A B S T
R A
C TS
ha r o nN
ap pie r :
Th
e U s e of T he rm
al In a ctiv ation ofM
ale-S
pe ci fi c Col i p hage s a s Pote nt
ia
l
Ind
ic ato r s o f Patho ge n Red
u cti
o n si
n Th
e rm
op hi
li
c A n a e r ob i
c Di
ge stio n
(
u nde r the d ir e ctio n of Dr.M
a rk Sobs ey)
M
ale
-spe c
i fi
c(
F+)
c ol i p hage sw
e r e in v e sti gated
a si
ndi
c ato r s of vi
r u si
n a cti
v ati
o nd
u ri
ng the rm
op h i l ic d i ge stio n a nd othe r the rm
al pr o c e s s e s. B e c a u s e pathoge nm
o nito rin
gi
ns
l
ud
gei
s d i f fi c ult, c o stl y, a n di m
pr a ctic al,m
ic r ob ial in d ic ato r s a r e n e eded to pr ed ic
tp
ath
oge n r ed
u cti
o n si
nC
la s sA b io s o
li d
s F+ c ol i p hage s a r e a pr om is
in
g c a nd i d
atei
nd i
c ato ro
f f
e c al
c o ntam in a
tio n
a nd a s u r r ogatef
o r vi
r u s r edu ctio n in wa ste tr e atm
e nt pr o c e s s e s. F+R N A gr o up I, F+ R
N
A gr o up 111, a n d F+ D
N
A p hage s we r e is o lated fr o
m m
u nic
i
pal
sl
ud g
e.In
la
b
o r ato ry studi
e s the ki
n etic s a nd e x te nt o fi
n a ctiv atio n of gr o ups I a nd I I I F+ R N A , a nd
F+ D
N
A c ol i p hage sw
e r e qu a nti fi ed a nd c om
pa r ed at 5 3 "^C, a tem
pe r atu r e u s ed i
nt
h
e rm
oph i l i
c a n a e r ob i
cd i
ge sti
o n . Is ola
te s of
gr o ups I a nd
I I I F+ RN
A a nd F+ DN
Ac ol
i
p hage s w e r e e x po s ed to 5 3 "C
in
a n a utom
ated, the nn o r egu lated he atb
lo ck a nd
ti
te r ed
a
ft
e r0
, 5 a nd
6 0m i
n ute s.A f
te r6 0 m i
n u te s at 5 3 °C
, F+ RN
A gr o up I I I c ol i
ph
age s we r ei
n a ctiv a
ted si gni fi c a ntl y gr e ate r(
P < 0 0 0 1)
tha n the F+ R N Agr o up I a n
d
F+ DN
Ac o
H
p hage s. T hein a c
ti
v ati
o nk i
n eti
c s of gr o up I I I F+ RN
A c oli
p hage s r e s em b l
e tho s e of
s o
m
e e nte ri
c vi
r u s e s a nd
s om
e othe r pathoge n s T he r e s ults of this
stud
y elu ci d
ate thet
h
e rm
al pr ope rtie s of them
ale-spe ci fi c c o
l i
p hage s ub gr o ups a ndf
a ci
lit
ate the dev elo
pm
e nt of
t
i m
e a nd
tem
pe r atu r e r el
atio n shi
ps th
at pr ed ic
t e nte ri
c vi
r u s a n d othe r pathoge n r ed
u ctio n si
nA C
K
NO
W
L E DG
EM
E N T SI wo ul d l i ke to tha nk Br o
w
n a nd Cal d w el l fo r fu nd ing of th is pr oj
e ct a nd theColu
m
bu s(
G
e o rgia
) W
ate rW
o rks fo r its s up po rt. Iw
o ul d als o li
ke to th
a nk Dr.
M
i
cha elA itke n , Dr
M
i
n aSh
eh
e e,N i
c ol
e v anA b
el,K i m
be rl
y B la uth, a nd
Ph i l l i
pC
r u nkf
o rh
el
pw i
ththe
C
B F T 3 pr oj
e ct a nd D o ugW
ait, D r. Ja n V inj
e, T i in a Pa s a n e n, a nd S
j
o n Oudej
a n s fo r theirhel p w ith the s e r oty p
i
ng, P C R, R T-P
C
R, a nd
R L B H yb
ri
di
z atio n pr o c ed
u r e s.T A B L E
O
F CO
N T E N TS
Page
L I S T O F F I G
U
R E S viL I
S
TO
F F IG
U R ES
vi
L I
ST
O
F A B B R E V I A T IO N S
vi i
I I
N
T RO
D UC
T IO N
1G e n e r al O b
j
e ctiv e s
5S pe ci fi c O
b
j
e ctiv
e s 5I I R E V I E
W
O
F T H E L I T E R A T UR
E 7Pri
m
a ry a nd S
e c o nda ry Tr e atm
e nt a nd
theC
r e ati
o n of S lud ge 7T he r
m
oph i l i
c An a e r ob
ic Di
ge stio n 9C
la s s A Bio s o
li d
s a nd L a nd A
p p Uc atio n o f Sewage S lud ge 1 2Pote ntial E
ff
e cts of Pathoge n s 1 4V ir u s
I
n a cti
v ati
o nK i
n etic s
1 8Ba cte r
i
oph
ag
e s a s Indi
c ato r s of Tr e atm
e n t of C
la s s A B io s o l i ds 2 2L
i
te r atu r e R e vi
ewC
o n clu si
o n s 3 5I I I
M
A
T E R I A LS
A N DM
E T HO
DS
3 6Expe r
i m
e ntal
D e si gn 3 6T he r
m
oph i l i
c An a e r obi
c D i ge ste r(
TA
D)
3 9M
ale-S pe ci fi
cC
ol i
p hage An al ys
i
s fr om
M
u n ici pal S lud ge 4 2M
ale-S
pe c
i fi
cC
oli
ph
ageC
ha r a cte riz atio n 4 5Lab Sc ale He at In a c
fi
v atio n Expe ri m
e nts o n Co l i p hage s 5 2I V R E
S
U L T S 6 1T he rmop h i
l i
c A n a e r ob ic D i ge stio n
Expe rim
e nts 6 1M
ale-S
pe ci
fi
cC
oli
p hageC
ha r a cte riz afi
o n 6 8La
b Sc a
le T he rm
al
In a ctiv a
fi
o n Expe rim
e nts o n F+C
oli
p hage Is o late s 7 2
R
e s ult
sSu
m m
a ry8 3
V D I S
C U
SSI
O N
8 5T he r
m
oph i
li
cA
n a e r ob i
c Di
ge sfi
o n Experi m
e nts 8 5Is olate
C
ha r a cteri
z atio n 8 8Lab
Sc a
le In a cfi
v ati
o n Experi m
e nts9
1V I C
O N
C L US
IO N S
9 6A P P E
N
D IC
I ES
9 8
L I S T
O
F TA
B L E SPa
g
eT a
b
le 1 Pathoge n a nd In dic a
to rC
rite ria fo r C la s sA
B io s oli
ds 1 3T ab le 2. Ente
ri
cV i
r u s Th
e rm
al In a cti
v ati
o nC
ha rt18
T a
b
le 3C
ha r a cteri
stic s o fS
lud
ge So u r c e sU
s edi
n theC
B F T^ Pr oj
e ct 3 7T ab le 4 R T -P
C
R T he r
m
o cycle r
Pr o gr am
49
T a
b
le 5.M
a ste rM
i
x Com
po n e nts fo r PC
R Re a ctio n s 50T ab
le
6 PC
R T he rm
o cycl
e r Pr ogr am 50
T ab le 7.
C
o n c e ntr atio n(
Lo gi o/ g TS
)
a nd R edu ctio n s o
f
M
ale
-S
pe c
i fi
cC
oli
p hage sb
yTr e at
m
e nt in theC
o nti
n u o u s D i ge ste r6 3
T ab le 8.
C
o n c e ntr ati
o n s(
Log l0
/ g TS
)
a nd Redu c
ti
o n s of
M
ale
-S
pe c
i fi
cC
oli
ph
age s T r e atm
e nti
n th
e Batch
Re a cto r6 4
Tab le 9 B e st-fi t Pa r a
m
ete r s
f
o r In a ctiv a
fi
o n o fM
ale-spe ci
fi
cC
oli
p hage s6 7
Tab le 1 0 F+ D N A a nd F+ R N A Is olate s fo u nd
i
n Fe ed a nd Batch Sam p le s6 9
Tab le 1 1 F+ R N A Se r oty pe s
f
o u nd i
n Fe ed a nd BatchS
am
p le s 70
Tab le 1 2 F+ D N A Ge n oty pe s
f
o u nd
in Fe edS
am
p le s vi
a R L B-H y
b
ri d iz ati
o n 7 2Tab le 1 3
M
ale-Spe ci fi c Col
i
ph
age Logjo Redu ctio n s in Lab Sc a
leL I S T
O
F F IG
U R E SPage
F
i
gu r e 1 Fi
r st-O
rd
e r Ki
n etic s 1 9F
i
gu r e 2. T w o-Popu lat
i
o nM
odelK i
n etic s 2 1F i gu r e 3 Crite ria fo r
S
ele ctio n ofM
ic r obe si
n Bi
o s o l i ds o rW
a stewate r a nd Crite ria fo r a nI
d
e al In dic a
to r 2 5F i gu r e 4. Co n c e ntr atio n s of
M
ale-S pe ci fi c Col i p hage s a s a Fu n ctio n of T i
m
e in In a ctiv atio n Rate Expe rim
e nts at(
a)
5 1 °C
a nd
(
b)
5 3 °C 6 7
F
i
gu r e 5. Logi o Redu cti
o n s ofM
ale -S
pe c
i fi
cC
oli
p hageI
s olate s afte r6 0 m in u
te s at 5 3 °C
.7 4F
i
gu r e 6 Logi o Red
u cti
o n s of
M
al
e-S
pe c
i f
i cC
ol i
ph
age Is ola
te s af
te r6 0 m in u
te s at Ro om
T e
m
pe r atu r e 7 5F i gu r e 7. Lo
gi o Redu ctio n s of
M
ale-S
pe ci
fi
cC
o li
p hage Is olate s Du e to He at(
5 3 °C Onl y 7 5
F
i
gu r e 8 In a ctiv atio n of Gr o up I(
M
S2
)
F+ RN
A Col i p hage Fe ed Is olate I l lu str ating F ir st-O
rde rK i
n efi
c s 7 7F i gu r e 9. In a ctiv a
fi
o n of Gr o up I I I( Q|
S
)
F+ R N A Col i p hage Fe ed
Is olate 7 8F i gu r e 1 0 In a ct
i
v atio n Sum m
a ry Gr o up I(
M
S 2)
Fe ed, Batch, a nd Co ntr o l Is olate s at 5 3 "C
f
o r 5 a nd 6
0m in u
te s 8 0F
i
gu r e 1 1 In a cti
v ati
o nSu
m m
a ryG
r o up I I I(Q/3
Fe ed a ndC
o ntr ol
s Is olate s at 5 3"C
fo r 5a n
d
6 0m i
n ute s8
1F i gu r e 1 2 In a ctiv atio n Su
m m
a r y F+ D NA
Col i p hage Fi
el d a n dC
o ntr ol Is olate s at 5 3 °C fo rL I S T
O
F A B B R E V IA
T IO
N SA
N
O VA
= a n al ysi
s of v a ri
a n c eB
O
D = bi
olog ic al o xy ge n dem
a nd
b
p = ba s epair s
C
=C
elsiu sC
B F T =C
olum b
u s Bi o s ol i d
s Fl
ow T hr o ugh
T he rm
op h i l ic Tr e atme ntC
F R =C
ode of
Fed
e r al Regula
tio n s
C
FU
= c ol
o ny
f
o rm ing u ni
t DN
A = d io xyri bo n u cleic a ci d E c oli = Es cher ich ia c ol iE P A = En v ir o n
m
e n tal Pr ote cti
o nA
ge n cyF+ =
m
ale-spe ci f ic c ol i p hage
F+ D
N
A =m
ale-spe ci
fi
c DN
A c ol i p hage F+ R NA
=m
ale-spe c
i fi
c R N A c oli
p hage FC
= fe c al c oli
fo rm
sg = gr a
m
sm
l -m
i l l ih
te r sM
P N =m
o stpr oba
b
le n um b
e rN H
3 = am m
o ni
aN R = n o r e
m
o v alO
W
AS
A =O
r a n geW
ate r a nd Se
we rA
utho ri
ty P BS
=p ho sp
h
ateb
uf f
e r s oluti
o n PC
R =pol y
m
e r a s e chai
n r e a cti
o nP
F
R P = pr o c e s s e s to fu rthe r r ed
u c e path
oge n sP F U = p laqu e fo r
m
in g u n itP
O
TW
= Pub
l icl yO
w n ed
Tr e atme ntW
o rk
sR L B = r e v e r s e l in e b lot
R
N
A = ri b
o n u c lei
c a ci d
R P
M
= r otatio n s pe rm i
n uteR T-P
C
R = r e v e r s e tr a n s c ri pta s e
-pol y
m
e r a s e chain r e a ctio nSC
W
R F = So uthC
olum b
u s(
G
A) W
ate r Re s o u r c e s Fa ci l itySS
= s u spe n
d
ed
s olid
ss s-D
N
A =s
in
g le str a nded D N As s-R
N
A =s
i
ng le str a nd
ed RN A
T A D = the r
m
oph i l i
c a n a e r ob i
cd i
ge stio nT N T
C
= to o n um
e r o u s to c o u ntT
S
= total s ol id
sT
SB
= try pti
c s oyb
r oth
W
S SL D
=W
e ste r n L ak
e Supe r
io r
Sa nita ry Di
stri
ctp X=
m
ic r oli
te r sI I N T R
O
D U C T IO
NIn the
U
ni
ted State s, the fi r st c om
pr ehe n siv e s a nita ry s ewe r system wa s n otc o n str u cte
d
u nti l
18
5 5(
in
C h i
c ago)
a nd th
ef
i r st s ew
ag
e tr e atm
e ntf
a ci l ityi
n 1 8 86
(
N
ew
Yo rk
C
ity)
.Cu r r e n
tl y the r e a r e o v e r 19,4 0 0m
u ni
ci
pal Pub lic
l yO
w n ed Tr e atme ntW
o rks(
P O TW
s)
in
theU S
., tr e ating r o u g h l y 5 0 b
il l
i
o nm
^of r aw s ewage a ye a r
(
N A S, 1 9 9 6)
Asthe s ewage is tr e ated, it go e s thr o ug h a s eri e s of pr o c e s s e s that r edu c e the c o n c e ntr atio n of
the e a s
i
l y-d
e c om
po s ab le o r
g
a ni
cm
ate ri
als a nd
pathoge ni
c o rga nis
m
s Sew
age slud
gei
s them
ate ria
l b
efo r eit
r e c eiv e s
bio
lo
gi
c al
o r chem i
c al tr e atme nt a nd b i
o s olid
s a r e the ge n e r al l ys et t
l
e ab l
e s oli d b i
olo
gi
c al
r e si d
u al
pr od
u c ed d
u rin
g the tr e atm
e nt of
s ew age w a stewate r. Itis
ofte n a
m
ixture of hum
a n a n d indu stri
al w a ste s a ndm
ay c o n sist of n om
o r e than 1%
of thew a stewate r f low .
C
ha r a cte ri
sti
c s of
th
e slud
ge depe n d o n the w a stewate r tr e atme nt pr o c e s sa n
d
slu
d ge tr e atm
e nt(
Eb
e rle et al 1 9 9 4)
.T he in stal latio n a n d ope r at
i
o n of
w a stewate r tr e atme ntf
a ci l itie s c o ntri butes
i g
ni f
i c a ntl y to poll
utio n
r ed
u ctio n, pr e v e nti
o n of d
amage to the e n vi
r o nm
e nt, a nd
pr o te ctio n
of pu
b
l ic he alth. How e v e r, thed
is cha rge of s ew age slud ge, w hethe r tr e ated
o r n ot, c a n c r e ates e rio u s
w
ate r pol l
utio n pr ob
lem s in the r e c eiving bod y of w ate r o r la nd Raw s ewage of
te nc o nta
i
n sm
a ny pathoge nic o rga nis
m
s, w h ichis a
gr e at pote ntial pub
l ic he al
th c o n c e r n .A d
d i
tio n a
l l y, the hi
g h c o n c e ntr atio n s of
s u spe nded
s o l i ds(
S S)
a nd n utri e n ts, a s w el l a s theo rga n
ic
m
at te r(
e g., BO
D)
of
r aw s ewage,m
ay c r e ate e utr op hi
c ati
o n pr ob l
em
s. T hec o
m m
o nm
et hodsf
o rfi
n al dis
po s al of slu
dg
e a r e la n dfi
l ls, la n d ap p
l
ic ati
o n, a ndi
n cin e r a
ti
o n(
Z ho u a ndM
a v inic
2 0 0 3)
S lud ge in cin e r ati o n
fi
r e s slud ge at h i g h tem pe r atu r e s in a c om
bu sto r. In cin e r atio n
isc o st
l
y a nd
e n e rg yi
nte n si
v e It pr od
u c e s of f
-ga s that n e eds to be r egu lated
(
e gh
yd
r o c a rb
o n s, a nd
c a rb
o nm
o n o xi de
)
Sl
ud
ged is
po s al to la nd fi
lls
,m
o stl yd i
spo s ed
al
o n gw ith mu nici pal s o
l i
dw
a ste s, r e s ultsi
nd i f
fi c ultie s in c om
pr e s sio n
of di
spo s edm
ate rials. T hec apa c
i
tie s of e x isting la n dfi
ll
s a r edi m in
is
hin
g; how
e v e r, the am
o u nts o f slud ge a nd d i
spo s alc o sts c o nt
in u e
toin c r e a s e
Itis
m
o r e a nd m
o r e di f fi
c ult tofi
nd
ap pr opria
te a nd
ad
equ ate n ews
i
te sf
o r la ndfi
l ls(
Zh
o u a ndM
a vin
i
c 2 0 0 3)
It
i
s r e c og
niz e
d thatb
e n efi
cial l
a nd
ap p l ic atio n(
e g agri
c u ltu r al s oi l
c o ndi
tio n
i
n g o rfo r e st fe rti l izin g
)
of pr o c e s s ed slud ge(
b io s ol i ds)
is a c o st-ef fe ctiv e a nd e n v
i
r o nm
e ntal l ys u sta
in a
bl
e optio n
, be c a u s e n utri
e nts a nd
o rga n ic mat te r a r e r e cycled
to s oi
ls In 1 9 9 3 theU S E PA r ele a s ed the te chnic al sta nda rds
(
4 0 C F R Pa rt 5 0 3)
fo r the u s e a nd di
spo s al ofb i
o s ol i d
s, a nd i
ntr od
u c ed
the c ri
te ri
af
o rC
la s s -Ab i
o s o
h d
sC
la s s-Ab i
o s ol i d
s a r e e s s e nt
ia
l l ypathoge n
f
r e e, me et a c c eptab
l y lowm
etal
c o n c e ntr ati
o n s a nd
v e cto r at tr a ctio n
r edu c
tio n
r equ
ir e
m
e nts, a nd c a nb
eb
e n efi
ci
al l
y la nd-ap p
h
ed wit
ho ut r e strictio n s(
US
E P A 19 9 9; N AS
2 0 0 2; Z ho u a nd
M
a vin ic 2 0 0 3)
T he s e r equir e
m
e nts a r em
et thr o ug h Pr o c e s s e s to Fu rthe rRedu c e Pathoge n s
(
P FR
Ps)
, w hi
ch tr a n sfo rm
slud ge fr om
wa ste pol luta nts w ith h i g h le v elsof pathoge n s
i
nto a v alu ab leb i
o s o li d
s r e s o u r c e(
Z ho u a ndM
a vin
ic
2 0 0 3)
.P F R Ps that a r e c u r r e ntl y r e c ogn
i
z ed b
y theE
P A a r e c om
po stin
g,h
e atd
ryin
g,h
e attr e at
m
e nt, the rm
op h i l ic a e r ob
icd
i ge sti
o n,b
eta r ayi
r r ad
iatio n,g
am m
a r ayi
r r adi
atio n , a nd
pa ste u r
i
z ati
o nW
he n the s ep
r o c e s s e s a r e ope r ated u sing spe ci fi
ed
c o nd
i ti
on s, pathoge ni
c(
U S E P A 1 9 9 9;N A
S 2 0 0 2)
. D e sp ite the pote ntial fo r the rm
op h i l ic a n a e r ob ic d i ge stio n tom
e etC
la s s A c rite ri
a, thi
s pr o c e s s is n ot c u r r e ntl
y r e c ogni
z ed
a s a P F R P to pr od
u c eC
la s s AB io s o l i ds.
In a
d
di
ti
o n to the pathoge n r equi
r em
e nts.C
la s s A bi
o s oli
dsm
u st bem
o ni
to r ed fo ri
nd ic ato r o rga ni
sm
s, fe c al c ol i fo rm
, o rS
al mon el la sp p ba cte ria(
1)
at the tim
e o f u s e o rd i
spo s al;(
2)
at the ti m
e th
eb i
o s ol id
s a r e pr epa r ed fo r s ale o r g iv e n aw ay in a bag o r othe rc o nta
i
n e rf
o r la nd ap p l ic ati
o n; o r(
3)
at th
e ti m
e theb i
o s oli
ds a r e pr epa r ed tom
e et th
r e er equ
i
r em
e nts fo r " e x c epti
o n al qu al ity" slud ge to e n s u r e that gr ow t h of b
a cte ri
ah
a s n oto c c u r r e
d
(
US
E P A 1 9 9 9)
M
u ni
ci pali
ti
e s a nd PO
TW
s ty pi
c al l y r el
y o n a s s ays of i
n di
c ato rm i
c r o o rga ni
sm
s tod
ete ct pathoge n r ed
u cti
o n s o r e x c e s siv em
ic r ob i
al
c o ntam i
n ati
o n o f pub l i
che alth c o n c e r n
To pr ote ct t
h
ep
ub l i
c 's
h
e al
th
a nd
to s a v e ti m
e a nd m
o n ey,i
ti
si m
pr a cti
c al
tod i
r e c tl
ym
o nito r,i
de nti f y, o r e n um
e r ate the hu nd
r eds o f path
oge ni
cm i
c r o o rga n ism
s a s s o ci
ated w ithf
e c al pol l
uti
o n .O
v e r 14 0
vi
r al path
oge n sh
a v eb
e e ni d
e nti fi
ed f
r omh
um
a nf
e c e s, n ew o n e s
c o ntin u e to be d
i
s c o v e r ed
a nd it is bel ie v ed that the r e a r em
a ny oth
e r s sti
l l u nkn own(
Ga ntz e ret al 1 9 9 8
)
.W
hi
lem
ethod
s ha v eb
e e nd
e v eloped
fo r dete cti
ng a nd
a s s ayi
n g spe ci fi c vi
r u s e so r vir u s gr o ups, they a r e ofte n e xpe n siv e, te chn
i
c al l yd
em
a ndi
n g, a nd
ti m
e-c o n s u
m i
n g Al
s o,v
i
r u s e s a r e ofte n pr e s e nti
n low but sti
ll
risk y c o n c e ntr ati
o n s, w hi
chm
ay r equi
r e th
e a n al ysi
sof la rge s a
m
p le v olum
e s, s u ch a sm
o r e tha n te n l ite r s of wate r o r mo r e tha n 10 0m
l of slud ge.T
h
e u s e ofi
ndi
c ato r s e ntai ls qu a n ti f y in gm
o r e p le nti
ful mi
c r ob
e s that c om m
o nl
yi
nhab i
t thei
nte sti
n e s of
wa rm
-b lo od
ed a ni m
als a nd
c o n si de ring the
m
a si gn thatm
o r e ha z a rdo u sC
u r r e ntl yf
e c al c ol i fo rm b
a cte ri
a a r e t he sta nda rd m
ic r ob i
alin
d i
c ato r u s ed i
n theU
nited State s fo r b io s ol i ds a ndm
u nici palw
a ste wate r H owe v e r , be c a u s e vir u s e s a r e sm
al le ra nd a r e
m
o r e r e sista nt to in a ctiv atio n pr o c e s s e s tha n ba cte ria, fe c al c ol i fo rm
s a r e c o n si de r edi
n ad
equ atei
nd i
c ato r s of
wate rb
om
e e n te ric v
i
r u s e s(
s u ch
a s Hepatitis A vir u s
, Rota viru s e s,a n
d
A de n o vir u s e s, a nd sm
al l, r o u nd str u ctu r ed
"ga str o e nte r
i
ti
s vi
r u s e s "s u ch a s Astro viru ses
a n
d N
or o vir u s e s, in cludi
n gN
o rwal k
vir u s
) (
H a v ela a r 1 9 9 3)
.Ente r
i
cb
a cte ri
op hage s, vir u s e si
nf
e cting e nte ri
c ba cte ri
a, ha v eb
e e n pr opo s ed
a sm
o r er el iab le ind ic ato r s
f
o r hum
a n vi
r al pathoge n s(
G
e rba 1 98
7; Le cle r c et al
. 2 0 0 0)
. Col i p hage s ,v
i
r u s e s w hi
ch i
n fe ct Es ch
e r ich ia c ol
i, ha v e pr ob
ab
le fe c al o ri
gin s
, a r e c o n sis
te ntl yf
o u nd i
ns ew age, a nd a r e a
l
s o e a si l y, quick l y, a nd in e xpe n siv el
y qu a n ti fi
ab le.T
h
e r e a r e s e v e r al di f f
e r e nt ta x o n om
ic gr o ups of
e nte ric
ba cte rioph
age s, n ot al l ofw h ich
m
ay be go od vir u s ind ic ato r s. Ba c te ri
op hage s th
ati
nfe ct their ho sts thr o ug h r e c epto r s
o n the c el l w al l a r e " s o
m
atic " "M
al
e-s pe cifi
c"
c ol i p hage s
i
n fe ct their ho sts thr o ug hr e c epto r s o
f
F pi l i
, wh i
ch a r e s u rfa c e ap pe nd
age s e n c od
ed b
y F-p
l
a sm i d
ge n e s. Th
e s om
atic
c o
l i
p hagef
am i l i
e sin c
ludeM
yo virid
a e,M
ic r o v ir id
a e,S
iph
o virid
a e(
o rS
tylo v
irid
a e)
a ndPodovir i da e Le viviri da e a nd In o vir i da e a r e
m
ale-spe c
i
fi c c oli
p hage fam i
l ie s w h ich c o ntai
nR N A a n d D
N
A ge n om
e s, re spe c tiv el y F+ R
N
A c ol i p hage s c a n be s ub d ivi
ded fu rthe r intofo u r gr o ups : gr o up I
(
M
S 2)
, gr o up I I(
G A)
, gr o up I I I(
Q
jS)
, a nd gr o up I V(
S P)
D i f fe r e ntp
e r si
ste n c e of
p hag
e sin
the e n vir o n
m
e ntis s u
g ge sted
to be r elated
to ph
ag
em
o rph
olog y(
La s ob
r a s et al
19 9
7)
Iti
s th
o ugh
t that th
e ph
ysi
c al str u ctu r e, c om
po si
tio n
a nd m
o rp holog yof F+ R
N
A p hage s c lo s el
y r e s em b
le th
o s e of hum
a n e nte ri
c vir u s e s T he e xte nt tow
h ichc o
l i
ph
age s a r e r el ia
b l
ein
d i
c ato r s of p
ath
o ge n r edu ctio n s
b y slud ge tr e atm
e nt pr o c e s s e s s u ch
G
e n e r alO
bj
e ctiv e sT
h i
s stud
y e x am i
n ed m
ale-spe c
i f
i c(
F+)
c o li
p hagein a c
tiv ati
o ni
n ala
b
-s c alet
h
e rm
oph
i l ic a n a e r ob
icd i
ge ste r a n d the pote ntial u s e of the s e p hage s a s a n in d ic ato r ofpathoge n r edu ctio n in the r
m
al pr o c e s s e s tom
e et C la s s A b io s ol i d r equir em
e nts Be c a u s e ofobs e r v e
d b i
-p
h
a sici
n a cti
v ati
o nk i
n eti
c si
n the rm
op hi
l ic a n a e r ob i
c di
ge stio n studi
e s(
A itke net al. 2 0 0 3
)
, F+ c oli
p hage s in r aw a nd tr e ated slud ge s we r e fu rthe r cha r a cte riz ed a s eithe r F+D N A o r F+ R
N A
, a nd
t he F+ RN
A c o li
ph
age s we r e fu rthe ri d
e nti fi e
d
a nd cha r a cte ri
z ed a s tow h
i
ch
gr o up theyb
el
o n ged
G
r o ups I a nd
I I I F+ RN
A a nd
F+ D N A c ol i
ph
age sw
e r ei
s olateda nd cha r a cte riz e
d
fr om
the u ntr e ated slud ge(
fe ed)
, the rmop h i l ic al l y d i ge sted slud
ge fr om
ac o nt
i
n u o u sfl
ow r e a cto r, a nd f
r om
th
eb io s o
li
ds e xpo s ed
to a the rm
oph i
li
c tem
pe r atu r ef
o rv a rio u s pe r
io
ds of ti m
ein
theb
atch r e a cto r. Be c a u s e of e vi
de n c e that the s e c ol i p hage sm
ayp
o s s e s sd i f
fe r e nth
e at s e n si
ti
vi
tie s
, t hei
s ol
ate s w e r ef
u rth
e r e v alu ated fo r
i
n a cti
v ati
o nk in etic s
i
n a lab
-s c ale he at e xpo s u r e e xpe r
i m
e nt at 5 3 "Cf
o r 5m
in ute s a nd
6 0 m in ute s.S pe ci f ic
O
bj
e ct iv e s1
E
v al
u ate th
ei
n a ctiv a
tio n
of m
ale-spe c
i fi
c c ol i
ph
ag
e sb
y t he rm
oph i l i
c a n a e r ob i
cd i
ge stio n(
T A D)
i
n c o ntin u o u s fl ow a nd batch r e a cto r s at 5 1, 5 3, a nd 5 5 "C
2. Dete r
m i
n e thei
n a cti
v atio n ki
n eti
c s ofm
ale -spe c
i f
i c c o l i p hage s at the rm
op hi
li
cte
m
pe r atu r e si
nb
atch e xpe ri m
e nts.3. Is o
l
atei
nf
e cti
o u sm
ale
-sp
e ci fi
c c oli
p hage s fr om
u ntr e ated
sl
ud
ge a nd
tr e ated4.
G
enoty pe a nd
/o r s e r oty pe F+ DN A
is olate s a s F d,M
l 3, o r C H and F+ RN A
is olate sa s gr ou p I, I I, I I I, o r I V .
4 Ev alu ate F+ R
N
A a nd
F+ DN A
c o li
ph
age s e n si
ti
vity to 5 3 °C
fo r 5m i
n ute s a nd
6 0m i
n ute s5 C ha r a cte riz e t
h
ei d
e ntitie s of the he at-r e sista nt a nd he at-s e n si
ti
v em
al
e-s pe ci f
i cba cte r
i
op hagef
r a cti
o n s o c c u r rin g in in a ctiv atio n r ate e xpe rim
e ntsi
n the d i ge stedb io s ol i ds
6. Dete r
m i
n ei f
pa rti
c ula r gr o ups o r ty pe s of
F+ R
N
A o r F+ D N A c ol i p hage s c o ul ds e r v e a s u s e
f
ul i
nd i
c ato r s of pathoge n r ed
u cti
o n si
n Pr o c e s s e s to Fu rth
e r Redu c ePathoge n s
(
P F R P)
ba s ed o n their in a ctiv atio n r ate s in th
e rm
oph
i l ic a n a e r ob icI I
R
E V I EW
O
F TH
E L I T ER A
T UR
EPri
m
a ry a n dS
e c o nda ry T r e atm
e n t a n d the Cr e at io n of S lud geW
he n r aw s ewagefi
r st a r ri
v e s at the P O TW
, it u s u al l
yp
a s s e s thr o ug h a s c r e e nin gd
e v ic e, c o n sisting of a s e ri
e s ofm
etal ba r s, to r em
o v e la rge obj
e cts that ha v e e nte r ed thes ewe r p
i
pe s a nd m i
g ht dam
age c om
po n e nts of
the PO
TW
Th
e s ewage the n fl ow
sin
to ag
ri
tc
h
am
be r, w he r e pa rticle s r o ug h
l y the siz e a nd de n si
ty o f s a nd
gr ain s s e
t tle o ut Rem
o v al of
th is c o a r s e grit is inte nded to pr ote ct the pu
m
ps in the r e st of
the system
W
ith la r ge obj
e ctsa n
d
grit thu s r em
o v ed
, the s ewage is pum
ped to a pri m
a ry s et tli
ng ta nk o r pr im
a ry clari f
i e r.In a ty p ic al tr e at
m
e nt p la nt,m
u ch of thefl
ow thr o ug h the r e st of the system i
s b y gr a v ity(
N
A S 19 9 6 ; Law
s 2 0 0 0)
In the pr
i m
a ry s et tl
ing ta nk, s et tle ab le o r fl o atab
le s oli d
s a r e r em
o v ed fr om
thes ewage
d
u ri
ng a pe riod
of abo ut 3 ho u r s. T he ta nkm
ay be cir c u
la r o r r e cta ngula r In ac
ir c u
la r ta nk, the s ewag
e e nte r s at the c e nte r a nd
slow l yfl
ow s to the ed gew
he r ei
t e xi
tsu n
d
e r a baf fl e In a r e cta n gl
e ta nk, the s ewage e nte r s at o n e e nd
a nd e xit
s at the othe rSo
li d
m
ate rials that fl o at to the s u rf
a c e du ri
ng the r e si de n c e ti m
e of
the s ew agein
the ta nk a r er e
m
o v ed b y am
e cha nic al ski
mm i
ng de vi
c e that pu she sfl
o ating ob
j
e cts to a hop pe r, fr om
w h ich they a r e pu
m
ped into th
e a n a e r ob icd
i ge ste r T he bot tom
of the ta n kis
in cl in ed, a nd
as
i m i
la r m e cha nic a
l de vic e
m
o v e s th
e sl
ud
ge that a c c um
ulate s o n theb
ot tom
towa rd
thed
e epe st pa rt of
the ta nk
,w h
e r ei
ti
sd
r awn of f
a nd
u s u al l yi
sp
um
ped
to th
e a n a e r ob i
cd i
ge ste r T hem
ate ri
al sk im m
ed
fr om
the s u rfa c e a nd fr om
theb
ot tom
o f the prim
a ry ta nki
si
s te rm
ed p ri m
a ry s ewage tr e atm
e nt Iti
s r eq
ui
r ed b y
fed
e r al law
that a PO
TW
op
e r ati
ng
w ith p
ri m
a ry tr e atm
e nt o n l y,m
u st r em
o v e at le a st 3 0%
of the BO
D a nd S S
fr om
the s ew ag
e(
Law s 2 0 0 0)
P hage r e
m
o v al is fairl y low a n d e r r atic du ri
n g th
e s c r e e ni
ng, g ri t cha
m
be r, a ndpr
im
a ry s edi m
e ntati
o n pr o c e s s e s He r e,m
o st vi
r u s e si
n th
e s ew
age a r e r edu c ed b y s et tl ingw
ith o nl y 0-3 0%
ef fi ci
ency T he
m
aj
ori ty of the vi
r u s e s r em
ai
n in the prim
a ry ef f lu e nt,b
uttho s e e nte ring the slud ge c a u s e the slud ge to ha v e a h i g her vir u s c o n c e ntr at
i
o n tha n th
e r aws ewage. In o n e e xpe r
i m
e nti
n wh i
ch p
hagef
2w
a s s e ed
ed i
nto t he wa stew ate r th
em
e a np
hage r edu ctio n wa s 3 7 1%
(
2 7 8-5 4 2%
)
i
n 2.5
m
i l li
o ng
al lo n s/ day b y pri
m
a ry tr e atm
e nt(
B it to n 1 9 8 7)
.I
f
s e c o nd
a ry tr e atm
e nti
s u s ed
, the ef f lu e nt
fr
om
th
e pri m
a ry ta nk f l
ow si
nto a s e c o nd
ta nk w
h
e r e bi
olog ic al
pr o c e s s e s a r e u s ed to r em
o v em
u ch o f th
e BO
Di
n the ef f
lu e nt. He r e ,o rga n
i
sm
si
n th
e ta nk
c o n s um
e the o rga ni
c s ub
sta n c e si
n the pri m
a ry ef f l
u e nt In th i
spr o c e s s, the c o n s u
m
e r o rga ni
sm
s gr ow
a nd m
ulti p l y, w h i le la rge pe r c e ntage s of the o rga nics ubsta n c e s a r e r e sp ir ed
A
s a r e s ult, th
e am o u nt of
pote nti
al l y o xi d i
z ab
lem
ateri
al i
n thew a ste is gr e atl y r edu c ed T he ef f lu e nt fr o
m
th is tr e atm
e nt pr o c e s s c o n sistsi
n pa rt of
theo rga nis
m
s thath
a v eb
e e n fe ed ing of
f the o rga nic wa ste s.M
o st of the b iom
a s s of the s eo rga n
i
sm
s c a nb
e r em
o v ed
b y tr a n sfe rri
ng th
e eff
lu e nti
nto a s e c o nd
a ry s et tl i
ng ta nk o rcla r
i fi
e r T he r e the bi
om
a s s s et tle s to theb
ot tom
in thef
o rm
of
af
lo e a ndi
s r em
o v edi
n am
a n n e r sim
i la r o r id
e nti
c al to that em
p loyedi
n th
e pri m
a ry ta nk
A po rtio n of the s e c o nd
a rys
l
ud gei
s the n r em
o v ed
fo r s epa r ate tr e atm
e nt a nd
di
spo s al, wh i
le the r em
aind
e r is r e cycl
ed
In the a ct
iv a
ted slud ge pr o c e s s,p
hage sm
ayb
e r emo v ed thr o ug
h: ads o rptio n to o re
m
bed
d ing wi
th in f lo e s,in a c
tiv atio n b y s ew
ageb
a c te ria, o r ing
e sti
o n b y pr oto z o a. Th
es e c o nda ry tr e at
m
e nt step ef f icie ntl y in a ctiv ate s p hage s, n o rm
al l y show ing gr e ate r tha n 9 0%
r e
d
u ctio n
of infe ctivity.O
n e stud y o f p hage r em
o v al thr o ug h a ctiv a
ted
slud ge fo u nd theef
f
i ci
e n c y r a n geb
etwe e n 9 6-9 7.3
%
, w hi
le the e nte r o vi
r u s e s a v e r aged 9 2%
r em
o v alef fi cie n c y
(
B it to n 19 8 7)
. Ad
d itio n al l y, w he n p hage s a nd E. c ol i s am
p le s we r em
o nito r edwe ek l y fo r a o n e
-ye a r pe r
i
od, itw
a s di
s c o v e r ed that p hage s w e r e r em
o v ed thr o ug h a ctiv atedslu
d
ge pr o c e s s e s ef fi
cie ntl y a nd
w e r e bet te r ga uge s of
e nte r o vi
r u s e s t ha n w a s E. c ol i.T he r
m
op h i l icA
n a e r ob ic D i ge st io nAn a e r o
b
ic di
ge sti
o nis a
m
o ng them
o st c om m
o nm
ethods of
tr e atin g pri m
a ry slud gea n d the wa ste
b
iom
a s s fr om b i
ologi
c al tr e atm
e nt pr o c e s s e s s u ch a s a ctiv ated slud ge T hea n a e r ob ic d i ge ste r is a clo s e
d
, u s u al l y cy l in dric al ta nk, w he r e it pr o vi de s fo od fo r a spe cia
lcla s s o f
m i
c r o o rg
a ni
sm
s that c a r ry o n th
ei
rm
etab
ol i
c a ctiv
i
tie s
in
th
e ab
s e n c e of
o xyg
e n ,i
.ea n a e r o
b
ic al l y. T he pr odu cts of the a n a e r ob ic di
ge ste r a r ed
i ge sted slud ge(
b io s oh
ds)
, as upe r n ata nt fl u i d, a nd ga s e s T he d i ge sted slud ge is r elativ el y stab le a nd
i
n o f fe n siv ec o
m
pa r ed
to th
e u ndi
ge sted
pri
ma ry a nd
s e c o nd
a ry slud ge s. Fu rthe rm
o r e, its v olume is o nl y
abo ut o n e-th ir d t
h
at of thepr
i m
a ry a nd
s e c o nda ry slud
ge s Th i
s r edu ctio nin
v olum
ei
sa ch
i
e v ed
bothb
y th
e c o n v e r sio n
of s om
e of the o rg
a nic s in the r aw slu d ge to ga s e s,(
pri m
a ri l
ym
eth
a n e a nd
c a rb
o nd i
o xi d
e)
,b
y a n a e r ob i
c c atab
ol i
sm
, a nd b
yd
ew ate rin
g
th
eslud ge to r edu c e
i
tsm
oi
stu r e c o nte nt. T he r aw
slud
ge ty p ic all
y ha s am
oi
stu r e c o nte nt o f 9 4
-9
9% b
y w ei
gh
t(
1-6
T he a n a e r ob ic d ige ste r
i
s in v a riab ly he ated to spe ed up them
etabohc r ate o f them i
c r obe s Fo rm
e s op hi
li
c a n a e r ob i
c di
ge sti
o n, ope r ati
ng tem
pe r atu r e s a r e u s u al l yi
n ther a nge of 2 7-3 5 °C
. Fo r the r
m
op h i l ic a n a e r ob ic d i ge stio n, ope r atio n te
m
pe r atu r e s a r e betw e e n5
0 a nd
7 0°
C
, alt
h
o ug h u s u al l y th
em
a xi m
um
tem
pe r atu r ei
s n om
o r e tha n 6 0 °C
(
Zh
o u a nd
M
a vinic 2 0 0 3)
T hem
etha n e ga s pr odu c ed in the d i ge ste r is adequ ate to pr o v i def
u el to he att
h
e d i ge ste r to the de sired tem
pe r atu r e T he e x c e s sm
etha n e pr odu c edi
n the d i ge ste r isb
u r n ed
ei
the r a s a wa ste pr od
u ct o r of
te n c o upl
ed
to the pr od
u cti
o n of
el
e ctri
cit
y. Th
es upe r n ata nt f lu
i
df
r om
thed i
ge ste r r etai
n s s om
e u nd
e si
r ab l
e a nd
ob
j
e cti
o n ab l
e pr ope rti
e s(
h
i g h o rga ni
cm
at te r a nd odo r)
a ndi
s u s u al l y r e cycl
ed thr o ug h the s e c o nda ry tr e atme ntp
r o c e s s. Th
e o nl y pr odu ct o f th
e di
ge ste r that r equ
i
r e s di
sp
o s al is the stab i
li
z ed sl
ud ge.In 1 9 9 3,
U
S E P A la u n ch
ed the n e ed
fo r spe ci
al d isi
n fe ctio n ofb i
o s ol i ds s u ch a sd i
ge sted s ewage slud
geb
efo r eit
c a n bed
epo si
ted o n agric ul
tu r al la nd
s o r ha v e othe r le s sr e str
i
cti
v ed i
spo s al opti
o n s(
US
E P A 19
99
)
M
e s oph i h
c di
ge stedb
io s ol i d
s a r e cla s si fi ed a sC
la s s B qu alit
y a nd h
a v e v e ry r e stricted
u s e.S l
ud
ged
i ge stio n at the rm
op hi
li
c tem pe r atu r e so r
b
y othe r adv a n c ed
pr o c e s s e si
s n e c e s s a ry tom
e et n ew sta nda rds fo r C la s s A Bi
o s ol i ds thatal low fo r
l
a nd ap p li
c atio n a nd othe r le s s r e str ictiv e di
spo s al optio n sT
h
e rm
op h i li
cd i
ge sti
o n c a n be c a r ri
ed
o ut eit
h
e r a n a e r obi
c al l
y, o r a e r ob i
c al
l y. La rg
e rtr e at
m
e ntf
a ci
li
ti
e s te nd
to ope r ate a n a e r obi
c al l
y(
e gG
r e ate r V a n c o u v e r A n n a ci
s Isl
a nd
W
a stew ate r Tr e atm
e nt P la nt, 45
0M
L / day f low) (
Kr ugal et al
1 9 9 8; Z ab
r a n sk a et al 2 0 0 3)
S m
al le r o rm
ed
ium
siz e fa ci l
iti
e s te nd
to ope r ate a e r ob
ic al l y(
e.g BritishC
olum b i
a 's
W
hi
stle rW
a stew ate r Tr e atm
e nt Pl
a nt, 1 2.5M
L/ d
ay f low
)
(
Z ho u a ndM
a vi
n ic 2 00
3)
T hea
d
v a ntage of
the a n a e r ob i
cd i g
e sti
o n of
sl
ud
gei
s pr od
u cti
o n of
e n e rg y a sb i
oga s(
Zabr a n sk
aet al. 2 0 0
3
)
. Th
ep
r od
u c ed
e n e rg
y c a n n ot o nl y s up
p l y the e n e rg y n e ed
ed
fo r th
e slud getr e at
m
e ntb
ut als o pr o vi
de a s ub
sta ntial pa rt of t he e n e rg y u s ed b
y the wh
o le tr e atm
e nt p la ntT he t
h
e rm
oph i l i
c tem
pe r atu r e r a nge of
th
e a n a e r ob i
c pr o c e s sb
ri
ngs a hi
gh
e r ef f i
c a cyi
n th
edegr a
d
ati
o n of
o rga nicm
at te r a s s o ciated
w ith a h i g he rb
ioga s pr od
u cti
o n a nd
a lowe r c o nten to
f
v olati
le s ol i d
si
n th
edi
ge sted
sl
ud g
e, wh i
ch
r epr e s e nts al
e s s e r am
o u nt of
o utput stab i l i
z ed
slud ge w ith bet te r h y g
i
e nic qu al ity(
Zab
r a n ska et al. 2 0 0 3)
.T he ope r at
i
o n al
tem
pe r atu r e of
th
e rm
oph i l i
c a n a e r ob i
c di
ge sti
o n(
TA D
)
i
s u s u al l
y5 5 °
C I
m
po rta n t r e a s o n s fo r ap p l y in g the rm
op hi
l ic tem
pe r atu r e s a r e th
e bet te r s a ni
ti
zi
ngef fe ct o f the h i g he r pr o c e s s te
m
pe r atu r e a n d the ab i li
ty to u s e lowe r r ete nti
o n ti m
e s th
a n u s edfo r
m
e s op h i hc d i ge sti
o n B y up gr adi
ng
e x istin gm
e s op hi
li
c di
ge ste r s to the the rm
op hi
l icte
m
pe r atu r e r a nge, th
edi
ge stin g c apa ci
ty c a n be do ub
led a nd c o n sid
e r ab
le r edu ctio n o fpatho
g
e n c o nte nt c a nb
e obtain ed
(
Kr ugal et al. 1 9 9 8 ; Zabr a n sk a et al
. 2 0 0 3, Zabr a n ska et al
2 0
0
3)
Fo r pr a cti
c al ope r ati
o n of f
ul l-s c alep la nts, a te
m
pe r atu r eb
etwe e n 5 2 a nd 56
°C i
spr efe r a
b
le, al low in g a sl i g ht v a ri
ati
o ni
n the tem
pe r atu r e wi
tho ut fatal
c o n s equ e n c e s fo r s om
eof the a ctiv e
m i
c r ob
e s(
A hri
ng 1 9 9 4)
. T he s e the rm
oph
il i
c tem
pe r atu r e s ki
l lm
o st path
oge ni
cba cte r
i
a a ndm
o st vir u s e s Howe v e r , s om
e he at-r e s
i
sta nt vir u s e s s u ch a s thepa r v o v ir u s w i l l
n ot be k i l led at a d i ge stio n te
m
pe r atu r e of 5 5 °C(
Lu nd
et al 1 9 9 6 a n d B o r o v e c et al. 1 9 9 8)
.T he r e
f
o r e, in c r e a s ed d
em
a n dsf
o r pathoge n k i l l du ri
ng a n a e r obi
c d i ge sti
o n of slud ge c o u l din c r e a s e the inte r e st fo r d
i
ge stio n at hi
g he r tem
pe r atu r e s of 6 0-6 5 "
C
to e n s u r e that th
em
ate ri
al i
s pr ope rl
y s a ni
tiz ed f
o r al
lowi
ng u n r e stri
cted
u s e a s a fe rti l i
z e r o n fa rm
la nd
(
A hri
n g2 0 0 1
)
In a n e v alu at
i
o n o f a T A D at Li
o n sG
ate in Va n c o u v e r, they s u c c e s sful l y tr a n siti
o n edfr o
m
am
e s op hi
li
c to the rm
op h i hc pr o c e s s. T hey fo u n
d
that a tw
o-stage the r
m
op h i li
cpr o c e s s, ope r at
i
n g at 5 5 "c ol
i f
o rm
(
F C)
r equi
r em
e nts w ith n o n-dete ctab le
l
e v els ofS
al
mo n el la ba cte ri
a. Af
te r the fi r ststage,
m
e a s u r em
e nts a v e r age sli
g htl y ab
o v eC
a s s A le v els of F C of 1 0 0 0M
PN
/ g T S a nd
afte rthe s e c o nd stage, F C
m
e a s u r em
e nts a r e r eli
ab l y below the fe c al c oli
fo rm
up pe r l im
it fo rC
la s s A r equi
r em
e nts. V olati
le s oli d
sd
e str u cti
o n a nd m
etha n ega s pr odu ct
i
o nw
e r e sli g
htl yh i g he r tha n in the pr e v
i
o u sm
e s op h i li
c ope r ati
ngm
ode, a nd
ope r ato r s r epo rted thatthe r
m
op hi l i
cb i
o s o li d
s a r e e a si
e r tod
ewate r a nd h
a nd l
e. T he vi
s u al ap pe al
of thethe r
m
op hi
li
c b io s o l id
s a s a n agri
c ul
tu r al am
e ndme nti
s als om
u ch i m
pr o v ed, ha vi
ng al i
g htgr a n u la r te x tu r e
(
K
r ugal et al 1 9 9 8)
.T
h
e stab le a nd
ef fi cie nt ope r ati
o n of the the rm
op h i l ic a n a e r obi
c di
ge ste r str o n g l ydepe n
d
s o n th
e a cfi
vi
t y of
a n a e r ob i
c c o n s o rti
ai
n th
ed i
ge ste r(
Zab
r a n sk
a et al
2 0 0 3)
. T he r ei
s al
a ck
of
u nd
e r sta nd i
ng o f thed i f f
e r e n c e sb
etw
e e nm i
c r o o rga ni
sm
s a cti
v e at thet
h
e rm
oph i l i
c tem p
e r atu r e s c om
pa r ed
tom
e s op hi l i
c tem
pe r atu r e s.S
ewage sludg
e o r oth
e rty pe s of wa ste w i l l
m
ai
nl y ho u s em
e s op h i li
cm
ic r obe si
n clu d ing a n a e r ob
e s(
A hrin g et al
.2 0 0 2
)
. H ow
e v e r, th
e n um b
e r s of
th
e rm
op hi l
e s a n d e spe ci
al l
y s om
e spe ci fi
c gr o ups s u ch a sa c etate-ut
i
l izing
m
etha n oge n s, pr op io n ate -degr a
d
e r s o r c el lul
o s e-d
egr ade r s w
i
ll
ofte nb
e v e rylow o r the s e gr o ups c a n e v e n be
m i
s si
ngi
n the w a ste(
Ah
ri
ng 1 9 9 4)
. T he o c c u r r e n c e of
the rm op h
i
le sw i
l ld
epe nd upo n theh i
sto ry of the wa stem
ate ri
al a nd the r efo r e s om
em
ate rialw i
l l
s om
etim
e s ha v e u npr ed ictab
l y hi
g h n um
be r s of,f
o r in sta n c e, the i t n op h i l icm
etha n oge n s(
Ah
ri
ng
2 0 0 2)
.C la s s A B io s ol i ds a nd L a nd A p p l ic at io n of Sewa
g
e S lud geA s state
d
ab
o v e, the r ei
s c o n si d
e r ab
lem
oti
v ati
o n fo r ap p l yi
ng
sl
ud ge to la nd
Th
eE P A
fi
r st pr om
ul gated
c ri
te ria fo r la nd
ap pl
ic ati
o n of
s ewage sl
ud ge to c r op la nd i
n 1 97 9
, a nd
c u r r e nt sta nda rds fo r the u s e a nd d
i
spo s al of s ewage slud ge w e r e in sti
tutedi
n 1 9 9 3(
U S
E P A1
99 9
)
, w hic
h a r e c om m
o nl y r efe r r ed to a s the "Pa rt 5 0 3
Sl
u d ge Rule. "T h
i
s r ule puts slud gein
to o n e o f two c atego ri
e s : Cla s s
A a ndC
la s s B .C
la s s A slud geis s a
f
ef
o r dir e c
t c o nta ct a nd
c a n
b
e u s ed
in a n u n r e stric
ted m
a n n e r How e v e r,C la s s
B slud gei
s of l
e s s e r qu al i
ty a nd i
tsu s e
i
s r egu lated
wi
th m
o r e stri
nge nt sta nd
a rd
s pe rtain
i
ng to t he li m i
tati
o n s of d i
spo s al
optio n s
a nd r e strictio n s o n a c c e s s o r c o nte nt. T he ge n e r al cri te ria fo r pathoge n s a nd fe c al c o l
if
o nn sin
C l
a s sA b i
o s oh d
s a r e s um m
a ri
z ed i
n T ab
le 1.T ab le 1. Pat hoge n a nd Ind ic ato r C ri te r ia fo r C la s s
A
B io s ol i dsIte
m
Cri
te ri
o nV ia
b
le helm in
the s o v a < 1 pe r 4 g dry s oli
dsEnteri c vir u s e s < 1 pe r 4 g dry s ol i ds
Sal
m
o n el la spe ci
e s < 3 cfu pe r 4 g dry s olid
sFe c al c ol i fo r
m
< 1,0 0 0 pe r g s ol i dsB
e c a u s e slud gei
s a pote ntial s o u r c e of n utrie n
ts a nd
a go od
s oil
c o nd i
tio n e r,la n
d
ap p
l i
c ati
o n of s ew age slu d geis a v e r
y pr a ctic al a nd de sir a
b lem
e a n s of
di
spo s al Cu r r e n tl yabo ut 6 0
%
of them
u nici
pal s ew
age slud ge in the U S is n ow la nd ap p l ied(
N
A S 2 0 0 2)
O
n ei m
po rta nt c o n sid
e r atio n in the la nd ap p lic a
ti
o n of slud ge is the fa ct that slu d ge c a n betr a n spo rted e c o n o
m
ic al l ym
u ch gr e ater d ista n c e s tha n w a stew
ate r Fo r e x am
p le.N
ew Y o rkC i
ty 's tr e ate
d
slud
gei
s c u r r e ntl
y sh i
p ped
to n o rthe a ste r n T e x a s a nd
e a ste r nC
ol
o r ad
of
o rc r op
la n
d ap p lic a
tio n
. An othe r c o n si d
e r ati
o ni
s that th
e u s e of
s ewage slud ge ha s be e n v e rys u c c e s sful in the r e sto r atio n o f stri p-
m
in ed la n d. Estab l ish ing v egetatio n o n s u ch la nd is
e xtr e
m
el
yd i f f
i c ult du e to the la ck of n utri
e nts, low
o rga nicm
at te r c o nte nt, low p H, loww ate r r ete ntio n a n