *< /*0 793+*E50 OY_Q 2*02506+,:*0[,2:;/69 /0 4*/. 494658 • S6 /4 05E,:;5 .*E,+/678 *< 675 ,2:;5 Y_ /0 4*.B:*0@ •
#A n J .*E tY_u
n .*E '[tY_u •
TANNU '( #:0$ TA U '( #:0$ Q1/$0 V Q1/$0 V SXSSSSSS4 4 D 4S
DY *< DB+5 =,65+K DY
n J.*E tY_u n J .*E t' C 'eJdu n J OJdQ .*E t' C 'eu n d .*E 'e ndC' nd
v
n .*E t'[tY_u n .*E t'[t' C 'eJdu n .*E 'ed n d .*E 'e ndC' nd
Soil pH •
G75 DY 42,.54 +,0E54 <+*8 e 6* '` =/67 d ,4 675 05B6+,. D*/06K TANU D T7A
•
"6 DY d> 675 Y_ 2*02506+,:*0 /4 5bB,. 6* TYJ K TANU V T7A
•
G75 Y_ 2*02506+,:*0 7,4 , 650<*.3 27,0E5 H56=550 5,27 =7*.5 DY 0B8H5+> 67B4 , 4*/. *< DY % 7,4 'ee :854 8*+5 Y_ /0 4*.B:*0 67,0 , 4*/. =/67 , DY *< d@
Classification of soil acidity
The sources of Hydrogen ion/acidic in the tropic soil
V"68*4D75+5[D+52/D/6,:*0 Xs5,27/0E wTC/3,:*0 *< D9+/65 xTC/3,:*0 *< 2*885+2/,. <5+:./-5+4 yTC/3,:*0 /0 2758/2,.4 O1B.D7B+Q zcD6,N5 *< 0B6+/5064 H9 D.,064 {fC27,0E5 *< 0B6+/5064 3B+/0E 0B6+/5064 BD6,N5 OY _ /*04Q |Z52*8D*4/:*0 *< TU }Z52*8D*4/:*0 *< TU ,03 +**6 +54D/+,:*0 OLT &Q
Influence of pH on nutrient availability and microbial activity •
1*/. DY 7,4 4/E0/h2,06 5I526 *0 4*/. 2758/2,. D+*D5+:54 ,03 H/*.*E/2,. ,2:;/:54@
S0 ,2/3/2 4*/. O.*= 4*/. DYQK $ # 8,2+*0B6+/5064 O)> W> R> L,> UE ,03 1Q@ $ " 8/2+*0B6+/5064 O P5> U0> ~0> LB ,03 L*Q •
S0 4./E76.9 6* 8*35+,65.9 ,.N,./05K $ " 8,2+*0B6+/5064 O5C25D6 WQ ,03 U*@ $ # 8/2+*0B6+/5064 OP5> U0> ~0> LB ,03 L*Q •
•
A,265+/, ,03 ,2:0*8925654
1*/. DY
Buffering capacity (BC)
ABI5+/0E 2,D,2/69K /4 675 ,H/./69 *+ 2,D,2/69 *< 4*/. 6* +54BDD.9 ,0 /*0 6* 675 4*/. 4*.B:*0@ • S6 85,4B+5 675 2,D,2/69 *< 4*/. 6* 8,/06,/0 675 2*02506+,:*0 *< 0B6+/5064 /0 4*/.@ • P*+ 5C,8D.5K g750 D.,06 +**6 ,H4*+H4 0B6+/5064 4B27 ,4 R_ <+*8 675 4*/. 4*.B:*0> 675 R_ /0 675 4*/. 4*.B:*0 =/.. 352+5,453@ G75 8/05+,. 4*/.4 +54BDD.9 675 R_ 6* 675 4*/. 4*.B:*0 <+*8 675 5C27,0E5,H.5 6* 8,/06,/0 675 R_ 2*02506+,:*0 /0 4*/. 4*.B:*0@ •
• " LfL> TU> ,03 *675+ 4*./3 2*04:6B5064> " AL@
"4 LfL /02+5,454 =/67 /02+5,4/0E 2.,9 2*06506> 675+5<*+5> AL /0 h05J 65C6B+53 4*/. q AL /0 2*,+453J65C6B+5 4*/.@ • AL /4 ;5+9 /8D*+6,06 4*/. D+*D5+:54 67,6 46+*0E.9 /0•B50254 0B6+/506 ,;,/.,H/./69@ •
Buffering capacity (BC) •
S8D*+6,06 *< HBI5+/0E 2,D,2/69K V G* 504B+5 +5,4*0,H.5 46,H/./69 /0 675 4*/. DY ! W+5;506 3+,4:2 27,0E54 *< 4*/. DY =7/27 7,;5 4/E0/h2,06 5I526 6* 7/E75+ D.,064 ,03 4*/. *+E,0/484 ! fC,8D.5K ,2/3 +,/0 X S0•B50254 675 ,8*B064 *< ,850385064 O./85 *+ 4B.D7B+ +5bB/+53 6* 5I526 675 354/+53 27,0E5 /0 4*/. DYQ
•
WA1 ,6 ,+*B03 %el /4 2*04/35+53 E**3 <*+ 8*46 4*/.4@
Determination of soil pH: Dye method
Determination of soil pH: Electrometric method
Methods of increasing or decreasing soil acidity •
S02+5,4/0E 4*/. ,2/3/69K – "2/3 TU – S0*+E,0/2 2758/2,. O5@E@M P5++*B4 4B.D7,65Q
•
Z52+5,4/0E 4*/. ,2/3/69K – s/8/0E 8,65+/,.4 4B27 ,4K • L,+H*0,65 <*+84 O5@E@M ./8546*05 67,6 2*06,/0 2,.2/65 OL,LTaQ ,03 3*.*8/65 tL,UEOLTaQ&uQ • TC/35 ,03 793+*C/35 <*+84K /@ L,.2/B8 *C/35 OL,TQ ! R0*=0 ,4 bB/2N./85[HB+053 ./85 ! W+*3B25 H9 75,:0E ./8546*05 O2,.2/65 *+ 3*.*8/65Q ,6 €%e*L ,03 +5.5,453 LT& //@ L,.2/B8 793+*C/35 tL,OTYQ&u ! R0*=0 ,4 793+,653 ./85 ! W+*3B253 H9 ,33/0E 7*6 =,65+
Lime requirement •
s/8/0E 8,65+/,. /4 ,3353 6* 4*/. /0 *+35+ 6* 352+5,45 675 4*/. ,2/3/69@
•
s/8/0E /4 , D+*2544 *< ,.65+/0E 4*/. DY 6* .5;5.4 67,6 ,+5 4B/6,H.5 <*+ D.,064@
• GZ$+/ '( *);$ '. %')* #0'#$0H$% K
/@
L,&_ ,03 UE&_
),_
W794/2,. • S8D+*;5 4*/. ,EE+5E,654
),_ ,6 4*/. 5C27,0E5 4/654
L,&_ ,03 UE&_ <+*8 ./8/0E 8,65+/,.4
L,&_ ,03 UE&_ <+*8 ./85 +5D.,253 675 ),_ ,6 5C27,0E5 4/65 ,03 ,F+,26 4*/. D,+:2.54
Lime requirement
//@ L758/2,. • S02+5,45 4*/. DY • +53B25 ". ,03 U0 6*C/2/69 • S02+5,45 675 0B6+/5064 ,;,/.,H/./69 ///@ A/*.*E/2,. U*46 4*/. *+E,0/484 ,+5 • 8*+5 ,2:;5 =/67 /02+5,45 4*/. DY
Lime requirement
?1+0'.:/0)$./% C'.<;).$01*
[0);10"
U*46.9 <+*8 ,/+ ,03 =,65+
L,+H*0 OLQ OLT&Q
-$+'.,10"
?)+0'.:/0)$./%
U*46.9 <+*8 4*/.
)/6+*E50 O)Q O)Y`_> )TaJQ
L,.2/B8 OL,Q OL,&_Q
Y93+*E50 OYQ OY_> TYJ> Y&TQ
W7*4D7*+B4 OWQ OY&WT`J> YWT`&JQ
U,E054/B8 OUEQ OUE&_Q
TC9E50 OTQ OT&Q
W*6,44/B8 ORQ OR_Q
1B.D7B+ O1Q O1T`&JQ
S+*0 OP5Q OP5&_> P5a_Q U,0E,0545 OU0Q OU0&_> U0`_Q A*+*0 OAQ OYaATa> ATaJ> A`Td&JQ ~/02 O~0Q O~0&_Q L*DD5+ OLBQ OLB&_Q U*.9H350B8 OU*Q OU*T`&JQ L7.*+/05 OL.Q OL.JQ )/2N.5 O)/Q
Movement of ions from soils to roots
4 F
O
Root interception •
$**6 /065+25D:*0K 5C27,0E5 *< /*04 67+*BE7 D794/2,. 2*06,26 H56=550 675 +**6 ,03 8/05+,. 4B+<,254@
•
S*04 *0 675 +**6 4B+<,25 O5@E@ Y_Q ! S*04 *0 2.,94 ,03 TU 4B+<,25@
•
/*04 ,34*+H53 *+ 675 4B+<,25 *< +**6 25..4 ,03 2.,9 D,+:2.54 ,+5 0*6 75.3 :E76.9 HB6 '%+)**1/$ =/67/0 48,.. ;*.B85 *< 4D,25@
•
S< 675 +**64 ,03 2.,9 D,+:2.54 ,+5 /0 2.*45 2*06,26 =/67 5,27 *675+> 675 *42/..,:*0 ;*.B85 *< /*04 ,34*+H53 *0 +**6 4B+<,25 8,9 *;5+ H9 675 *42/..,:*0 ;*.B85 *< /*04 ,34*+H53 *0 2.,9 D,+:2.54> ,03 675 /*04 ,34*+H53 *0 2.,9 D,+:2.5 8,9 H5 5C27,0E53 =/67 675 /*04 ,34*+H53 *0 +**6 4B+<,25 3/+526.9 =/67*B6 h+46 H5/0E 3/44*.;53 /0 4*/. 4*.B:*0@
Root interception T42/..,:*0 ;*.B85
/ ' ' \
AN
EN
9 , . L
G75 /*04 75.3 H9 5.526+*46,:2 <*+254 ,6 67545 4/654 *42/..,65 =/67/0 , 25+6,/0 ;*.B85@
/ ' ' \
EN
AN
9 , . L
g750 675 *42/..,:*0 ;*.B854 *< 6=* /*04 OY_ ,03 R_Q *;5+.,D> /*0 5C27,0E5 *22B+@
Root interception • Root interception can be enhanced by mycorrhiza which colonization is favor under conditions of slightly acidic soil pH, low P, adequate N and low temperature.
g/67*B6 2%-$..!'3"
g/67 2%-$..!'3"
Mass flow U,44 •*=K U*;/0E *< 3/44*.;53 0B6+/5064 /0 •*=/0E 4*/. 4*.B:*0 6*=,+34 675 +**64 • S6 *22B+4 =750 /*04 /0 4*/. 4*.B:*0 ,+5 6+,04D*+653 6* 675 +**6 ,4 , +54B.6 *
C N a O 2 3 + N - C O a2 3 -
+