Ef fect of pond ash on ground water quality: a case
study
I.V. Suresh
Disaste r Manage me nt Institute (DMI), Paryavaran Parisar, Bho pal, India
C. Padmakar, Prabha Padmakaran, M .V.R.L. M urthy, C.B. Raju and R.N. Yadava
Re gio nal Re se arc h Labo rato ry (CSIR), Bho pal, India
K. Venkata Rao
Vijayawada The rmal Po we r Statio n (VTPS), Ibrahimpatnam, India
The potential problems and
their consequences due to fl y
ash disposal have been well
studied around the world. Ash
pond is a common available
disposal facility for thermal
power plants. The pond ash is
subjected to weathering and
the ions present in ash
migrate to the soil and subsequently to the ground water
over a period of time. A study
has been carried out at
Vijayawada Thermal Power
Station (VTPS), Andhra
Pradesh, India, to monitor the
ground water quality in order
to determine the potential
impact of ash ponds. It has
been found that ground water
quality is deteriorated due to
the presence of fl y ash ions
(macro and micro such as Fe,
Ca, Mg etc.) which were
leached out from the ash up
to some extent. The contamination is likely to increase in
the case of toxic and other
ions with the passage of time.
The presence of vegetative
cover and plant growth on the
down stream slope and fl y
ash ponds which are covered
by soil may effectively control
the leaching of ions.
Enviro nme ntal Manage me nt
and He alth
9 / 5 [ 1998] 2 0 0 –2 0 8
© MCB Unive rsity Pre ss
[ ISSN 0956-6163]
[ 200 ]
Introduction
F ly a sh is pr odu ced a s a r esu lt of coa l com bu stion in th er m a l power pla n ts a n d
disch a r ged in a sh pon ds. In th er m a l power
pla n t boiler s, th e in or ga n ic m in er a l con ten t
of coa l is con ver ted in to a m or ph ou s gla ssy
m a ter ia l du e to com bu stion of coa l a t 1,3001,350°C a n d devitr ified a s a r esu lt of h igh
viscosity. Cu r r en tly, m or e th a n 60 m illion
ton n es of a sh per a n n u m a r e pr odu ced fr om
differ en t th er m a l power sta tion s in In dia ,
wh ich w ill tou ch th e figu r e of 100 m illion
ton n es by th e n ext cen tu r y. Th e pr edom in a n t
m eth ods for fly a sh disposa l in developin g
cou n tr ies a r e a sh settlin g ta n k s, du m pin g or
dir ect disposa l in loca l w a ter w ays. Th ese
pon d w a ter s con ta in m a n y solu ble ca tion s/
a n ion s th a t a r e r elea sed fr om th e gla ss m a tr ix
of th e a sh . After settlin g, w a ter w ith its
h igh er qu a n tity of tota l dissolved solids (TDS)
m ay eith er en ter in to r iver or str ea m or
pa r tly seep in to th e gr ou n d w a ter.
It h a s been r epor ted by Ma lek et a l. (1983)
th a t fly a sh con ta in s h igh er con cen tr a tion s of
B, Co, Cr, Cd, Mo, N i, As, a n d Se th a n
n or m a lly fou n d in soils. Th e m ost en vir on m en ta l con cer n com es fr om th e a bove a for esa id h eavy m eta ls in fly a sh . Th e lea ch in g
poten tia l of th ese h eavy m eta ls fr om a n open
system (fly a sh pon ds) is expected to be
gr ea ter du e to diu r n a l a n d sea son a l va r ia tion s in tem per a tu r e, m oistu r e con ten t, a n d
oth er pa r a m eter s.
Sin ce a ll th e m eta ls of fly a sh a r e in th e
pr ior ity pollu ta n ts list (USE PA, 1993), th eir
su ita bility a n d lea ch in g poten tia ls w ill be
expected to be h igh . It h a s been deter m in ed
by Ru ssel (1981) th a t lon gter m lea ch in g of fly
a sh u sin g low pH w a ter r elea sed su bsta n tia l
a m ou n ts of N a , K, Al, S, As, Mo, Se, a n d V in to
th e solu tion ph a se. Oth er stu dies by N a tu sch
et a l. (1975) in dica te th a t N a , S04, As, Se, Mo,
Cr, a n d P b levels wer e h igh er in fly a sh
a ffected gr ou n d w a ter th a n in sa m ples fr om
u n a ffected a r ea s.
Ou t of m a n y types of pa r ticles pr esen t in
a sh , th e gla ss-lik e pa r ticles a r e r ela tively
in solu ble in w a ter. Bu t, th e en r ich ed su r fa ce
elem en ts on th ese pa r ticles is solu ble a n d
h en ce ava ila ble to th e en vir on m en t on lea ch in g. Toxicity stu dies su ggest th a t th r ou gh
lea ch in g fl y a sh m ay a dver sely a ffect w a ter
ecosystem s, wh ile th e solid m a ter ia ls em itted
to th e a tm osph er e m ay be h a za r dou s to
ter r estr ia l ecosystem s by dir ect exter n a l
r ea ction s (sk in , eyes etc.) or by r ea ction s in
th e r espir a tor y tr a ct.
In th e developed n a tion s su ch a s USA, th e
gr ou n d w a ter qu a lity m a ps a r e r ecor ded fr om
tim e to tim e a n d well m a in ta in ed to k eep a
close w a tch on th e w a ter qu a lity in or der to
en for ce en vir on m en ta l pr otection law s
(Ch u gh , 1996). ln th e pr esen t stu dy it h a s been
pr oposed th a t it is ver y a ppr opr ia te to in itia te
sim ila r stu dies in a ll th er m a l power sta tion s
th r ou gh ou t In dia to k eep a ch eck on gr ou n d
w a ter qu a lity to fu lfil th e r equ ir em en ts of
en vir on m en ta l pr otection law s.
Study area
Th e Vijayaw a da Th er m a l Power Sta tion
(VTP S) is loca ted a t Ibr a h im pa tn a m , 16Km
aw ay fr om th e Ra ilw ay city, ca lled
Vijayaw a da , An dh r a P r a desh , In dia . VTP S
a sh pon d site togeth er w ith 13 sa m plin g sta tion s a r e pr esen ted in F igu r e 1.
M ethods and materials
Th e fly a sh u n der stu dy w a s collected fr om
th e a sh pon d of Vijayaw a da Th er m a l Power
Sta tion , Vijayaw a da (VTP S). Soil a n d gr ou n d
w a ter sa m ples wer e collected fr om differ en t
loca tion s cover in g a bou t 10k m s fr om th e a sh
pon d of VTP S. Ch em ica l con stitu en ts of th e
soil, a sh a n d w a ter sa m ples wer e ca r r ied by
well esta blish ed m eth ods u sin g a tom ic
a bsor ption spectr oph otom eter (AAS), dir ect
cu r r en t pla sm a (DCP ) em ission spectr om eter,
a n d fla m e ph otom eter. Wa ter a n a lysis k it w a s
u sed for m ea su r in g pH a n d electr ica l con du ctivity a t th e site. Den sity w a s m ea su r ed by
th e specifi c gr avity bottle m eth od.
Ava ila ble N, P, S a n d exch a n gea ble K in soil
a n d fly a sh sa m ples wer e exa m in ed by th e
sta n da r d m eth ods (J a ck son , 1973; Su bba Ra o,
1993). Ava ila ble Cu , Fe, Zn a n d Mn wer e deter m in ed by th e DTPA (dieth ylen e tr ia m in e
pen ta a cetic a cid) extr a ction m eth od (Gu pta ,
1993; Lin dsay a n d N or vell, 1978). Abou t 10gm
fly a sh w a s sh a k en w ith 20 m l DTPA extr a ctin g solu tion . Th e solu tion w a s fi lter ed a n d th e
con stitu en ts deter m in ed u sin g AAS a n d DCP.
X-r ay pow der diffr a ction a n a lysis w a s
ca r r ied ou t by th e P h illips diffr a ctom eter
m odel 1710 u sin g Cu K r a dia tion a n d n ick el
filter a t 40KV a n d 20m A. Th e iden tifica tion of
m in er a l ph a ses w a s don e w ith th e h elp of
Min er a l Pow der Diffr a ction fi le J CP DS a n d
ASTM diffr a ction da ta . In fr a r ed spectr oph otom eter m odel 984 G of M/ s Per k in -E lm er, UK
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
w a s u sed for m ea su r in g IR spectr a l lin es by
con ven tion a l KBr pellet m eth od.
Results and discussions
Che mic al c o mpo s itio n o f po nd as h
T h e ch em ica l com p osit ion of p on d a s h is
sh ow n in Ta ble I w h ich h a s a lk a lis (N a 2O +
K 2O) in t h e r a n ge of 1.5 – 2.3 w t p er cen t a n d
a lk a lin e r a r e ea r t h ’s (Ca O + MgO) less t h a n
3.0 w t p er cen t (P r a b h a et a l., 1994). T h e
m a jor con st it u en t s a r e SiO 2 (59 – 61 w t % )
a n d a lu m in a (28 – 29 w t % ). Fe 2O 3 d oesn ’t
exceed 5.5 w t % . In a d d it ion t o t h e a b ove,
p on d a sh sa m p les h ave m icr o-n u t r ien t s s u ch
a s Cu , Fe, Zn , Mn a n d m a cr o-n u t r ien t s lik e
ava ila ble n it r ogen (n it r it es), p h osp h or u s,
p ot a ssiu m , sod iu m a n d su lp h u r (Ta ble II).
T h e va lu es in Ta ble II sh ow som e of t h e
Figure 1
Lo c atio n map o f sampling statio ns ne ar ash po nd
Hillocks
HYDRABAD VUAYAWADA
CAPITAL
THERMAL POWER STATION
Fly as h Pond
(About 180 Acres )
10
TRILOCHANAPURAM
N
AGRICULTURAL LAND
7
KOTA MULAPADU
S
8 QUALITY STONE CRUSHER
11
MULAPADU
GUDEM
9
3
NH 9
NH
9
2
J UPUDI EAST
4
J UPUDI
SDA SCHOOL
5
1
6
Table I
Che mic al c o mpo sitio n o f po nd ash sample s o f VTPS (wt%)
LOI
0.50 – 2.50
SiO2
Al2 O3
Fe 2 O3
Na 2 O
K2 O
CaO
M gO
59.0 – 61.0
28.0 – 28.8
2.70 –5.52
0.24 – 0.50
1.26 – 1.76
0.7 – 1.0
1.40 – 1.90
[ 201 ]
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
Table II
Available mac ro -nutrie nts and mic ro -nutrie nts in po nd as sample s o f VTPS
Name of
macro-nutrient
Total
(ppm)
Available N2
– do – P
– do – K
– do – S
155
014
007
040
Name of
micro-nutrient
Total
(wt%)
Available
(ppm)
Cu
Fe
Zn
Mn
0.087 – 0.102
1.90 – 3.8
0.008 – 0.042
0.02 – 0.06
0.40 – 00.76
4.0 – 14.50
0.6 – 20
0.60 – 2.80
– 180
– 045
– 019
– 121
Figure 2
X-ray diffrac tio n patte rns o f fly ash sample s fro m VTPS
Key
– MULLITE
–
QUARTZ
Relative Intens ity (I/I0 )
– MAGNETITE
10
20
30
40
50
60
70
2∅
Figure 3
Infrare d spe c tra o f re pre se ntative fly ash sample s fro m VTPS
tota l m icr o-n u tr ien t s su ch a s Cu , Fe, Zn a n d
Mn wh ich a r e in th e for m of both lea ch a ble
a n d n ot ea sily lea ch a ble ion s r espectively.
Abs orption
495
1092
790
3800
3000
Wave Number (Cm –1 )
[ 202 ]
1900
1100
540
394
300
Mine ralo gy and mic ro -struc ture o f fly ash
F ly a sh con sists of m ostly a m or ph ou s gla ssy
ph a ses of SiO 2 a n d a lu m in o-silica te in th e
poor ly cr ysta llin e m u llite for m . X-r ay pow der
diffr a ction a n a lysis a n d IR spectr oph otom etr y h ave con fir m ed th e pr esen ce of a lph a
qu a r tz a n d m u llite (F igu r e 2 a n d 3). Fe is
pr esen t m ostly in th e for m of Ma gn etite h avin g d(Å) = 2.5 (F igu r e 3). A pa r t of it is in
m olten sta ge a n d for m s a coa tin g on th e su r fa ce of th e a lu m in o-silica te cen o-sph er es
(F igu r e 4). Th e ch a n ces of m olten ir on pr esen t in sph er ica l sh a pe ca n n ot be r u led ou t.
Sca n n in g electr on m icr o-gr a ph s of va r iou s
sa m ples su ggest th e pr esen ce of sph er ica l a n d
n ea r sph er ica l sh a pe pa r ticles w ith h a r dly
a n y cr ysta llin e str u ctu r e or ph a se sepa r a tion
(F igu r e 4).
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
Crystal struc ture
Th e SiO 2 r ich ph a se is cr ysta llin e a n d h a s th e
tetr a h edr a l str u ctu r e a s sh ow n in F igu r e 5.
Th e cr ysta l str u ctu r e of th e sph er ica l pa r ticles ca n be expected to be m ostly disor der ed
beca u se of th e a m or ph ou s n a tu r e of th e m a ter ia l wh ich for m ed a s a r esu lt of su per coolin g
of th e pa r tia lly fu sed silica te/ a lu m in o-silica te pr esen t in th e coa l. Alu m in o- silica te n et-
Figure 4
SEM mic ro graph o f flyash (VTPS)
Si-O-M or Al-O-M; wh er e M – N a , K, B, Ca ,
Mg, Zn , Cu , N i, P b, As.
X-r ay pow der diffr a ction pa tter n (F igu r e 2)
a n d IR spectr a (F igu r e 3) h ave clea r ly sh ow n
th e a bsen ce of ca r bon a tes or spin a l. Hen ce
th e F igu r e 5 a n d 6 r epr esen ts th e tr u e str u ctu r e of fiy a sh .
Weathering of fly ash and its effec t on soil
and ground water in the vic inity of ash pond
It h a s been n oticed th a t pH of pon d a sh va r ies
fr om 7.09 to 8.63, electr ica l con du ctivity
r a n ges fr om 0.017 to 0.036m m h os/ cm , specific
gr avity 1.63 to 1.83 a n d or ga n ic m a tter 0.73 to
1.94 w t% w ith a n in cr ea se in dista n ce u p to
650/ 700 m etr es aw ay fr om th e disposa l poin t
th a t is cover in g th e en tir e br ea dth of th e pon d
(Ta ble III a n d F igu r e 1). It w a s r epor ted
ea r lier th a t th e ch lor ide, su lph a tes, bica r bon a tes, or ga n ic m a tter, w a ter extr a cta ble solids
a n d electr ica l con du ctivity va lu es of fly a sh
a r e decr ea sed pr ogr essively fr om th e su r fa ce
of th e pon d w ith a n in cr ea se in depth of th e
a sh pon d (Ra ju , 1993). Su ch a situ a tion sh ow s
th e possibility of w a ter con ta m in a tion wh en ever th e w a ter ta ble r ises h igh .
Th e test r esu lts of gr ou n d w a ter sa m ples
collected fr om a bou t 13 sta tion s over a dista n ce of 10k m fr om th e a sh pon d of VTP S a r e
given in Ta ble IV. Th e TDS of gr ou n d w a ter
h a s been pr esen ted in F igu r e 7 a s con tou r s.
An a lysis of th ese r esu lts sh ow a n in cr ea se in
th e ca lciu m h a r dn ess (96-298ppm ), tota l h a r dn ess (168-904ppm ), Ma gn esiu m (17-147ppm ),
Cl¯ (56-499ppm ) a n d tota l a lk a lin ity 105-
10 µm
Figure 5
Crystal struc ture ne two rk o f silic a
Figure 6
Crystal struc ture o f alumino silic ate glass in
flyash
Key
: Si
wor k h olds m a n y ca tion s a n d a n ion s in th e
va ca n t spa ces (F igu r e 6). Th e va r iou s ca tion s
lik e N a , K, B, Ca , Mg, Zn , Cu , N i, P b a n d As
a r e a tta ch ed to Si/ Al th r ou gh oxygen “O”. At
th e sa m e tim e, som e of th ese ca tion s occu py
va ca n t spa ces a s sh ow n in th e F igu r e 6.
: O2
Table III
Physic o Che mic al analysis re sults o f po nd ash VTPS
Samples
distance from
disposal point
(meters)
700
650
550
400
300
200
pH
Electrical
conductivity
(mmhos/ cm)
Specific
gravity
Organic
carbon
(wt%)
Organic
matter
(wt%)
8.63
8.54
7.24
7.09
7.10
7.40
0.036
0.032
0.025
0.021
0.017
0.019
1.836
1.755
1.702
1.660
1.630
1.680
0.425
0.461
0.503
0.713
0.754
1.128
0.733
0.794
0.867
1.229
1.229
1.944
Key
∅: M
: Si (or) Al
: O2
[ 203 ]
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
Table IV
Charac te ristic s o f gro und wate r ne ar ash po nd site (VTPS)
Regulatory body
M in.
M ax.
M ean
Desirable
limit
(ppm)
Zn
0.01
Pb
0.01
Fe
0.10
Na
100
K
20
Ca
38.6
Ca hardness 96.6
Total hardness 168
Mg
17.4
Chloride
56.8
Total alkalinity 105
pH
6.5
1.30
0.05
4.20
155
170
129.5
298
904
147
499
533
7.5
0.17
0.03
1.30
122.8
81.18
85.72
214.18
457.45
59.22
270.30
314.2
7.0
5.00
0.05
0.30
–
–
75
300
300
–
250
200
6.5–8.5
Elements
USEPA
(1976)
ES
ISI
(1983)
–
–
–
200
–
200
–
–
125
250
–
6.5–8.0
–
–
–
175
12
–
–
100-500
125
250
–
6.5–8.0
115
NR
1.00
–
–
200
600
600
125
1,000
600
6.5–9.2
Number of
samples
exceeding
limits
Nil
Nil
5
Nil
Nil
Nil
Nil
3
1
Nil
Nil
Notes:
US = US standards; ES = European standards; ISI = Indian standards; NR = no relaxation
533ppm (Ta ble IV). A m a r gin a l r ise in th e
con cen tr a tion of Zn (0.01 to 1.30ppm ) a n d P b
(0.01-0.05ppm ) a r e n oticed. High er va lu es of
Fe u p to 4ppm sh ow th a t th e lea ch a bility of Fe
is a s h igh a s 40 tim es. Th e effect of pon d a sh
on a lk a li ion s N a a n d K in gr ou n d w a ter
a ppea r s to be n ot ver y sign ifica n t (Ta ble IV).
Th is m ay pr oba bly be du e to h igh er ion ic
r a dii of N a a n d K ion s wh ich a r e r ea dily
exch a n ged to th e soil a n d w a ter slu r r y. F r om
th e lea ch in g stu dy of fly a sh a n d ch em ica l
a n a lysis of th is w a ter solu ble m a ter ia l, it h a s
been n oted th a t a ll of th e m a jor elem en ts
pr esen t in th e fly a sh a r e a lso pr esen t in its
w a ter solu ble fr a ction s. Th e a m ou n t of w a ter
solu ble fr a ction s in differ en t a sh es va r ies
sign ifica n tly. Th er e is n o sign ifi ca n t cor r ela tion between th e com position of a sh a n d
w a ter solu ble fr a ction of a sh .
Th e m ovem en t of th e ca tion s Ca a n d Mg
a n d th e tota l h a r dn ess follow a n in cr ea sin g
tr en d a t th e loca tion s in th e or der 5 > 1 > 6
wh er ea s ch lor ide h a ppen s to be a t its m a xim u m va lu e a t th e loca tion -l wh ich m ea n s, Cl¯
Figure 7
Co nto ur plo t o f TDS c o nc e ntratio n
TDS
0.40
4.40
8.40
12.40
16.40
29.20
48.40
29.20
25.23
25.23
21.26
20.40
24.40
28.40
32.40
36.40
40.40
44.40
21.26
8
9
17.29
4
17.29
2
3
13.31
13.31
5
9.34
9.34
1
5.37
5.37
1.40
1.40
0.40
[ 204 ]
4.40
8.40
12.40
16.40
20.40
24.40
28.40
32.40
36.40
40.40
44.40
48.40
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
is m or e loca lized h er e th a n a t loca tion s 5 a n d
6 (F igu r es 8 a n d 9). If we con sider th e loca tion s 7, 4, 3, 9 a n d 8 th er e is a r e gu la r tr en d in
th e pr esen ce of both ca tion s a n d a n ion s (F igu r es 10-11). In gen er a l, loca tion N o. 3 h a s
m a xim u m qu a n tities of ca tion s a n d a n ion s a s
com pa r ed to th e oth er loca tion s. Wh en th e
loca tion s 8, 9 a n d 3 a r e on ly con sider ed it is
seen th er e is a r e gu la r fa ll in th e con cen tr a tion s of Cl¯, Ca , Mg a n d tota l h a r dn ess a s 8 < 9
Figure 8
Mo ve me nt o f mac ro nutrie nts (a)
Concentration (mg/I)
800
600
400
200
0
0
2
4
6
8
10
Sampling points
Key
Ca
T.hardne
Na
K
< 3. Th ese r esu lts a r e sh ow n in F igu r es 6-12
a n d th e m ovem en t of th e ion s h a s som e bea r in g on th eir ion ic r a diu s, ion exch a n ge ca pa city, geologica l ter r a in a n d pH of th e fly a sh .
Th e bigger th e ion ic r a diu s of elem en ts, th e
h igh er is th e r a te of th eir exch a n ge.
Apa r t fr om sligh t solu bility in w a ter, fly a sh
is ch em ica lly ver y sta ble a n d th er e is n o deter ior a tion on exposu r e to th e a tm osph er e.
F u r th er m or e, sin ce th e solu ble con ten t
becom es fi xed by pa r ticipa tion in th e pozzola n ic a ction , w a ter pa ssin g over or th r ou gh
th e a sh is u n lik ely to pick u p sign ifica n t
qu a n tities of a n y com pou n d th a t wou ld lower
th e qu a lity of str ea m or gr ou n d w a ter.
Th e pa r a m eter s th a t gr ea tely a ffect th e
lea ch in g pr ocess a lso in clu de soil textu r e, pH,
pa r ticle size, th e pr esen ce of ch ela tin g a gen ts
in soil, r a tio of fly a sh to th e solu tion ’s
tem per a tu r e, pr esen ce of lea ch a te collection
system s a n d th e or igin of fly a sh .
Exc hange of ions from soil/ fly ash to plants
Con cen tr a tion of solu ble elem en ts in soil
h ave sh ow n a n u pw a r d tr en d by a ddin g m or e
fly a sh to it (P a ge et a l., 1979). It is essen tia lly
du e to th e fa ct th a t th e solu ble fr a ction of
elem en ts com in g fr om fly a sh a r e r ea dily
a bsor bed a n d r eta in ed by th e soil in or der to
en h a n ce gr ow th of pla n ts. Soybea n , la dy’s
fin ger, pea s a n d ben ga l gr a m h ave sh ow n
en cou r a gin g gr ow th r a te in th e fly a sh (30 – 90
w t% ) a m en ded soil (RRL, Bh opa l, 1996). Th e
edible pa r ts of th e th ese pla n ts wer e a n a lyzed
for Fe, Mg, N i, Cu , Zn , N a , K wh ich h ave
sh ow n h igh er u pta k e of th ese ion s wh en com -
–
Cl
Mg
Figure 1 0
Mo ve me nt o f mic ro nutrie nts (a)
Figure 9
Mo ve me nt o f mac ro nutrie nts (b)
Concentration (mg/I)
Concentration (mg/I)
4
500
400
3
300
2
200
1
100
0
0
4
2
6
8
10
0
0
Sampling points
4
2
6
8
10
Sampling points
Key
Ca
T.hard
Na
K
Mg
–
Cl
Key
Zn
Pb
Fe
[ 205 ]
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
pa r ed to th e cr ops gr ow n on con tr ol soil
(Ta ble V). In a ddition to th e h igh er con cen tr a tion of th e a bove ion s in th e edible pa r ts of
th ese pla n ts, th e r a te of u pta k e of th e
elem en ts va r ied fr om pla n t to pla n t. Th is m ay
be du e to m eta bolic r ea ction s a t th e r oots of
th ese pla n ts a n d by con tr ollin g a ssim ila tion
of solu ble elem en ts by pla n ts (Adr ia n o et a l.,
1980). F u r th er, a ddition of m in er a ls su ch a s
Figure 1 1
Mo ve me nt o f mic ro nutrie nts (b)
Concentration (mg/I)
5
4
3
2
1
0
0
4
2
8
6
10
Sampling points
Key
Zn
Pb
Fe
Figure 1 2
Princ ipal c o ntro ls o f fre e me tal c o nc e ntratio ns in so il so lutio ns (adapte d
fro m Mattigo d e t al., 1 9 8 1 )
Mas s Trans fer
Ion
Exchange
and
Ads orption
Precipitation
&
Dis s olution
of Solids
Free Metal
Concentration in
s oil s olution
Redox
Reaction
Acid-Bas e
Reaction
Biological
Reaction
[ 206 ]
Complex
Formation
low gr a de r ock ph osph a te en h a n ced th e
gr ow th pa tter n of pea s a n d oth er pla n ts
ow in g to th e in ter a ction of ph osph a te ion
w ith som e of th ese elem en ts lea din g to a n
in cr ea se in th eir lea ch a bility. Th e a bove stu dies in dica te a possible m eth od of con tr ollin g
th e seepa ge of va r iou s ion s to th e gr ou n d
w a ter by selective ve geta tion a n d system a tic
pla n t gr ow th on a sh pon ds a n d fly a sh
a m en ded soils. Th is exer cise w ill fu r th er
r edu ce th e pollu tion of gr ou n d w a ter.
Th e envir on m en ta l pa th w ays of a ll pollu ta n ts ca n be pr edicted a s a ser ies of even ts.
On ce th e con stitu en ts a r e r elea sed to th e
a qu eou s ph a se, th ey m ay dir ectly be a bsor bed
by pla n t r oots or th ey m ay lea ch to th e su bsu r fa ce. If th ey a r e a bsor bed by th e pla n ts,
th en th ey w ill r em a in fixed u n til th e pla n ts
a r e con su m ed by a n im a ls or decom posed. In
th e la tter ca se th e con stitu ten ts a r e r elea sed
ba ck to th e soil. If th e con stitu en ts a r e
r elea sed in to th e su bsu r fa ce en vir on m en t,
th ey pa r ticipa te in sever a l ch em ica l a n d
h ydr ologic pr ocess. Th e com bin ed effects of
su ch ph ysica l, ch em ica l a n d h ydr odyn a m ic
pr ocesses con tr ibu te to decr ea se th e con cen tr a tion of th e solu tes r elea sed fr om th e w a ste
a s a fu n ction of dista n ce fr om th e poin t of
a pplica tion .
Th e tr a n spor t of pa r ticu la r ch em ica l
species in ter r estr ia l system s is of in ter est to
a va r iety of scien tists (Bower a n d Wilcox,
1965; Cole, 1980), sin ce m ea su r em en t or
r epor tin g of tota l con cen tr a tion of a pa r ticu la r in or ga n ic com pou n d (E n field et a l., 1980)
in th e soil m ay be m islea din g in m a n y en vir on m en ta l m a n a gem en t situ a tion s. Toxic
effects of tr a ce m eta ls m ay be a ffected m or e
by th eir ch em ica l for m th a n by th eir tota l
con cen tr a tion (F lor en s, 1977). Th er efor e
m a th em a tica l m odels ca pa ble of sim u la tin g
th e distr ibu tion of in or ga n ic pollu ta n t
species in soil a n d gr ou n d w a ter system s a r e
va lu a ble tools for a n a lysin g con ta m in a n t
pa th w ays. An eva lu a tion of th e fa te of in or ga n ic com pou n ds in soil a n d gr ou n d w a ter
r equ ir es a deta iled con sider a tion of th e ph ysica l, ch em ica l a n d biologica l pr ocesses a n d
r ea ction s in volved su ch a s com plexa tion ,
a dsor ption , pr ecipita tion , oxida tion -r edu ction (Ma h ier et a l., 1980), ch em ica l specia tion
a n d biologica l r ea ction s (F igu r e 12) to deter m in e th e fr ee m eta l con cen tr a tion in soil
solu tion s. Th ese pr ocesses ca n a ffect su ch
ch a r a cter istics a s species solu bility, ava ila bility for biologica l u pta k e ph ysica l tr a n spor t
a n d cor r osion poten tia l (Lym en et a l., 1982;
P r ick ett et a l., 1981)
E n vir on m en ta l m on itor in g com pr isin g
collection a n d a n a lysis of gr ou n d w a ter, su r fa ce r u n -off, a n d th e lea ch a te a n a lysis of a sh
ta k en fr om w ith in th e a sh pon d sh ow s th a t fl y
I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
Table V
Elemental c onc entration (ppm) in edible portions of c rops grown on pure soil and 9 0 per c ent fly ash
Elements
Soybean
Control
F.A.
Lady’s finger
Control
F.A.
Peas
Control
F.A.
Bengal gram
Control
F.A.
Calcium
M agnesium
Sodium
Potassium
M anganese
Iron
Nickel
Copper
Zinc
900
2,000
3,020
2,500
70
425
10
16
40
1,900
1,820
1,050
4,550
13
175
8
11
32
1,100
1,400
4,500
1,435
30
235
10
19
77
1,500
1,700
1,435
3,100
80
350
8
13
45
850
2,100
3,820
4,850
50
300
21
31
70
2,200
1,850
1,200
4,700
25
200
10
16
37
2,750
2,300
1,800
3,315
23
150
15
13
35
2,700
1,500
3,315
3,750
61
100
21
17
30
Notes:
F.A. = fly ash; Control = soil without flyash
a sh pon d does n ot n ecessa r ily detr im en ta lly
a ffect gr ou n d w a ter con cen tr a tion s. However,
poten tia l im pa ct of fl y a sh pon d on th e loca l
en vir on m en t m ay gen er a lly a r ise ou t of w in d
er osion , su r fa ce w a ter er osion , dissolu tion by
su r fa ce r u n -off, r a in a n d su bsequ en t per cola tion to gr ou n d w a ter. Per cola tion of w a ter
th r ou gh fly a sh pon ds gen er a lly yield h igh
a lk a lin e solu tion (pH: 8-10) th a t w ill r estr ict
h eavy m eta l lea ch in g. Th e con cer n , h en ce,
lies on th e lon gevity of th is su ffer in g con tin u a l r a in fa ll in filtr a tion or gr ou n d w a ter
in tr u sion . Acid extr a ction pr ocedu r es, su ch
a s th e USE PA, E P -toxicity test (sim u la tes th is
lon g-ter m con dition in a n a ggr essive ba tch equ ilibr iu m lea ch in g test) in dica te th a t th e
efflu en t fr om th ese fly a sh pon ds a r e w ill
w ith in lim its a s pr escr ibed by USE PA (1976)
by a t lea st on e or der of m a gn itu de for a ll
m eta ls of con cer n except ir on .
In or der to m in im ize th e occu r r en ces of
su ch en vir on m en ta l pr oblem s w ith str u ctu r a l fly a sh pon d, it is a dvisa ble to r estr ict
th e r a te of w a ter per cola tion by a pr oper ly
design ed dr a in a ge a n d collection system .
Conclusions
• N ea r th e a sh pon d th e gr ou n d w a ter qu a lity
is ch a n ged ow in g to th e lea ch in g of solu ble
ion s pr esen t in fly a sh .
• Addition of fl y a sh to th e n a tive soil lea d to
a n in cr ea se in th e ava ila bility of n u tr ien t
ion s lik e Cu , N i, Zn , Fe, P, K a n d N a a n d
en h a n ced gr ow th of pla n ts.
• E xter n a l er osion du e to w in d, r a in a n d
w ave a ction ca n a lso be con tr olled by a
su ita ble ve geta tive cover on th e
dow n str ea m slope wh ile pr otectin g th e
u pstr ea m slope. Adequ a te spillw ay or r u n off diver sion s m u st be pr ovided a n d w ill be
m a in ta in ed pr oper ly.
• Selection of pa r ticu la r type of pla n ts a n d
th eir pla n n ed gr ow th , wou ld con tr ol th e
m igr a tion of m eta llic ion s to th e gr ou n d
w a ter.
Avoidin g h igh in pu ts of fly a sh in soil a m en dm en t sch em es for better cr op gr ow th a n d
in tr odu ction of m eta bolic m ech a n ism s wou ld
con tr ol th e lea ch a bility of solu ble ion s a n d
r edu ce m igr a tion of va r iou s elem en ts to th e
gr ou n d w a ter.
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I.V. Sure sh, C. Padmakar,
Prabha Padmakaran,
M.V.R.L. Murthy, C.B. Raju,
R.N. Yadava and
K. Ve nkata Rao
Effe c t o f po nd ash o n gro und
wate r quality: a c ase study
Enviro nme ntal Manage me nt
and He alth
9 / 5 [1 9 9 8 ] 2 0 0 –2 0 8
The authors express their
sincere thanks to Professor
T.C. Rao, Director, CSIR, for
his kind permission to publish the work. The authors
are also highly thankful to
the Environmental Engineers
of VTPS for their co-operation and the Central Board
of Irrigation and Power, New
Delhi for fi nancial support of
this project.
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