ManagementofminespoilforcropproductivitywithligniteyashandbiologicalamendmentsL.C.
Rama,*, N.K. Srivastavaa, R.C. Tripathia, S.K. Jhaa, A.K. Sinhaa,
G. Singha, V. ManoharanbaCentral FuelResearchInstitute,
PO-FRI,828108Dhanbad, Jharkhand,IndiabCentreforApplied Researchand
Development,NeyveliLigniteCorporationLimited, Neyveli607801, Tamil
Nadu,IndiaReceived
3October2003;accepted21June2005Availableonline26October2005AbstractLong-term
eldtrials usinglignite y ash(LFA) werecarried out in ricecrops
during the period 19962000 at Mine I, Neyveli LigniteCorporation,
Tamil Nadu. LFA, being alkaline and endowed with an excellent
pozzolanic nature, silt loam texture, and plant nutrients, hasthe
potential to improve the texture, fertility, and crop productivity
of mine spoil. The rice crops were the rst, third, fth, and sixth
crops inrotation. The other crops, such as green gram (second) and
sun hemp (fourth), were grown as green manure. For experimental
trials, LFA wasappliedatvariousdosages(0,5,10,20,50,100,and200
t/ha),withandwithoutpressmud(10
t/ha),beforecultivationoftherstcrop.Repeat applications of LFA were
made at the same dosages in treatments of up to 50 t/ha (with and
without press mud) before cultivation
ofthethirdandfthcrops.Pressmud,alightweightorganicwasteproductfromthesugarindustry,wasusedasanorganicamendmentandsource
of plant nutrients. Also, a recommended dosage of chemical
fertilizer, along with gypsum, humic acid, andbiofertilizer
assupplementing agents, was applied in all the treatments,
including control. With one-time and repeat applications of LFA,
from 5 to 20
t/ha(withandwithoutpressmud),thecropyield(grainandstraw)increasedsignicantly(p!0.05),intherangefrom3.0to42.0%overthecorresponding
control. The maximum yield was obtained with repeat applications of
20 t/ha of LFA with press mud in the third crop. Thepress mud
enhanced the yield in the range of 1.510.2% with various dosages of
LFA. The optimum dosage of LFA was 20 t/ha for both one-time and
repeat applications. Repeat applications of LFA at lower dosages of
up to 20 t/ha were more effective in increasing the yield than
thecorrespondingone-timeapplicationsofupto20
t/haandrepeatapplicationsat50
t/ha.One-timeandrepeatapplicationsofLFAofupto20 t/ha (with and
without press mud), apart from increasing the yield, evinced
improvement in the texture and fertility of mine spoil and
thenutrient content of crop produce. Furthermore, some increase in
the content of trace and heavy metals and the level of g-emitters
in the minespoil andcropproducewasobserved, but well
withinthepermissiblelimits. Theresidual effect
ofLFAonsucceedingcropswasalsoencouraging in terms of
eco-friendliness. Beyond 20 t/ha of LFA, the crop yield decreased
signicantly (p!0.05), as a result of the formationof hardpan in the
mine spoil and possibly the higher concentration of soluble salts
in the LFA. However, the adverse effects of soluble saltswere
annulled progressively during the cultivation of succeeding crops.
A plausible mechanism for the improved fertility of mine spoil
andthecarryoveroruptakeoftoxictraceandheavymetalsand
g-emittersinminespoilandcropproduceisalsodiscussed.q
2005ElsevierLtd.Allrightsreserved.Keywords:Lignite
yash;Minespoil;Management;Crop productivity;
Sustainability1.IntroductionThe generation of huge amounts of mine
spoil (four timesthe amount of coal), comprising unwanted
extraneous shalymatter and other refuse from opencast
miningextensivelypracticed in India, currentlydisturbs the natural
soil strataand ecological balance. Likewise, production of about100
Mt/yearof y ashfrom82 thermalpowerplantsinthecountry poses problems
with handling, storage, and disposal(requiring large areas of
land), apart fromapprehensionabout possible contamination of soil,
crop produce, andgroundwaterwithtoxic
traceandheavymetals(Furretal.,1977; CarlsonandAdriano, 1993;
RubeinsteinandSegal,1993) and radionuclides (Ramachandran et al.,
1990;Vijayan and Behera, 1999), especially in viewof theminimal use
made of it. In particular, the mine spoilgenerated by opencast
mining of lignite by Neyveli LigniteJournal
ofEnvironmentalManagement79(2006)173187www.elsevier.com/locate/jenvman0301-4797/$-seefrontmatter
q 2005
ElsevierLtd.Allrightsreserved.doi:10.1016/j.jenvman.2005.06.008*
Corresponding author. Tel.: C91 326 2381001-10 (Extn 357/224);fax:
C91326 2381113/2381385/2381560.E-mailaddress:
[email protected](L.C.Ram).Corporation(NLC),TamilNadu,is
moreproblematic,
asaresultofitsfragilenature,poorporosity,decientnutrientlevel, and
failure to offer any appreciable biological activity.The lignite y
ash (LFA) currently generated by
twothermalpowerstations(TPSIandII;capacity2070 MW),tothetuneof w1.0
Mt/year, doesnot ndanymajoruse(hardly 12%, mainly in civil
construction, buildingmaterials, andlandll), andthisisdistressing.
Theminespoil producedinthe extractionof coal andthe yashproduced in
power generation are two major environmentalproblems, suggesting a
need for a suitable eco-friendlytechnology, inonestroke, not
onlytosolvetheenviron-mental concerns, but alsoincreasethegainful
bulkuseofthesematerials.Much research and development (R&D) has
beencarried out in the recent past on the use of y ash
inagricultureandintherevegetationof dumpingsites andsurface mine
soil (Fail and Wochok, 1977; Bhumblaet al., 1991), where the
potential of y ash as
limingagent,sourceofplantnutrients,andsoilmodierhasbeenexploited.
Theuptakeor enrichment of various nutrientsandtoxictraceelements
insoil after y-ashamendmenthas beeninvestigated, andcropproduce has
beenfoundsafe for consumption (Sen et al., 1997). At the
CentralFuel Research Institute (CFRI), Dhanbad,
investigations(Singhet al., 1997; Singhet al., 1998; Ramet al.,
1999)of theapplicationofyashunder varioussoil typesandagroclimatic
conditions have suggested the benecialeffects of y ash in
agriculture as liming agent, soilconditioner, sourceofessential
plant nutrients, andawayto reclaim waste or degraded lands. Though
y ashcontains several essential plant nutrients, it is
devoidofhumus andnitrogen(Menonet al., 1990),
whichcanbesupplemented by organic amendments (Adriano et al.,1978),
together with effective reduction in leaching
ofmetalsbychelation(LoganandTraina,
1993).TheLFAoftheNLChasbeenreportedtobealkaline(pHZ1012, Ca, 812%),
with a cementitious nature usefulin inhibiting the inltration of
water into sandy (loose-textured) soils andprovidingplant nutrients
essential forcrop growth (CARD (Centre for Applied Research
&Development, 1997)). Like most y ashes, LFAbeingdominated by
silt-sized particles (Adriano et al., 1980),could be expected to
improve the texture, bulk density (BD),water-holdingcapacity(WHC),
andfertilityof the minespoil of NLC. Practically no detailed
R&D was available onthemanagement of minespoil
throughbulk-scaleuseofLFA, andhence this studywas carriedout. The
presentpaper describes the results of long-term eld trialsperformed
during 19962000 on mine spoil, involvingamendment with various
dosages of LFA, with and withoutpress mud, for cultivation of rice
crops. The study includesthe effects onthe fertilityof mine spoil,
cropyieldandnutrient status, trace and heavy metals content, and
the levelofradioactivityoftheminespoilandcropproduce.2.
Materialsandmethods2.1.ExperimentaldetailsTheselectedmine-spoilarea(w6000
m2, lleduptoadepthof10 m)wasproperlyleveledandploughedseveraltimes
in order to maintain uniform fertility.
Theexperimentalsetupwasarandomizedblockdesignhaving18treatments(T1T18),eachinquadruplicateofa15
m!4 marea, treatedwithvarious dosages (0, 5, 10, 20, 50,100, and200
t/ha) of LFA, withandwithout press mud(Table1), wheretreatment
T1(control)waswithout LFAand press mud, and T2was with press mud
only. IntreatmentsT3, T5, T7, T9, T11, andT13, LFAalone(5, 10,20,
50, 100, and200 t/ha) wasapplied. IntreatmentsT4,T6, T8, T10, T12,
andT14, LFA(5, 10, 20, 50, 100, and200
t/ha)wasappliedincombinationwithpressmud;andinT15T18, LFA(5, 10,
20, and50 t/ha) was appliedincombination with press mud. For all
applicationsinvolving press mud, the dosage was 10 t/ha.
One-timeapplication of LFA was made in T11T18; repeatapplications
of LFAweremadebeforecultivationof thethirdandfthcropsinT3T10at
thesamerateasbeforethecultivationof therst
crop.2.2.CroprotationandotherdetailsThecroprotationwasasfollows:rice(JanApr1997)green
gram(AprMay 1997)rice (AprAug 1998)sunhemp (Dec 1998Jan 1999)rice
(JanMay 1999)rice (Dec1999Apr 2000). The recommended dosage of
NPKfertilizer was 100:50:50 kg/ha as urea (NH2CONH2): singlesuper
phosphate (Ca(H2PO4)2) and muriate of potash
(KCl)forcultivationofeachricecrop.Table1Treatments detailSl.No.
Treatment Detail1 T1Control2 T2Pressmud (10 t/ha)3
T3Ligniteyash(LFA)(5 t/ha)4 T4LFA(5 t/ha)CPM (10 t/ha)5 T5LFA(10
t/ha)6 T6LFA(10 t/ha)CPM (10 t/ha)7 T7LFA(20 t/ha)8 T8LFA(20
t/ha)C(PM 10 t/ha)9 T9LFA(50 t/ha)10 T10LFA(50 t/ha)CPM (10 t/ha)11
T11LFA(100 t/ha)12 T12LFA(100 t/ha)CPM (10 t/ha)13 T13LFA(200
t/ha)14 T14LFA(200 t/ha)CPM (10 t/ha)15 T15LFA(5 t/ha)CPM (10
t/ha)16 T16LFA(10 t/ha)CPM (10 t/ha)17 T17LFA(20 t/ha)CPM (10
t/ha)18 T18LFA(50 t/ha)CPM (10 t/ha)L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187
1742.2.1.OtheramendmentsOtheramendments,suchasgypsum(325
kg/ha),humicacid (20 kg/ha), and biofertilizer
(RhizobiumCPhospho-bacterium; 8 kg/haeach), wereapplied,
alongwithbasaldosageofchemical fertilizers, inall treatments,
includingcontrol. Theseamendments weremadeas supplementingagents,
especially in viewof the poor fertility of minespoil andthenormal
practiceof usingsuchamendmentsby local farmers. No applications of
NPKfertilizer andother amendments as green manure were made
forgrowing green gram or sun hemp. Press mud, alightweight waste
product from the sugar industry,abundantlyavailableinareas
nearbytheNLC, was
usedasasourceoforganicmatterandplantnutrients(Table2)to improve the
texture and fertility of the mine spoil.Gypsum, of a locally
available, commercial-grade com-position, including14%sulfur,
wasappliedtoreducethecrustformationintheminespoil.
Potassiumsaltofhumicacid(20%humicacidcontent),preparedfromlignitebyachemical
method at Centre for Applied Research &Development (CARD), NLC,
was applied in the minespoil tostimulatemicrobial
growthandtoprovidesomeessential plant elements. Biofertilizer, a
composition ofRhizobium and Phosphobacterium developed in
theCARDmicrobiologicallaboratory, wasmixedwithlignitetoact
asacarrier of
microbes.2.3.Collectionandcharacterizationofminespoil,LFA,pressmud,andcropproduceThevarious
samples of dryLFAusedfor eldtrials,mine spoil and press mud before
the start of the eldexperiment (cultivation ofthe rst
ricecrop),crop produce(grain and straw), and mine spoil from
control and amendedplots after harvest of each rice crop were
collected,processed, and analyzed by the standard
procedurediscussedbelow.2.3.1.MethodsofanalysisThe physical
properties, such as mechanical compo-sition, BD, porosity, WHC,
andhydraulicconductivity, ofLFAand mine spoil were determined by
the standardmethods (Piper, 1950; Black, 1965; Jackson,
1967).Chemical properties, namely, pH, electrical conductivity(EC),
and total and available major secondary nutrients (N,P, K, S, Ca,
and Mg) of LFA and mine spoil weredetermined by the standard
methods (Black, 1965; Jackson,1967;Tandon,1995).The samples of mine
spoil, LFA, and crop produce weredigested in an analytical
microwave system (AMS, ProlaboMicrowave Oven), usingvarious
Suprapure acids
fromMerck,Germany,asreagentsforanalysisoftotalcontentsof
micronutrients (Cu, Zn, Mn, and Fe) and trace and heavymetals (Pb,
Ni, Co, Cd, etc.). For determination of
availabletraceandheavymetalscontentinLFAandminespoil,theextractionofsampleswithdiethylenetriaminepentaacetate(DTPA)
was carried out by the prescribed method (Tandon,1995),
bywhichtheavailablecontent wasestimated.
TheDTPA-extractablefractionoftotalcontenthasbeenfoundto be
relatively bioavailable for root uptake (Adriano et al.,2002).Total
trace- and heavy-metals content in variousdigestedmine spoil, LFA,
grain, andstrawsamples andavailable content in DTPAextracts of mine
spoils andLFA were estimated by liquid ion chromatography(Waters).
Thedeterminationof Cu, Zn, Mn, Fe, Pb, Ni,Cd, andCowas
madewithaC18column, withsodiumoctanesulphonate, tartaricacid,
andacetonitrileaseluent;postcolumn reagent; and ultraviolet light
(UV) detector(520 nm). The ICPak-AHRcolumn, borategluconateeluent,
and UV detector (365 nm) were used fordetermination of Cr (as
CrO4K2). The standard samplefor various trace and heavy elements
was ICP multi-element standard solution IV(Cat. No.
1.11355.0100),procuredfromMerck.ThedetectionlimitforCu,Co,Mn,and
Zn, was 5 ppb; and for Cd, Cr, Fe, Ni, and Pb,15
ppb.TheAsandHgwereanalyzedwithaUnicomSP-2900atomicabsorptionspectrometerbythehydridecold-vapor
generationmethod. Thedetectionlimit for As andHgwas5 ppb.The
g-emitting radionuclides were measured with ag-rayspectrometer,
comprisinga high-puritygermanium(HPGe)detectorwitharesolutionof1.95
kVat1.33 MeVand a volume of 77 cm3. The detector was kept at
2pgeometry for counting. The g-rays emitted from
thesampleweredetectedbytheHPGedetector,
withtheleadshieldinglinedby1 mmof aluminum, andwerededucedwith a
PC-based multichannel analyzer. The data wereanalyzed, and
radionuclides226Ra,228Ac, and40Kwereestimated for various samples
of mine spoil, LFA, andcropproduce. Thedetectionlimitsof
theseradionuclidesinthemine-spoil andLFAsampleswas5 Bq/kg;
andforgrainandstrawsamples, 0.05 Bq/kg.
ThedehydrogenaseTable2Physico-chemicalcharacteristicsofpress
mudValueParameterspH 7.44Electricalconductivity(dS/m) 1.874WHC(%)
149.4Organiccarbon(%) 13.2Moisture(%) 9.4Ash(%) 39.3Volatile
matter(%) 47.7Fixedcarbon(%) 3.6Ultimate analysisCarbon (%)
26.19Hydrogen (%) 2.67Sulfur(%) 1.82Nitrogen(%) 0.82L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 175activity in mine
spoil was estimated by the standardmethod(Kleinet al.,
1971).2.4.StatisticalanalysisOne-way analysis of variance was
performed andcomputedfor the critical difference (CD) value with
anMSTAT package (Russel et al., 1991), to assess thesignicance
(p!0.05) of the yield data, analysis of thesamples, and various
biological parameters. For other cases,wherever applicable,
standard error has been shown intablesandgures.3.
Resultsanddiscussion3.1.BiometricobservationsBiometricobservationof
thegrowthanddevelopmentstagesof ricecropsrevealedthat plant height,
numberoftillers, and plant population varied between treatments
(datanot shown). One-time and repeat applications of LFAfrom 5to20
t/ha, withandwithout pressmud, signicantly(p!0.05) increasedplant
growthperformance, withthemostpromisingresults fromrepeat
applications of LFAat thesame dosage in treatment T8(20 t/ha
LFAwith press mud)
ofTable3Physico-chemicalcharacteristicsofminespoilofexperimentalsiteatmine-I,NLCbeforeconduction
of eldexperiments,andofLFA appliedatdifferentstagesof
eldtrialsOriginalsoil(mine spoil) Lignitey ashParametersSand(%)
Coarse 16.2G1.01 30.7137.47Fine 36.9G2.15Silt(%) Coarse 14.6G0.91
51.2861.6Fine 17.8G0.1Clay(%) 14.5G0.85 8.6610.61Bulkdensity(g/cm3)
1.72G0.12 0.881.051WHC(%) 19.8G1.42 41.5950.4Porosity(%) 29.2G1.85
49.2257.81EC(dS/m) 0.436G0.02 3.774.52Dehydrogenase activity (mg/kg
hK1) 0.032G0.001 pH 6.50G0.93 10.2310.54Totalmajor
nutrientsOrganicC(%) 0.30G0.02 0.1220.180N(%) 0.021G0.001 P(ppm)
46.0G2.69 72.591.24K(ppm) 77.2G5.17 816.4993.4S(%) 0.22G0.012
0.961.15Ca(%) 0.16G0.009 9.2811.28Mg(%) 0.04G0.002
1.191.53Availablemajor andsecondary nutrientsN(%) 0.006 P(ppm)
2.8G0.13 2.863.89K(ppm) 20.6G0.93 52.5268.25S(ppm) 37.8G1.81
93.96105.22Ca(ppm) 40.2G2.13 16952000Mg(ppm) 22.5G1.23
30.2037.01Traceandheavymetals Total(ppm) Ava(ppm) Total(ppm)
Ava(ppm)Cu 70.63G4.20 2.30G0.17 40.5751.47 1.962.30Zn 79.38G6.03
1.52G0.15 148.52162.05 1.902.30Mn 133.74G8.69 6.49G0.49
162.17192.19 15.6020.72Fe 1.63bG0.11 19.61G1.31 3.97b5.44
55.9675.66Pb 18.80G1.35 BDL 12.8817.31 0.060.10Ni 44.23G3.01
2.11G0.16 129.13141.82 4.895.23Cd 1.96G0.14 0.03G0.002 10.0312.20
0.140.30Co 15.54G1.15 BDL 19.5424.10 0.370.54Cr 36.43G2.48 BDL
46.8456.88 0.400.66As BDL BDL 1.191.44 BDLHg BDL BDL
Radioactivity(Bq/kg)220Ra 15.7G0.67 74.1984.87228Ac 31.9G1.78
74.5087.5240K 150.3G8.14
352.59413.03aAv,DTPAextractable.bTotalFecontent
inpercent.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 176the third crop.
The overall growth condition of rice plants wasluxuriant, withless
incidenceof pests, plant disease, andweeds;
uniformandearlymaturity; intensecolorofgreenleaves; and bigger size
of panicles in the plots amended withLFA alone and in combination
with press mud. However, atdosages beyond 20 t/ha of LFA, with and
without press mud,particularly at 100 (T11 and T12) and 200 t/ha
(T13 and T14),biometricvalues droppedabruptly, toevenless
thanthecorrespondingcontrol values. However,
suchloweringofbiometricvaluesdiminishprogressivelyduringthegrowthof
successive crops. Also, no apparent symptoms whatsoeverof toxicity
due to trace and heavy metals and radionuclidespresent in LFA could
be observed.No biometric observations were made of greengram(second
crop) or sunhemp(fourthcrop), as these
weregrownasgreenmanure.3.2.CharacteristicsofminespoilandLFA3.2.1.MinespoilFrom
Table 3, it can be observed that the textural class
oftheminespoilissiltloamtypewithmassivestructureandverypoor
aggregates andnoappreciable similarity withnormal arablesoils.
Thesandisthepredominant fraction(53.1%) followed by silt content
(32.4%), wherein bothcontain a higher content of ne fraction than
coarse fraction.The clay content (14.5%) is quite low. The BD is
very high(1.72 g/cm3), incomparisontoarablesoil. WHC(19.8%)and
porosity (29.2%) were found to be very low,
comparedwiththecorrespondingvaluesofnormalfertilesoil(ICAR(IndianCouncilofAgriculturalResearch),1969).The
mine spoil is just acidic (pHZ6.5). The EC is quitelow (0.436 dS/m)
indicating the prevalence of a poor
salinecondition.Organiccarbon(OC)isalsolower(0.30%)thannormal for
Indian soil, 0.40.6% (ICAR (Indian Council
ofAgriculturalResearch),1969).Similarly,theconcentrationoftotalandavailablemajorandsecondarynutrients(N,P,K,
S, Ca, and Mg) and micronutrients (Cu, Zn, Mn, and Fe)in mine spoil
indicates its poor fertility. The total content oftrace and heavy
metals, such as Pb, Ni, Co, and Cr, is in therange15.544.2 ppm,
andCdis1.9 ppm. Othertraceele-ments, such as As and Hg, are below
detection limit (BDL).The available content of Ni and Cd is 2.11
and 0.03 ppm,respectively, and that of Pb, Co, Cr, As, and Hg is
BDL. Thedehydrogenase activity, ectomycorrhiza,
P-solubilizingbacteria, and total bacterial count in mine spoil
arepracticallynegligible, comparedwiththenormalsoil.
Theradioactivitylevel, particularlywithrespect
tog-emitters220Ra,228Ac,40K, is 15.7, 31.9, and 150.3
Bq/kg,respectively. Altogether, the physico-chemical
character-istics and fertility of mine spoil compare poorly with
normalagriculturalsoil.3.2.2.LigniteyashFrom Table 3, it can be
observed that the LFA applied atvariousstagesof
eldtrialsincludeslowercontentofsandand clay and higher content of
silt than mine spoil. The BDis lower, and WHC and porosity are
quite a bit higher, thanin mine spoil. EC and alkalinity (pH
10.2510.54) are
muchhigherduetothehighercontentofCa(9.2811.28%)andMg(1.191.53%).
The OC(0.120.18%) is muchlowerthan in mine spoil. Furthermore, LFA
is completely
devoidofnitrogenanddehydrogenaseactivity,andthecontentofmajor and
secondary nutrients (P, K, S, Ca, and Mg) is
muchhigherthanthenegligiblevaluesfoundintheminespoil.Totalandavailablecontent
ofmicronutrients, suchasZn,Mn, and Fe, is higher, and Cu is lower.
Similarly, total andavailable content of trace and heavy metals Ni,
Cd, Co, Cr,and As is higher, and that of Pb is lower. Besides, the
levelof radioactivity in respect to g-emitters220Ra,228Ac,40K
ishigher. In sum, the LFA could be used to modify the textureand
improve the fertility of mine spoil, provided
theapplicationiseco-friendly.3.3.CropyieldIt is evident from Fig. 1
that because of the increase in thedosageofLFA(alone)from5to20
t/ha,thegrain yieldofthe rst crop increased signicantly (p!0.05)
andprogressivelyintherangefrom11.59to24.63%overthecontrol (T1). An
additional increase in the crop yield of
1.510.2%wasduetothecombinedeffectsofLFAandpressmud. However, at
higher dosages, the yield decreasedsharply and to lessthan the
control,particularly in T11T14(100 and 200 t/ha LFA, with and
without press mud).Nonetheless, however little the growth,
nosymptoms oftoxicity were noticed from trace or heavy metals
present inLFA. This observation of increase and decrease in the
yieldalsoholdsforthegrainsofthethird,fth,andsixthcrops.Signicant
increase (p!0.05), in the range from3.0 to42.0%over corresponding
control values of individualcrops, with increasing dosage of LFA
(520 t/ha), with andwithout pressmud, anddecreaseat
dosagesbeyondthesevalues were observed. The maximum increase in
yield overthe control appearedwithrepeatapplications in T8 (20
t/haLFAand press mud) of the third crop. Also, a
greatereffectiveness was noticedof repeat applications at
lowerdosages, up to 20t/ha, of LFA made before cultivation of
thethird and fth crops, compared with both one-timeapplication at
100 and 200 t/ha of LFA(T11T18) andrepeat applications at 50 t/ha
inT9andT10. Hence, theoptimumdosageofLFA(withandwithout
pressmud)is20 t/ha for both one-time and repeat applications.
TheadverseeffectoftheapplicationofhigherdosagesofLFA(beyond20 t/ha)
was observedtodecrease insuccessiveyears of growing crops, and the
yield was either at par withthe yield of the corresponding control
of a particular crop
orslightlyhigher.Thetrendofincreasedyieldwithupto20
t/haofLFA(withandwithout pressmud),
togetherwithadecreaseathigherdosages,alsoappearedinstraw,wheretherangeofincreasewasalmost
thesame, althoughthedecreasewasL.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 177less. Such
adverse effects on the yield were wellcorroborated in a separate
investigation (CARD, 1997),and they are possibly attributable to
compaction of thesurface (hardpan formation, observed clearly
duringcultivation)resultinginpooraerationandrootpenetration,owing
to the highly pozzolanic nature of LFA containing theCaAlSi
typeofmineralsandtothehighersolublesaltsand silt content with
moisture. However, the gradualdecrease in the adverse effects on
crop yield at higherdosages of LFA(beyond20 t/ha, withandwithout
pressmud), together with progressive improvement in
growthperformance, during the course of growing successive crops(on
the basis of the biometric observations discussed
above),indicatestheprogressiveameliorationoftheconditionsofmine
spoil, favorable for crop growth. Furthermore, it seemsthat both
green gram and sun hemp grown as green manurehave contributed to
enhancing the yield of the next crop. Asanillustrationof the point,
the yieldof grain, 1.92and2.05 t/ha in the treatments T1 (without
any amendment) andT2 (with press mud only), respectively, of the
third crop wasconsiderably higher than that of the
correspondingtreatments of the rst crop (1.38 and 1.58 t/ha),
whichclearlyindicatesthepositiveeffectofgreenmanure.Thus,theoverall
benecial effect of LFAapplicationsof upto20 t/ha, alone and in
combination with press mud, insignicantly (p!0.05) increasing the
yield of various
cropsoverthecorrespondingcontrols(evenuptothelastcrop),suggestsbettermine-spoilhealthandsustainability.3.4.EffectofLFAapplicationoncharacteristicsofminespoil3.4.1.Physico-chemicalcharacteristicsAtrendwasobservedintheminesoil
withincreasingdosage of LFA, up to 200 t/ha (with and without press
mud),aftertheharvest oftherst crop:
adecreasefromcontrolvaluesforsand,from52.8to47.8%;forclay,
from14.5to14.2%; and for BD, from1.71 to 1.64 g/cm3and
anincreaseforsilt,from32.7to38.0%;forWHC,from20.1to24.2%; andfor
porosity, from30.5to34.8%(Fig. 2).Fig. 1. Effect of one-time and
repeat applications of different dosages of LFA with and without
press mud on the grain yield of rice crops (CD at 5% for
CropI0.031, Crop III0.030, CropV0.034, CropVI0.031).L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187
178Thisobservationisimportant inagriculture, especiallyasregards
the easypenetrationof theroot andbetter plantgrowth. The
morphological structure of y ash is such that
ithasasphericalhollowshape,anditispossiblethatsmall-sized particles
of LFA, containing a larger proportion of silt(54.058.0%) than mine
spoil (33.4%), accumulate in voidscreated by bigger-sized particles
of mine spoil. Thiscontributed to the modication of the texture of
minespoil (Khan et al., 1996). Furthermore, with increaseddosage of
LFA, up to 200 t/ha (with and without press
mud),anincreaseoccurredinpH, from6.50(control) to7.69;andinEC,
from0.413(control) to0.795 dS/m(Fig. 3).051015202530354045T1 T2 T7
T8 T9 T10 T11 T12 T13 T14Silt (%)0102030405060T1 T2 T7 T8 T9 T10
T11 T12 T13 T14Sand (%)024681012141618T1 T2 T7 T8 T9 T10 T11 T12
T13 T14Clay (%)051015202530T1 T2 T7 T8 T9 T10 T11 T12 T13 T14WHC
(%)BD (g/cc)0510152025303540T1 T2 T7 T8 T9 T10 T11 T12 T13
T14Porosity (%)1.581.601.621.641.661.681.701.721.74T1 T2 T7 T8 T9
T10 T11 T12 T13
T14(a)(b)(c)(d)(e)(f)Fig.2.EffectofLFAontexture(sand,silt,andclay),WHC,porosityandBDofminespoilafterharvestof
rstcrop.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187
179TheincreasesinthepHandECvaluescouldbeascribed,respectively, to
the alkaline nature and the higher solubilityof the inorganic
constituents of LFA. In fact, the increase inEC could be considered
high and likelyto suppress normalgrowth, especially as the EC
values in the range 0.51.0
dS/mcanreducegerminationandcauseburningorwiltingofsensitivecrops(CSTPA(CouncilofSoilTestingandPlantAnalysis),
1992). Probably, enhancement of EC, particu-larlyenhancement
beyond20 t/haof LFA, is oneof thefactors responsible for poor
growthandlowyields. Theincrease in OC, from 0.31 to 0.43%, could be
ascribed to theapplication of organic matter, such as press
mud,biofertilizer,andhumicacid.The available major and secondary
nutrients (N, P, K,
S,Ca,andMg)intheminespoilaftertheharvestoftherstcropincreaseddistinctivelywithvariousdosagesof
LFAof upto200 t/ha, withandwithout press mud(Fig. 4).Forexample,
Caincreasedintherangefrom40.6(T1)to44.3 ppm(T13) and from41.3 (T2)
to 45.1 ppm(T14),respectively, with increasing dosage of LFA of up
to 200 t/ha, alone andin combinationwith press mud. The
increaseofMgforcorrespondingtreatmentswasintherangefrom22.8 (T1) to
25.7 ppm (T13) and from 23.4 (T2) to 26.9 ppm(T14). This increase
in the content of Ca and Mg reects thegradual increase in pH of
mine spoil with increasing dosageof LFA. The available
micronutrients (Cu, Zn, Mn, and
Fe)weresimilarlyenhanced(Fig.5).Thisobservationisclosetondings
byothers(Simsetal., 1994).Alongwiththis,ahigher increase in
nutrient status was noticed in
combinationtreatments(LFAwithpressmud)thaninindividual ones,which
may possibly be ascribed to the benet for cropgrowth of the
complementary nutrient status of theseFig.4.EffectofLFA
onavailablecontentofmajorandsecondarynutrients
inminespoilafterharvestof rstcrop.0.01.02.03.04.05.06.07.08.09.0T1
T2 T7 T8 T9 T10 T11 T12 T13 T14pH0.00.10.20.30.40.50.60.70.80.9OC
(%)/EC (dS/m)pH EC (dS/m) OC
(%)Fig.3.EffectofLFAonpH,ECandOCvaluesofminespoilafterharvestof
rstcrop.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 180amendments. It
is pertinent to mention that thoughthe availability of nutrients
increased in the mine spoilwhen LFA was increased beyond 20 t/ha
(with and withoutpress mud), the enhancement of ECvalues, along
withhardpanformation,
probablypredominatedtocausebothpoorgrowthandlowyield.Theresultsonavailabletraceandheavymetalsinminespoil
after the harvest of the rst crop reveal that even
aftertheadditionofvariousdosagesofLFAofupto200 t/ha,with and
without press mud, the concentration of Cr, Pb, Co,Cd, and As
remained BDL. Conversely, an
appreciableincreasingtrendinNiwasnoticed,intherangefrom2.06(T1) to
2.45 (T13) and 2.10 (T2) to 2.48 ppm (T14), up to thehighest dosage
of LFA of 200 t/ha, alone and
incombinationwithpressmud(Fig.5),whichiswellwithinthepermissiblelimits
(SrivastavaandGupta, 1996). Thephysico-chemical characteristicsof
minespoil
onamend-mentwithLFA,aloneandincombinationwithpressmud,improved
appreciably, depending on the dosage andcharacteristics of the
amendments, where the rice
cropwasnotaffectedduetobuildupofsalinity,particularlyupto20
t/haofLFA.Othershavemadesimilarstudiesoftheeffectsofcoal
ashinimprovingphysico-chemical charac-teristics of mine spoil, with
no adverse symptoms of
toxicity(HillandLamp,1980;MollinerandStreet,1982).Analogoustotheobservationsmadeofminespoilafterthe
harvest of the rst crop, a trend of decreased sand, clay,and BDand
increased silt, WHC, and porosity was noticed inthe mine spoil
after harvest of the third, fth, and sixth crops,where the range of
values shows a gradually improvedtexture. The same trend could be
observed for pH, EC, andOC; available major and secondary nutrients
(N, P, K, S, Ca,and Mg); and micronutrients and trace and heavy
metals (Cu,Zn, Mn, Fe, and Ni) in the mine spoil with these crops
withincreasing dosage of LFA, with and without press
mudwithonlyslight variation. Thisvariationoccurredinaslightlyhigher
range for chemical properties and nutrient content andin a lower
range for trace and heavy metals than for the minespoil of
theprecedingcrops(datanot shown), dependingontheoverall
effectsoftheamendmentsdiscussedabove.However, other trace and heavy
metals remained
BDL.Theimprovementinthephysico-chemicalpropertiesofamended mine
spoil indicates its possibly benecial impacton crop yield, where
the role of press mud and other
organicmatter,viatheirdecompositionandNdemineralization,iscrucial
(Adrianoet al., 1982).
Theacidifyingtendencyofprotonsfromorganic-matterdecompositionofpressmud,biofertilizer,
humic acid, and even gypsum would offset
thealkalizingtendencyoftheCaOandMgOpresentinLFA,whichmaintainednear-neutralpH(6.88)oftheminespoilafter
the harvest of the last crop (sixth). As a result, the widegap
between the pH values of mine spoil (6.5) and those ofLFA
(10.2310.54) and the increase in buffering capacity donot matter
much and result in no toxicity due to thecontrolled carryover of
toxic trace and heavy metals by cropproduce. Here,
thehypothesiscanalsobeconsideredthatmixing y ash with biosolids
produces a material with morebalancedproperties (e.g. neutral
pHandthepresence ofessential elements) and less potential for
environmentalcontamination than in either material applied
alone(Stevenson, 1982; Sims et al., 1993; Wong, 1993).
Thebenecialeffectshavebeenreportedofsewagesludgeandother
amendments, such as lime and gypsum, added to coal-ash material in
maintaining pH, changing the
water-solubleOCandEC,andreleasingN,P,andKforassimilationbyplants
during the revegetation of the soil (Martens andBeham, 1976; Pietz
et al., 1989). Similarly, a
reducedincidenceofpestsinLFA-amendedplotsmight alsohaveenhanced
crop yield (Narayanaswamy and Nambirajan,2000). Thus, after
application of various dosages of LFA, upFig.5.EffectofLFA
onavailablecontentofmicronutrientsandtracemetalsinminespoilafterharvestof
rstcrop.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 181to200 t/ha,
aloneandincombinationwithpressmudandother amendments as
supplementingagents, thephysico-chemical properties and fertility
of the mine spoil improved,but with uptake of trace and heavy
metals withinpermissible limits. However, hardpan formed, and
thesoluble salt content increased, particularly at dosagesbeyond20
t/haof LFA, whichwere, of course,
graduallyannulledinthecourseofsuccessivecrops.3.4.2.RadioactivitylevelThe
radioactivity levels in the mine spoil after the harvestof thelast
crop(sixth), withrespect tog-emitters220Ra,228Ac, and40K, were
observed to have gone above thecontrol value,from14.2to 26.1,
29.7to41.6,and145.2to170.3 Bq/kg, respectively, with the
application of themaximumdosage of LFAof 200 t/ha alone (data
notshown). But the levels of the radionuclides were well
withinpermissiblelimits andinagreement withthendings byothers
(Ramachandran et al., 1990; McMurphy
andRayburn,1996).3.4.3.BiologicalactivityThe biological activity of
the mine spoil, almostnegligible initially, was found to have
improved signicantly(p!0.05) as a result of the addition of LFA of
up to 20 t/ha,aloneandincombinationwithpressmud.Aftertheharvestof
the rst crop, a signicant (p!0.05) increase occurred inmicrobial
activities over the control. The ectomycorrhizaincreased from0.0
(T1) to 38.0 spores/g; P-solubilizingbacteria, from0.01 (T1) to1.5
CFU!104; total bacterialcount, from 0.18 (T1) to 4.5 CFU!104g; and
dehydrogenaseactivity, from0.035 (T1) to 0.068 mg/kg hK1, up to
thedosageof 20 t/haof LFAalone(T7). Asimilar trendwasobserved for
treatments of up to 20 t/ha of LFA incombinationwithpressmud(T8),
withenhancedrangesofdifference (data not shown). This trend was
also observed inthe mine spoil after harvest of succeeding crops,
withprogressively increased ranges of difference. With
appli-cations of LFA beyond 20 t/ha, the total bacterial
populationdecreased (as was also evident from a decrease in the
enzymeactivities), probablyas a result of
hardpanformationanddevelopment of anaerobic and waterlogging
conditions.These enhanced microbial activities in the mine
spoilmight have played a crucial role in improving the
soilfertilityandyieldof various crops appreciably. Here, theorganic
amendment as supplementing agent might havecontributed to the
improvement in the condition of the minespoil by increasing cation
exchange capacity (CEC) andorganic-matter (humus) content,
resultinginbetter fertilityandenhancedmicrobial activity, besides
enhancedimmo-bilization of toxic elements and other factors
inhibitingmicrobes (Chaney and Giardono, 1977). As well, the role
ofthe improved texture of the amended mine spoil in
enhancingbiological activitycannot beruledout (Lyonet al.,
1952).These observations are in agreement with ndings by
others(Pitchel,1990;Laietal.,1999).3.5.EffectsofLFAonthecharacteristicsofcropproduce3.5.1.CharacteristicsofgrainFig.
6 shows that the total major and secondarynutrients, suchas N, P,
K, S, Ca, andMg, inthe grainsamples fromtreatment T7(20 t/ha of
LFAalone) afterharvest of the rst cropincreasedover the control
(T1),from1.28to1.34, 0.059to0.071, 0.66to0.75, 0.068to0.70,
0.035to0.42, and0.019to0.026 ppm, respectively.Concomitantly,
anincrease occurredinthe total contentof thesenutrients
inthegrainsamplefromtreatment T8(20 t/haof LFAwithpress mud),
withnotablyenhancedranges of difference. With applications beyond
thisamount, the concentration of these nutrients decreased,similar
tothecropyield.Fig.6.EffectofLFA onconcentrationoftotalmajor
andsecondarynutrients ingrainsamplesof rstcrop.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 182The
concentration of micronutrients and trace and heavymetals also
increased over the corresponding control valuesin the LFA
treatments (with and without press mud) of up to20 t/ha, for each
element (Fig. 7). In a trend quite similar tothat of the results
obtained for yield and major andsecondary nutrients, the
concentration of micronutrientsdecreased with the increase in LFA
dosagebeyond20 t/ha,whichsuggests that suchhighdosages of LFAhave
noappreciable impact on the nutrient status of grain. Likewise,the
concentration of the trace and heavy metals Cr, Pb, andNi
inthegrainsamples fromtreatment T7(20 t/haLFAalone) increased over
control T1, from 1.64 to 2.39, 1.22 to1.38, and 5.21 to 6.33 ppm,
respectively. This observation isalso pertinent to the grain sample
from treatment T8 (20 t/haLFAwith press mud) with a notably higher
range ofdifference. However, therewasalsoadecreaseat
dosagesbeyond20 t/haofLFA(withandwithoutpressmud). Butthe
concentrations of Co, Cd, and As were BDL in all LFAtreatments. The
trendobservedfor major andsecondarynutrients, micronutrients,
andtraceandheavymetalswasalsoobservedfor thegrains
fromsucceedingcrops, withranges of difference being a little on the
high side in the
caseofmajorsecondarynutrientsandbeingonthelowsideinthecaseofmicronutrientsandtraceandheavymetals.Thesmallincreaseintraceandheavymetalscontentissuggestiveof
lowavailabilityof traceandheavymetals,which gradually decreased
because of the increase in the pHof the mine spoil
withincreasingLFAdosage (Fulekar,1993), thepresenceof
metalsinoxideform(Pageet al.,1979), an increase in adsorption of
metals by soil withincreasedpH, andtheresultingmarginal
uptakebycropproduce(Adrianoetal.,1980).However,thepossibilityofmetalsbecoming
moresoluble aftera long duration cannotbe entirely ruled out, as
the liming effect of y ashapplication is prone to diminish due to
natural oranthropogenic soil acidication processes (Sims et
al.,1995). Thecarryover of toxictraceandheavymetals ingraindepends
onseveral factors, suchas pH, OC, CEC,micro-organisms,
concentration of metals, and their form ofoccurrence,
andthemobilityofsuchelementstotheroot,theirtransport fromroot
surfacetoroot interior, andtheirtranslocation fromroot to shoot
(Chaney and Giardono,1977)playsasignicantrole.
ThePbandCrabsorbedbyroots normally remain in the root and are not
readilytranslocatedtotheshoot(Alloway,1995),whereasCdcanreadily be
translocated from root to shoot, but it is the highervalues of Zn
and pH that reduce the uptake of Cd. Probablyfor thisreason,
theuptakeof thesetoxictraceandheavymetals in the grain was well
within the critical toxicity limits(MacNieol andBeckett, 1985;
Alloway, 1995; SrivastavaandGupta, 1996).
AsfarasthehigheruptakeofNi, from5.21 to 6.35 ppm, is concerned, it
is probably because of itsreadily mobile characteristics in plants,
leading to itsextensive accumulation in the seeds (Alloway,
1995),which is also not alarming. Furthermore, the concentrationsof
Co, Cd, andAswerebelowdetectionlimits, whichisobviously due to
their relatively lower initial content in bothminespoil andLFA.
Asaresult, thegrainsamplesfromtreatments at theoptimumdosageof
LFAhadimprovednutrient status, whereas the carryover of toxic trace
andheavy metals was well within permissible limits.
Thedecreaseinconcentrationof nutrientsingrainat dosagesbeyond 20
t/ha of LFA is probably due to hardpan formationin the mine soil,
together with an increase in its salt content,resulting in poor
growth. This observation is well
bolsteredbyotherstudies(Pitcheletal.,1994;Senetal.,1997).3.5.2.CharacteristicsofstrawConcomitantly
with the variation in the characteristics ofthe grain samples after
the harvest of the various rice cropswithdifferent dosagesof LFA,
aloneandincombinationwith press mud, the characteristics of the
straw samples alsoFig.7.EffectofLFAonconcentration
oftotalmicronutrients andtraceandheavymetalsingrainsamplesof
rstcrop.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 183varied(datanot
shown). Theobservedtrendofdecreasedconcentrations of major and
secondary nutrients, micro-nutrients, and trace and heavy metals in
the straw, like in thegrain, beyond20
t/haofLFAispossiblyduetothesamereasonsdiscussedabove.3.5.3.RadioactivitylevelincropproduceFig.8showstheradioactivitylevelof
g-emitters226Ra,228Ac,
and40Kinthegrainsamplesofvariouscropsfromplots amended with higher
dosages of LFA in T11 (100 t/haLFA)andT13(200
t/haLFA),suggestingaslightincrease,particularly in226Ra and228Ac.
But in40K, the increase wassubstantial,
from40.2(control)to52.6and64.8 Bq/kginT11andT13, respectively,
inthegrainsampleof
therstcrop.Thisobservationalsoholdstrueinthecaseofstraw,with lower
ranges of difference (Fig. 9). Furthermore, in
thegrainandstrawsamplesofthesucceedingcrops,asimilartrend of
progressive increase from one crop to the next
crophasbeenobserved,butwithlevelswellwithinpermissiblelimits(EisenbudandThomas,
1977; Boweh, 1996). Thus,the radioactivity levels of these emitters
increased onlymarginally, except in the case of40K, probably as a
result oftheapplicationofLFAcontainingahighercontentof40K,170.3
Bq/kg, thanminespoil (145.2 Bq/kg). Althoughtheradioactivity of
muriate of potash (KCl) was not measured,it is possible that its
application as one of the components ofthe basal dosage of chemical
fertilizer (NPK) duringcultivationmight
havecontributedtotheenhancedlevelof40Kincropproduce(SrivastavaandGupta,
1996). Inaseparatestudy, Geerardo(2001) expressedconcernaboutthe
radioactivity in crop produce resulting from theapplication of
chemical fertilizers, including KCl. Theapplicationof
phosphaticfertilizers, liming, andmanuresto reduce the uptake of
radionuclides in crop plantsFig.9.EffectofLFA ongammaradioactivity
ofstrawsamplesfromdifferentcrops.Fig.8.EffectofLFA
ongammaradioactivityofgrainsamplesfromdifferent crops.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 184(Skiba, 1987)
through reduction in exchangeable fraction ofradionuclides has
beeninvestigated(ButnikandIshenko,1990).3.6.PlausiblemechanismforimprovementofsoilhealthThe
overall benecial effects of y ash on soil health maybe ascribable
to the cumulative effect of the improvement
inphysico-chemicalandbiologicalcharacteristicsofthesoil.Because of
the presence of CaSi minerals with apozzolanic nature (zeolite
formation), along with themoisture of the soil (Fulekar and Dave,
1986), y ashbrings about improvements in various
physico-chemicalproperties, suchasBD, porosity, WHC,
andtheavailablewaterinthesoil.Inparticular,theyashhasahighersiltcontentthansoil,
andtheinltrationrateofsandysoilsormine spoil is drastically checked
because of the increase insilt (Furr et al., 1977), whereas in the
clay-rich type of soils,thereverseis thecase, withbetter water
movement andworkability, apart from decreased plasticity or
crackformationafterdrying.Asyashhasmostoftheessentialplant
nutrients other than nitrogen and humus (Menon et al.,1990),
applying it to the soil naturally improves its fertilityby
enriching it with these elements, and this results
inincreasedcropyield.
Theorganicamendmentsmadewithyashalsohelpinimprovingthe humus
andmicrobialactivities of the amended soil or mine spoil,
besidesadjustingthepHby wayofdecompositionandNdeminer-alization
(Adriano et al., 1982; Stevenson, 1982; Sims et al.,1993; Wong,
1993), controllingtheavailabilityof metalstothe plant bychelation,
andreleasingnutrients duringvegetation(LoganandTraina,1993).The
formation of a zeolite layer on the surface of y-ashparticles
results into two exchangeable sites, one with
6-foldcoordinationandthe other with12-foldcoordination,
toaccommodatemicro- andmacronutrients, respectively, sothat each
ash particle becomes a repository of nutrients anda potential
nutrient pump (Sahu, 1999). Besides,
adsorption,desorption,andexchangebeingpHdependent,themineralpump is
energized selectively for nutrient transfer toachieve rapid growth
of plant in the y-ash-amendedsoils. Furthermore, during the
ashwater interaction,oxyhydroxide of iron(goethite) is
formedandacts as agreat scavenger of trace metals. The
oxyhydroxideocculates,eitherascoatingorasdiscretegrains,andthusimmobilizes
the heavy metals, leading to their
reducedavailability(Leekieetal.,1980).Consequently,thelossofnitrogen
fromthesoilbecauseofvolatilization,leaching,and denitricationis
signicantly reduced, and thisimproves the N-utilization efciency of
nitrogenousfertilizersandminimizessoilwaterpollution.
Theplants,then, takeupnitrogeninphases, asandwhenneeded.
Flyashalsohelps inthe retentionof the chemical
fertilizerappliedthroughinorganic sources inthe soil
systemforlongerperiods(CFRI, 2000),
leadingtoresidualeffectsofy-ashapplication.
Theuptakeandcarryoveroftraceandheavy metals in grain depend on
several factors, such as pH,OC, CEC, micro-organisms,
concentrationof metals andtheir formof occurrence, their mobility
to the root andtransport fromroot surface to root interior, and
theirtranslocationfromroottoshoot.4.ConclusionsLFA acts as an
excellent soil modier and conditioner, avery good limingagent, anda
source of essential plantnutrients for appreciably improving the
texture and fertilityof the mine spoil, with signicant (p!0.05)
increase in thecrop yield (about 42%) over the control, together
with betterresidualeffects, especiallyupto20 t/haofLFA,
withandwithout press mud. In general, the optimum dosage of LFAis
20 t/hafor bothone-timeandrepeat applications,
andoverallmaximumyieldwasobtainedonrepeatapplicationofthesamedosageof20
t/haofLFAwithpressmud.
Noadverseeffectonthequalityofminespoilorcropproducewas observed up
to the optimum dosage of LFAapplications, except for
hardpanformationinmine spoiland the enhancement of soluble salt
content at dosagesbeyondtheoptimum, which, infact,
decreasedprogress-ively during cultivation of succeeding crops. The
uptake andcarryoverofcertaintraceandheavymetalsandg-emittersin mine
spoil and crop produce were well within permissiblelimits.
Therefore, aside fromrestoring the ecology of amine-spoil area and
making it agriculturally worthwhile,
thejudiciousapplicationofLFA,withandwithoutpressmud,provides a
gainful and eco-friendly solution to the
problemofthedisposalofLFA.AcknowledgementsThe authors express their
sincerest gratitude to StandingScientic Research Committee (SSRC),
Department ofCoal, India for providing nancial assistance. They are
alsothankful tothe Director, CFRI, andNLCauthorities forproviding
infrastructure facilities and permission to
publishthepaper.ReferencesAdriano, D.C., Woodford, T.A., Ciravolo,
T.G., 1978. Growth andelemental compositionof cornandbean. Journal
of EnvironmentalQuality 7,416421.Adriano, D.C., Page, A.L.,
Elseewi, A.A., Chang, A., Straughan, I.A., 1980.Utilization
anddisposal of y ashandothercoal residues interrestrialecosystem:
areview.Journal ofEnvironmental Quality9,333344.Adriano, D.C.,
Page, A.L., Chang, A.C., Elsweei, A.A., 1982. Cdavailability to
Sudan grass grown on soils amended with sewagesludgeandyash.Journal
ofEnvironmentalQuality 11,197203.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 185Adriano, D.C.,
Weber, J., Bolen, N.S., Paramasivam, S., Koo, B-J.,Sajwan, K.S.,
2002. Effects of high rates of coal y ash on soil turf grassand
ground water quality. Air Water &Soil Pollution 139
(14),365385.Alloway,B.J.,1995.
HeavyMetalsinSoil,seconded.Blackie,London.Bhumbla, D.K., Singh,
R.N., Keeker, R.F., 1991. Water quality fromsurface mined land
reclaimed with y ash. Proc. Ninth Ash Use Symp.Am. Coal, Ash
Assoc., vol. 57. Academic Press, Orlando, FL, pp. 122.Black, C.A.,
1965. Methods of Soil Analysis Part 1& 2. American
SocietyofAgronomy
Inc.,Wisconsin,USA.Boweh,H.J.W.,1996.TraceElementsinBiochemistry.AcademicPress,London.Butnik,
A.S., Ishenko, G.S., 1990. Effect of mineral and organic
fertilizersonuptakeof uraniumandthoriumbycottonandwheat. Soviet
SoilScience42,4247.CARD(Centre for Applied Research
&Development), 1997. Soil Reclama-tionof BacklledAreas of
Neyveli Opencast Mines. CARD, NLC,NeyveliandFaculty
ofAgriculture,Annamalai University 1997.Carlson, C.C., Adriano,
D.C., 1993. Environmental impacts of coalcombustion residues.
Journalof Environmental
Quality22,227247.CFRIReport,2000.Bulkscaleutilization of
yashfromChandrapur andBhusawal TPPsinagricultureandfor
reclamationof degradedland.No.TR/CFRI/1.01/2000-01,CFRI, Dhanbad,
Jharkhand, India.Chaney, R.L., Giardono, P.M., 1977. Microelements
as relatedtoplantdeciencies and toxicities. In: Elliot, L.F.,
Stevenson, F.J. (Eds.), Soilsfor Management of Organic Waste Water.
American Society ofAgronomy, Madison,WI, pp.235279.CSTPA (Council
of Soil Testing and Plant Analysis), 1992. Hand Book onReference
Methods for Soil Analysis. Soil and Plant Council, Inc,
GA.Eisenbud, M.,Thomas, G., 1977. Environmental
Radioactivity.AcademicPress,NewYork.Fail Jr., J.L., Wochok, Z.S.,
1977. Soybean growth on y ash amended stripminespoils.
JournalofPlantSoil48,472484.Fulekar, M.H., 1993. The pH effects of
leaching of heavy metals: laboratoryexperiment.Indian
JournalofEnvironmentalProtection 13,185192.Fulekar, M.H., Dave,
J.N., 1986. Disposal ofyashanenvironmentalproblem.
InternationalJournalof Environmental Studies26,191.Furr, A.K.,
Kelly, W.C., Bache, C.A., Gutenmann, W.H., Lisk, D.J.,
1977.EnvironmentalScienceTechnology 11,11041120.Geerardo, C.M.,
2001. Environmental potassiumradioactivityandpublichealth(Source:
physics.msuit.edu.ph/spvm/papers/2001/maxino.pdf).Hill, H.S., Lamp,
L.A., 1980. Australian Journal of ExperimentalAgricultureAnimal
Husbandry377, 31.ICARC(IndianCouncil of Agricultural Research),
1969. HandBookofAgriculture.ICAR, NewDelhi.Jackson, M.L.,1967.Soil
Chemical Analysis.Prentice-Hall,Delhi.Khan, S., Taira, B., Singh,
J., 1996. Effect of FAonphysico-chemicalproperties and nutrients
status of soil. Journal of Environmental Health38(1),4146.Klein,
D.A., Loh, T.C., Goulding, R.L., 1971. Arapid procedure to
evaluatedehydrogenase activity of soils low in organic matter. Soil
Biology andBiochemistry 3,385387.Lai, K.M., Ye, D.Y., Wong, J.W.C.,
1999. Enzyme activities in sandy soilamended with sewage sludge and
coal y ash. Air Water &SoilPollution113, 261277.Leekie, J.O.,
Benjamin, M.M., Hayes, Kaufman, A., Atman, S.,
1980.Adsorption/Co-PrecipitationofTraceElementsfromWaterwithIronOxy-Hydroxides.ElectricPowerResearch
Inst,PaloAto, CA.Logan, T.J., Traina, S.J., 1993. In: Allen, H.E.,
Perdue, E.M., Brown, D.S.(Eds.), Trace Metals in AgriculturalSoils,
in Metals inGround Water,vol.309. LewisPublishers, Chelsea,MI.Lyon,
T.L., Buckman, H.O., Brady, N.C., 1952. The Nature and
PropertiesofSoils.Macmillan,NewYork.MacNieol,R.D.,Beckett,P.H.T.,1985.Criticaltissuesconcentrationsofpotentially
toxicelements. PlantandSoil 89,107.Martens, D.C., Beham, B.R.,
1976. Proc. 4thInternationalSymp. onAshUtilization
(St.Louis,Mo),pp.657666.McMurphy, L.M., Rayburn, A.L., 1996.
Nuclear alternations of maizeplants grown in soil contaminated with
coal y ash. Report.Archives of Environmental Contamination and
Toxicology 25(4),520524.Menon, M.P., Ghuman, G.S., James, J.,
Chandra, K., Adriano, D.C., 1990.Physico-chemical
characterisationof water extracts of different
coalyashesandyash-amendedcomposts. AirWater&Soil Pollution50,
343.Molliner, A.M., Street, J.J., 1982. Proc. Soil Crop Science
Society, Florida,vol.41,pp.217220.Narayanaswamy, P., Nambirajan,
S.G., 2000. Discovering y ash
aspesticide.Proc.2ndInternationalConferenceonFlyAshDisposalandUtilization(Session-IX),NewDelhi,
vol.31,p.31.Page, A.L., Elseewi, A.A., Straughan, I.R., 1979.
Physical
andchemicalpropertiesofyashfromcoal-redplantswithreferencetoenviron-mentalimpacts.
ResidueReview 7,83120.Pietz, R.I., Carson Jr., C.R., Peterson,
J.R., Denz, D.R., Lue-Hing, C., 1989.Application of sewage and
other amendments tocoal refuse: I.
Effectsonchemicalcomposition.Journal ofEnvironmentalQuality
18,164.Piper, C.S., 1950. Soil &Plant Analysis. The
Universityof Adelaide,Adelaide,Australia.Pitchel, J.R., 1990.
Microbial respiration in y ash/sewage sludge
amendedsoils.Environmental Pollution63,225.Pitchel, J.R., Dick,
N.A., Sutton, P., 1994. Journal of EnvironmentalQuality23,766.Ram,
L.C., Jha, S.K., Jha, G.K., Tripathi, R.C., Singh, G., 1999. Effect
of yashfromFSTPPonthecultivationofwheatandricecropsinalluvialsoil
ofmurshidabaddistrict. In: Ram, L.C., Tripathi, R.C., Jha,
S.K.,Srivastava, N.K., Singh, G. (Eds.), ProceedingsNational
SeminaronUtilizationof FlyAshinAgriculture &for
Value-AddedProducts(ISBN81-7525-184-0).CFRI, Dhanbad.Ramachandran,
T.V., Lalit, B.Y., Mishra, U.C., 1990. Modications innatural
radioactivitycontent of soil samples aroundthermal powerstations in
India. Indian Journal of Environmental Health 32 (1),
1319.Rubeinstein,R.,Segal,S.A.,1993.In:Allen,H.E.,Perdue,E.M.,Brown,D.S.
(Eds.), RiskAssessment of MetalsinGroundWater, vol.
209.LewisPublishers, Chelsea,MI.Russel, D.F., Russel, D., Scott,
P.E., 1991. MSTAT (version 1.41)Computer Programme, Crop and Soil
Department, Michigan StateUniversity.Sahu, K.C., 1990. In: Dayal,
U., Sinha, R., Kumar, V. (Eds.), Environ-mental Aspects of Ash
Pond: A Critical Appraisal. Proc. Symposium onFly Ash Disposal and
Deposition Beyond 2000 AD, vol. 8490.
NarosaPublishingHouse,NewDelhipp.8490.Sen, P.K., Saxena, A.K.,
Bhowmick, S., 1997. In: Raju, V.S.V. et al. (Ed.),GroundWater
ContaminationAroundAshPonds andAshDisposalSystem,Narosa, NewDelhi,
pp.326342.Sims, J.T., Vasilas, B.L., Ghodrati, M., 1993. Effect of
coal yashandcompostedsewage sludge onemergence andeasygrowthof
covercrops.CommununicationinSoilScienceandPlantAnalysis24,503.Sims,
J.T., Vasilas, B.L., Ghodrati, M., 1994. Soil hydraulic properties
andelementalleachingduetoamendmentofsoilbyyashaddition.
AirWater&Soil Pollution81,349361.Sims, J.T., Vasilas, B.L.,
Ghodrati, M., 1995. Evaluation of y ash as a
soilamendmentfortheAtlanticCoastalplant:II.Soilchemicalpropertiesandcrop
growth.AirWater&SoilPollution 81,363372.Singh.
G.,Tripathi,P.S.M.,Tripathi,R.C.,Gupta, S.K.,JhaR.K.,Rudra,S.R.,
Kumar, Vimal.,1997. In: Proc. of the 13th Internationalconference
on Solid Waste Technology &Management. WidenerUniversity,
Philadelphia, PA,USA,pp.114119.Singh, G., Tripathi, P.S.M.,
Tripathi, R.C., Jha, S.K., Gupta, S.K., Roy,R.R.P., Jha, R.K., Ram,
L.C., Srivastava, N.K., Yenprediwar,
M.,KumarVimal,1998.SolidwastemanagementinTPPs:environmentalimpactsofabandonedashpondsandtheirbiologicalreclamation.
In:Proc. FourteenthIntl. Conf.
onSolidWasteTechnology&Manage-ment.WidenerUniversity,
Philadelphia, PA,USA,pp.10A.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 186Skiba, T., 1987.
Ability of some crop species to take up and
transport90Srand137Sinrelationtofertilizerapplication. Pamiet
Putawsk, vol. 891987, pp.185193 (Polish).Srivastava, P.C., Gupta,
U.C., 1996. TraceElementsinCropProduction.OxfordandIBHPublishing
Co.Pvt.Ltd,NewDelhi.Stevenson, F.J.,1982. HumusChemistry.
Wiley,NewYork.Tandon, L., 1995. Methods of Analysis of Soils,
Plants Waters and Fertilizers.Fertilizer Development and
Consultation Organization, New Delhi.Vijayan, V., Behera., S.
N.,1999. Studies on heavy elements andradioactivity of crops grown
in soils treated with y ash.Proceedings National Seminar on
Utilization of Fly Ash inAgriculture andfor Value AddedProducts
(ISBN81-7525-184-0)heldat CFRI, Dhanbadon15and16Nov, 1999,
Technical SessionII, p. 61.Wong, J.W.C., 1993. The production of
articial soil mixture from coal
yashandsewagesludge.EnvironmentalTechnology 16,741.L.C.Rametal.
/JournalofEnvironmentalManagement79(2006)173187 187