Aerobic in situ stabilization of completed landfills and old sites
Investigations
of aerobic m situ stabilization of old sites inlaboratory-scale
tests show that asignificant
reduction of thenitrogen concentration in the leachate takes
place.
Thedegradation
and release of organiccompounds
via the gasphase
could be accelerated. Therequired
aeration volumesfor the
biological
stabilization aretechnically
realizable as the total oxygen demand isrelatively
low.K. Leikam
K.-U. Heyer
R. Stegmann
Technical University of Hamburg-Harburg, Harburger
Schloßstr 37, 21071 Hamburg, Germany
Keywords -
Aerobic treatment, completed landfills, in situ stabilization, reduction of emission potentialCorresponding
author: K Leikam, Techmcal University of Hamburg-Harburg, Harburger SchloBstr. 37, 21071 Hamburg, GermanyWaste Manage Res) 1999 17 555-562 Copynght (Q ISWA 1999
Printed in UK - all rights reserved Waste Management & Research
ISSN 0734-242X
Introduction
In
Germany approximately
540 landfills are moperation
andover 86000 old sites are known m total
(BMU 1994).
If techmcal barriers do not exist or ifthey
areinsufficient,
environmental impact may occur via gas and leachateemission
pathways.
Results from research activities
by
the TUHamburg- Harburg
mto thelong-term
behaviour of landfills show thatemission concentrations
especially
for leachatedrop
tocompletely
harmlesslimiting
valuesonly
afterlong periods
of 100 to 300 years
(Heyer
&Stegmann 1997).
Completed
landfills and old sites without bottom lmer canbe secured
by mstalling
a landfill capping system in combmation with active gas extraction. The gasproduction
rate in old
completed
landfills is low. For this reason landfillgas
(LFG)
cannot be used for thermal or energetic purposes.Nevertheless LFG has to be
treated,
e.g.by
usingcatalytic
combustion or biofilters.
Although
thebiological
activity of oldcompleted
landfills isrelatively low,
leachate representsan emission
potential
forlong periods
of time. Landfillcapping systems reduce or prevent leachate
production
butthey
may fail m function and again leachateproduction
hasto be
expected.
It becomes clear that no real remediation of the landfill can be achievedby
the above-mentionedmeasures but
only
a securingby reducmg
emissions whilstconserving the emission
potential.
The
objective
should be todevelop
suitable remediationmeasures to reduce the
long-term
emissionpotential
of alandfill.
f’
Objective of in situ stabilization
measuresThe
objective
of in situ stabilization measures is to transfer the landfillbody
as soon aspossible
to a state of lowbiological
reactivityby accelerating
the microbial conver-sion processes. To realize
this,
treatmentprocedures
withactive aeration are suitable.
By
this means, organiccompounds
which are noteasily biodegradable
will beaerobically degraded.
As there is a considerable reduction mpollution potential,
a lesscostly
soil cover with atopsoil
layer
which could be used for recultivation should be considered instead of the installation of a liner system. Thissoil cover should be
designed
in a way that leachateproduction
is minimized and there is apotential
for methane oxidation.Due to the in situ pretreatment, leachate concentration will decrease so that the
period
for leachate treatment could be reduced. Intotal,
thefollowing
economicpotentials
resultfrom the in situ stabilization:
o substitution of a landfill
capping
systemby
lesscostly
andlong-lasting topsoil
cover of sufficient thickness so that a water balancedevelops;
o lower operating costs for the treatment of the
leachate;
o lower costs for the maintenance of the
topsoil
cover;o reduction of the aftercare
phase
for severaldecades;
o oxidation of trace organics and methane m the top soil
cover.
Investigations of in situ stabilization of
wastesfrom completed landfills
on alaboratory scale
Material and methods
To carry out the investigations on aerobic
stabilization,
several wastesamples
from two landfills have been examined. The solid wastesamples
were takenduring
gas wellsdrilling.
The age of the wastes was between 8 and 14 years. Thepresented
test results refer to the wastesamples
of landfill A with extraction
depths
between 11 and 17 m.The
investigations
mto aerobic stabilization were carned outin three landfill simulation reactors
(LSR)
at a temperature of 30°C. Further informationregarding
theexpenmental
set-up of the landfill simulation tests can be found m
Heyer
et al.1998.
The three landfill simulation reactors were
imtially operated
under anaerobic conditionsby
leachate recircula-tion for several hundred test
days.
This was done to mamtamtypical
environmental conditions of a closed landfill when starting the aeration tests, and m order to be in the positionto assess the
potential
of emission under anaerobicconditions.
Subsequently,
the reactors were aerated withthe aeration rates as mentioned below m: ’Aerobic stabilization of wastes from
completed
sites’.Results
Chemical-physical
solid examinationsTo charactenze the waste
samples, chemical-physical
examinations of the solid
samples
were carried out beforeplacing
them mto the landfill simulation reactors, and at thebeginning
of the aerationpenod.
The results of the solidanalyses
are shown in Table 1.The low volatile solid values and the carbon contents of the waste
samples
at thebeginning
of the aerationpenod
show that a
significant degradation
of the orgamc substance tookplace durmg
the landfill simulation under anaerobic milieu conditions. At thebeginning
of the aeration tests, thesolid
samples
B2Z15 in the reactor LSR 5 show the lowest carbon concentrationsindicating
that these solidsamples
are
already
to alarge
extent stabilized. Thus a faster aerobic stabilization of the solids isexpected.
The decrease of the nitrogen m the solid matter and theconductivity
of theleachate
during
the anaerobicphase
m the LSR ismamly
because of
dilution,
which is the result oftakmg
leachatesamples
andreplacing
the same amount ofliquid by
tapwater.
Respiration activity of
wastesamples
from closedlandfills
Thebiological
activity of the solidsamples
was determinedby
means ofrespiration activity (RA)
examinations with theSapromat (Voith, Heidenheim, Germany).
The way aSapromat
functions is described in Leikam &Stegmann
1995.
Apart
from the usual determmation of the oxygen consumption after 96h, long-term
investigations of 500 h - andpartly
of more than 1000 h - have been carried out. Via theselong-term
investigations the maximum oxygen Table 1. Results of the solidanalysis
landfill(Leikam et al. 1997) LSR=Landfill simulation reactors
Fig 1 Oxygen demand of solid
samples
after 96 h (RA96 h) and calculated maximum oxygen demand (RAmax )
according
toLineweaver-Burk (in Kramer et al 1993).
demand of the solid
samples
can be ascertained. The oxygen consumption is related todry
matter(dm).
The respiration activity has been determmed before
placing
the solidsamples
mto the landfill simulation reactors.Fig.
1 shows therespiration
activities after 96 h(RA96 h)
and the maximum respiration activities(RAmaX)
for LSR 3 andLSR 5
compared
to ’fresh residual wastes’.The determmation of the maximum oxygen demand was
effected after a test
period
of 500 h or 1000 hoursby
meansof
reciprocal plots according
to Lmeweaver-Burk(m
Kramer&
Sprengler 1993).
It becomes evident that the
samples
taken from inside the landfillonly
showapproximately
10% of their imtialbiological
activity(fresh
residual wastes of householdsRA96
h = 50 to 80 mg02g dm-’).
The total air volumeneeded for m situ stabilization of 1
t deposited
waste can becalculated from the determined maximum oxygen demand of the solid
samples (RAmax
= 25 to 32 mg02
gdim-1).
Thetotal air demand of waste
sample
B1B2(LSR 3)
isapproximately
105m3/t dm
and for thesample
B2Z15(LSR 5) approximately
85m3 air
tdm- 1
Aerobic stabilization of
wastesfrom completed
sitesThe aeration tests were started after an anaerobic
phase
mthe LSR of
approximately
350 to 400 testdays.
The start ofaeration is marked
by
means of arrows inFig.
2. The aerationof the three landfill simulation reactors was effected at
intervals. The aeration rates were as follows:
9 LSR
1/BlN13 approximately
0.09 1kg dm
m approx-imately
1 mm. The aeration was carried out two to fourtimes per week.
~ LSR
3/B 1 B2 approximately
1.8 1kg dm h~ for
approxi-mately
4 h. The aeration was carried out every seventh and every fourteenthday.
. LSR
5/B2Z15 approximately
1.8 1kg
1 dmh-1
forapproximately
4 h. The aeration was carried outweekly.
Leachate
The
pH-value
in the leachatechanges
as a function of theaeration rate. Whilst a
significant
increase of thepH-value
>pH
7.0 can be stated for the reactors LSR 3 and LSR5,
where
higher
aeration rates wereapplied,
the low aerationrate for LSR 1 does not have an effect on the
pH-value.
The sulfate content in the leachate increase pattern is quite similar to the parameter
pH-value.
An influence of the aeration on the stronger decrease of the bicarbonate content cannot be found for the different aeration rates and mtervals.The lime-carbonic acid balance does not seem to be disturbed at these aeration rates.
The chosen aeration rates
scarcely
have an effect on the organic contaminants in the leachate. The chemical oxygen demand(COD)
concentration does not showsignificant changes
but it has to be taken into consideration that the COD content is within the range of 400 to 500 mg1-1
andalready
very low at thebeginning
of the aeration tests. Afteran aeration
period
of 200days,
the COD concentrations arebelow 200 mg
1-1.
TheBODS
contents(biological
oxygendemand)
in the leachate at thebeginning
of the aerationtests are
only
at 25 to 50 mg1-1
and decreaserelatively
fastto values below 20 mg
BOD5 1-1.
Due to the very lowconcentration, a faster decrease of the
BODS
valueduring
Fig 2 LSR 3/B1 B2: aeration (1
81 /kg
dm*h in 4 h) fromday
407 on’ ~
LSR 5/B2715 aeration (1
1 81 /kg
dm*h in 4 h) fromday
454 onTKN in the leachate landfill A, LSR 2 (anaerobic) LSR 3/5 (Leikam et al 1997).
the aeration
phase
could not be foundcompared
with thestrictly
anaerobic landfill simulation.The nitrogen content in the leachate of reactor LSR
1/B1N13 only changes
to a small extent. The decrease of the TKN concentration(Total Kjeldahl Nitrogen)
m theleachate of reactors LSR
3/B1B2
and LSR5/B2Z15
isclearly
discernible
(see Fig. 2).
The TKN concentration for reactorLSR 3 is far below 70 mg
1-1
after 200days
of aeration whilstthe concentration for reactor LSR 5 is far below 70 mg
1-1
after
only
50days
of aeration. An increase of the nitrateconcentration m the leachate of reactors LSR 3 and LSR 5 could not be found. Part of the nitrogen is released via the
gas
pathway
as ammomum m condensate and as ammonia mexhaust air.
Fig.
2 shows the TKN content m the leachate of the landfill simulation reactor(LSR 2) operated
under anaerobic conditions which was also filled with wastesamples
fromlandfill A. Even after 900
days,
the nitrogen content in the leachate of reactor LSR 2hardly
falls below 100 mg1-1.
As aresult of the aerobic in situ
stabilization,
the nitrogen contentin the leachate can be reduced
significantly
in a few months(LSR 3/5).
This effect is very important asespecially
theparameter nitrogen influences
significantly
the aftercare-period (see Heyer
&Stegmann 1997).
The
heavy
metal content m the leachate wasextremely
low for all exammed landfill simulation reactors. Even at the
beginning
of the aeration no increased release ofheavy
metals could be
found,
e.g. as a consequence of apossible
demobilization or oxidation of metal sulfides.
Gas
At the
beginning
of aeration, the gasatmosphere
in thelandfill simulation reactors showed
typical
gas composition for the stable methanephase
of a landfill.The low aeration rates for reactor LSR
1/B1N13
werechosen to simulate ’natural’
change
from anaerobic toaerobic environmental conditions of an old
deposit.
Due to the low air
supply
in LSR1/B1N13
the oxygen is consumedimmediately
after the addition(5 1 d-1)
which isindicated
by
the low oxygen content and theslight
increaseof the
CO2
concentration in theproduced
gas(see Fig. 3).
By
the aeration and the involved dilution of the landfill gasproduced anaerobically,
the methane concentration decreases and the inert gasportion
of nitrogen increases.The organic substances in the solids are converted
aerobically dependent
upon the amount of airsupplied.
After
complete
oxygen consumption the anaerobicdegrada-
tion continues. An inhibition of the anaerobic microorgan- isms is not detectable. A stimulation of the microorganisms is more
likely
as the carbonrelease,
in the form ofmethane,
still increased after the
beginning
of the aeration(see Fig. 4).
In LSR
3/BIB2
anaerobic conditions are also restored after several hours of intensive aeration(100
1 airh-1
= 1.8 1air
-lkg
dmh-1 ).
Thus methane concentrations between 15 and 35 vol. % in the landfill gas are found at the end of the ’non-aeration’phase. During
the aerationphase,
themethane concentrations decrease to zero. In the reactor
LSR
5/B2Z15
similar fluctuations of the gas composition are ascertained. At the end of the ’non-aeration’phase,
themethane concentrations amount to
only
10 vol. % and less.Fig 3 Gas composition in the LSR 1 /3/5, landfill A.
LSR 1 /BIN 13 3 aeration (0 09
I kg ~
dm in 1 min) from day 321 onLSR 3/B1 B2 aeration (1 8
I kg ~
dm*h in 4 h) from day 407 onLSR 5/B2Z15 aeration (1 8
1 kg-’
dm*h in 4 h) from day 454 onFig. 4 Carbon release via the gas
pathway
in LSR 1 /3/5, landfill A.The influence of the aeration on the
degradation
of the organic components becomes evident. The release of the converted orgamc components takesplace
via the gaspath
m the form of methane and carbon dioxide.
Fig.
4 describes the influence of aeration on the carbon turnover.The mcrease m carbon release
by
aeration is apparent for the low aeration rate for LSR 1 as well as for the aeration rates for LSR 3 and LSR 5. The influence of the aeration onthe
degradation
processes is quitesignificant, especially
mLSR 3.
By
aeration thedegradation
of orgamc substanceswas
approximately
five timeshigher compared
to thedegradation
under anaerobic conditions over the sameperiod
of time.In LSR
5,
thedegradation
rate of the organic substances could be more than doubled. The lower carbon release ofreactor LSR 5
compared
to reactor LSR 3 isprobably
due tohigher
gasproduction during
the anaerobicphase
oftreatment
(until
the 420thday
of thetest)
which resultsm less lower
biodegradable
substances at thebegmnmg
ofthe aeration tests.
The
laboratory-scale
testsregarding
the aerobic stabiliza-tion of solids waste
samples
fromcompleted
landfills showthat, by
aeration, a strong reduction of the mtrogenconcentration m the leachate can be achieved. The data
m
Fig.
2 showthat,
due to aeration, the target value of the 51stappendix
of the German waste waterregulation (Rahmen-AVwV)
is reached more than 400 to 500days
earlier
compared
to reactor LSR 2 whichoperated
understrictly
anaerobic conditions.Therefore,
it can beexpected
that the
penod required
for leachate treatment can besignificantly
reducedby
several years.The carbon turnover is increased
significantly during
theaeration
phases. Organic
substances medium-difficult ordifficult to
degrade,
which canonly
bedegraded
over along period
of time m an anaerobicenvironmental,
are mcreas-mgly
convertedduring
the aerationphases.
After a test
penod
ofapproximately
500days,
there arestill also anaerobic environmental conditions present. When
evaluating
the data from thelaboratory
scale tests it has to betaken mto consideration that aeration was
only
effectedonce a week or every 14
days -
that means that due to lack ofoxygen between the aeration measures there was
always
achange
m environmental conditions frompartly
aerobic tocompletely
anaerobic.By
practismglonger periods
andshorter mtervals of aeration, aerobic
degradation
processes will become moresignificant.
This may result in a faster mineralization of the waste. Further investigations to optimize these intervals are necessary.Transfer of the laboratory
testresults
toactual completed landfills
An assessment of the maximum oxygen demand can be made
via the
long-term
test m theSapromat -
as described m’Respiration
activity of wastesamples
from closed landfills’above. The maximum amount of air needed is between 85 and 105
m3/t dm
for the wastesamples
derived fromlandfill A
(deposition
age between 8 and 14years).
On thebasis of the
laboratory
aeration tests it is assumed that for the aerobic in situ stabilization a maximumpenod
of 1 to1.5 years may be necessary.
Assuming
an aerationperiod
of 1 year and an averagewater content of the wastes of 35%
(wet waste)
as well as a total airsupply
of 100m3/t dm,
adaily
aeration rate resultsm up to 0.18
m3 t wet waste-’ (=
0.0075m3
wet wasteh-1 ).
As the calculated airsupply
rateonly
covers therequired
oxygendemand,
the aeration rate should behigher
to cover inevitable losses
(e.g., mcomplete
utilization of theoxygen).
It becomes evident that the airsupply
rate isrelatively
low and that the aeration caneasily
be realized without causing techmcalproblems.
Conclusion
The investigations of the in situ stabilization carried out on a
laboratory
scale showedthat, by
aeration measures, asignificant
reduction of the nitrogen concentration in the leachate takesplace
within a few months.Furthermore,
thedegradation
and release of organiccompounds
via the gasphase
could besignificantly
accelerated. It can be concluded from the test results obtained up until now that the aerobic in situ stabilization is suitable for the stabilization of olddeposits
m so far that the hazardouspotential
issignificantly
reduced. _
The
required
aeration volumes for thebiological
stabiliza-tion are
technically
realizable as the total oxygen demand of thedeposited
wastes is very low(m
the order of 100m3 t
tdm-1).
Theadvantages
involved with m situ stabilization are the reduction of environmental impacts and cost savings, where a welldesigned
soil covenng system, instead of acapping system is
mstalled;
which is lesscostly
m construction, operation and maintenance. In addition thephase
of aftercare issignificantly
reduced.References
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