Document aBrpQ2RR5aGkydYJyy2BQwNe9
MAatyta4,ch20m0e0:tnotEnLevtitreorntmoenCt.aAluSetruDdaietsedon Perfluorooctanesulfonates (Post-1875)
IPhysicalichemical Properties
Laboratoroyr Completion zy
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000172
ENVIRONMENTAL FATE AND TRANSPORT
sTohiilsadsescotripotniopnressteundtisesi.nDfeorgmraatdiaotnioanndsttuedsitesreisnucltlsudferhoymdraobliyostiics,,
and biotic degradation photolysis, and
and
biodegradation. Much of this work is in progress with final reports scheduled for the June
to August, 2000 timeframe.
As these studies progress, there are certain key findings that can be presented as preliminary results:
1. There has been no indication that perfluorooctanesulfonate undergoes any degradation from hydrolysis, photolysis, or biodegradation mechanisms.
d2.etIenctaleldhaysdraoldyesgirsadaantdiopnhoptroolydsuicstsitnudaineys,cpoenrcflluusoirvoeoecxtpaenreismuelnfto.naTtheihsapsrneoltimbieneanry ffilnudoirnogchceamlliscailnstotqoupeesrtfilounortohcetaansessuumlpftoinoanteo.f expected degradation of other
S3.trIuncttuhreesotfudtihees sfpoeccuisfiecd ionnduhsytdrrioallyasinsd ocfofnlsuuomreorchpermoidcuacltsp,olitymhearssbteheantdfeotremrmtihneed
that these following
materials are relatively half-lives are estimated
stable in the environment. for various polymers:
For
example,
the
POLYMER
HALF-LIFE
Acrylate and ester
1-5 years
Polyethylene glycol based
3-50 years
Urethane
>500 years
For hydrolysis to occur, polymers must be subjected to an aqueous environment, `which is not expected to occur in a municipal or industrial landfill w4.ilRleplhaottiovleytzoepthootcoalrybsoisx,yltahteecsutrrruecntturdeast.aThsuegsgeessttsruacthuyrpeosthheasvies mthuacththdeisfefemraetnterials properties then sulfonates in that they are much less bioaccumulative in ecological species. Additional discussion of these results and ongoing studies will be presented in subsequent submissions and reports.
000173
EFT)
SOIL ADSORPTION
:
TEST SUBSTANCE
Identity: Perfluorooctanesulfonate; may also be referred to as PFOS or FC-95. (1-Octanesulfonic acid, 1,1,22,33.4,4,6,5,6.6,7.7.8.8,8heptadecafiuoro-, potassium salt, CAS # 2795-39-3)
Remarks field: The test substance is a white powder of upnecrhcaurrarcetnetrpirzoedcepduurirteys. aTnhdisbetessttianvgaiilsabbeleinpgrarcetpiceeast.ed
METHOD
Method: ~~ Adsorption-Desorption study using the approach
GLP (YIN): rNeocommended by the U.S. EPA for pesticide registration Year (study performed): 1978 Statistical methods: Statistical analysis and plotting of the data was done with the MINITAB package of the 3M TRAC computer service. Temperature: ~~ 16-19C Stock and test solution preparation: Test solutions were made by
diluting a stock solutionof "C-labeled Perfluorooctanesulfonate. The type
of solvent used to make the stock solution is not noted, nor is the activity ofthe radio-labeled test substance. Remarks field: The Brill sandy loam soil was characterized as having w5i7th%psHan6d.,53a6n%d csialtt,io7n%exclcahya,n2g.e5c%aopragcaitnyicofma1t5t.e3r,me1q..5/%10or0gganmisc.carbon, Standard solutions of the 14C-labeled compound were prepared in D.1. `waterat concentrations of 262 mg/L, 158 mg/L, 90 g/L, 51 mg/L, and 28 mg/L. Twenty-five miofeach solution was shaken with duplicate 5 gram samplesofthe sail in a 50 ml polypropylene centrifuge tubes for 24 hours on a wrist shaker at room temperature (16-19C). Desorption extraction were performed with D.1. water after the adsorption phaseofthe experiment. The samples from the adsorption and dmeisnourtpetsi,oanfteexrpwehriicmhe,ntthsrweeeraelicqeunottrsioffugeeadcihndsiuvpieduranlaltyaantt5s0o0lu0tiropnmweforre10 prepared for scintilation counting. From the raw counting data, compound concentrations were calculated for al of the supematant solutions.
RESULTS
00174
Ki 099 (N=1) Koc: 66 Remarks field: The linear shapeofthe adsorption isotherms indicated that perfiuorooctanesulfonate adsorption on soil would be independent of concentration. + The study report had calculated a soil / organic carbon partitioning coefficient of 45. After review, it was determined that the value should have been 66 based on the formula (Kee = K' x 100/1.5(% organic carbon); K'= (m)/Co).
CONCLUSIONS
The study substance is expected to exhibit high mobility in the kind of soil tested and would move with the groundwater. Submitter: 3M Company, Environmental Laboratory, P.O. Box 33331, St. Paul, Minnesota, 55133
DATA QUALITY
Reliability: Kiimisch ranking 2. This study lacks detail on the stock solution and the purityofthe radio-labeled test substance. Additionally, `some calculations have questionable reliabilty.
REFERENCES
3M Technical Report "Adsorption of FC 95 and FC 143 on Soil." SK. Welsh, Project 9970612633 Fate of Fluorochemicals, Report No. 1, Feb. 27,1978
OTHER
"
Last changed: 5/2/00
000175
SUMMARY OF THE SOIL ADSORPTION STUDY OF THE
POTASSIUM SALT OF PERFLUOROOCTANESULFONIC ACID
.
.
Soil adsorption-desorption studies were conducted to indicate the mobility of potassium perfluorooctanesulfonate in a sandy loam soil. The approach used was that recommended by the U.S. Environmental Protection Agency for pesticide registration.
The Brill sandy loam soil was characterized as having 57% sand, 36% silt, 7% clay, 2.5% organic matter, 1.5% organic carbon, with pH 6.5 and cation exchange
capacity of 15.3 meq./100gms. Standard solutionsofthe "C-labeled compound were
`preparedin D.Iwateratconcentrationsof 282 mg/l, 158 mg/l, 90 mg/l, 51 mg/l, and
28 mg/l. Twenty-five mlofeach solution was shaken with duplicate 5 gram samples of
the soil in a S0'ml polypropylene centrifuge tubes for 24 hours on awrist sheker at room
temperature (16-19 C).
'
Desorption extractions were performed with D.L. water aftr the adsorption phase ofthe experiment. The samples from the adsorption and desorption experiments were centrifuged individually at 5000 rpm for 10 minutes, after which, three aliquots of each supematant solution were prepared for scintillation counting. From the raw counting dats,compound concentrations were calculated for all ofthe supematant solutions.
R
_--
The linear shape ofthe adsorption isotherms ifificated that potassium
perfluorooctanesulfonate adsorption on soil would be independent of concentration. A soil adsorption coefficient (K) of 0.99 indicated that this compound would be mobile in this kindofsoil and would move with the groundwater.
A soil organic carbon partitioningcoefficient(K..) was calculated in this report to be 45. However, afer closer examination the K. value should be 66 (K,, = 100 * K / (1.5% organic carbon). Again, this value indicates high mobility in this kindofsoil.
000176
July 2, 1998
MICHIGAN STATE UNIVERSITY eTevvLeoea,m
yay 15, 1993
roe aston
25c. cCtoomompatbneye.suaso, w2t-38-00 Hora sili eae De. Bowe ET SeaectnoinstsEITaie roemasy rFeoviTewaN TpovcoorFmtonorT .testtelreuagaahlrcicdaishn,yrg otf"ehFevlcieshasieneneeeInoredeMniv.viiTebawucnhttnhticsslbuaIddntfeRorarspioerstcnisdo,n AEdRoEEEhtahevotevceedesnoemmrmeeasnntisattdtiahoFensasttbeaaTtiosesroictciftobigoeyeotvsirpoTeonesesroaetfracrshTcoohuaperopePofesipseorln.potdssu0cvbeen3sHochioenusLdisnsssionarfcdouarnnmscaetion Jly acoLnyEsuicaSinsgEffaontEfFooxnecsheoewforakeeieirafto]araeSaadd.copOedsaecseIatiiaoRn3,o2f00r.o0p0eck(schephwossanosde JPAR Sincerely, J4
S FroetaesoAr. Boyd, Ph.]
MSUisanAffmationActionsOportmityntiuion
00177
ReviewofTechnical Report Summary `AdsorptionofFC 95 and FC 143 in Sail Material and Methods Should give recoveriesofcompoundins blank (no-s0i) experiments. States that polypropylene: 501s less than glass on polyethylene, but doesn't givae numerical value. `The large headspace (25 ml in a 50 tube) is undesirable; any lossesofthe "C-label, e.g., from volatilization or sticking to the tube, will inflate the sorption coefficient since the method c`caolnccuelnattreastitohnes.amAolusnottsheor2b4edhobuyrdmiiffxeirnegncpeerbieotdweseenemtshearibniittriaarly.andWefrinealexeqpueirliimbernitusm dsoonleutifoonr different periods of time 10 establish that equilibrium was reached within 24 hours? Detailsonthestocksolutionarelacking. Whatsolventwasusedandwhatisthespecific activity and radiochemical puriyofthe "C-FC 95.
`sToihle aisdewaeollf uassiwnagtaerc.ottTohnesw~a2ba0f%terofthleessdrdaeicnrienagsestineispsoluuntuesucaoln.cenHtorpaetfiuolnldyuie s igor" wowvte ashighas I'dlike osee it. A SO%orgreater decrease wobueblettder =
This section generally lacks detail that would normally be required for \ NE
Results and Dicscuussssion
wep
`The linearity of the isotherm has been shown over the concentration range us 2
cdoenmcoennsttrraattieontshatthattheapepnrtoiraechistohtehewramteirs sloilnuebai,littyhoefltihneearciotympmouusntde.xtDenodytooueqkunio
a
of FC95 or FC143: If not, how were the initial solution concentrations selected
`The sorption coefficient (K)ofFC 95 appears to be about 1 as indicated. The organic matter normalizedsorptioncoefficient(Ka, = K/f,2isKoy = 110.025 = 40,orloKge, = 1.6. This isasoil sorption coefficient intermediate betweenbenzeneand toluene. It would 10 examine some additional soils to confirm this Kos value. Generally, the Ko convergewithin afactorof 2to 3 fordifferentsoils. This would increase my coi accuracy of the one measured value.
I've spot checked the soil concentrations of FC-95 for both the sorption a ~~ experiments and 1 get essentially the same values. The calculations look good.
The K values for FC 143 is lower than FC 95 indicating that it probably has a solubility. The hystersi inthedesorption isoitsshurperirsinmg, and has been ovt `The sorption isotherm is linear indicatinga single sorptive process. The conclusion regaraing c"othnrveeersdeifafterleontwebrincdoinncgenmtercathiaonniss"miss .v.e.rwyitshpescturloantgievre bbiansdeidngonatthhiegshienrglceonecxepnetrriamteinotn.s aInfdotnhee examinescolumn I "AmountDesorbed2s a PerocfAemonuntt Adsorbed" the values range from
000178
26 10.212 percent,so t's pretty inconclusive. There is afairlygood discussionofhysteresis in
J. Environ. Qual. 12:325-330 by Koskinen and Cheng who observed this phenomena for the
`weak acid pesticide 2,4,5-T. The causes of hysteresis are varied and complicated and may
ainncdl/uodrecmhiecmriocbailalprdoepgerratdiaetsioofn tohfe tshoeilc-osomlpuotiuonndsydsutreimn.g dFeosrorepxtiaomnp,lea,nddecshoarnpgteiosniunstihneg pdhiystsiilclaeld
cwoautledr n(oatsbiestohbeaciansede. hTehrei)sccaounldcaruesseulqtueinncshoiinlgdoisfpreardsiiooanctsiovittyhaitn asoclluetaironsaupnedrnoatthaenrtprsoolbulteimosn
leading to error.
_
`The "material balance" as presented in the report is a little misleading. To obtain a material balance you should measure the amountof "C-activity insoilat the end oftheexperiment, and add it to the measured solution concentrations.
General Comments. The K,, values calculated here use an organic carbon content of 2.2%
`whereas the value stated in the Materials and Methods is 1.5%?
`TTahteerwavtaelruesoilsubwirliotniges. arIef ctihteedsoalsub3il0i0timesg/arLeftorrlFyCth9a5t adinfdfe>rent2,0gt/heLnfotrheFsCor1p4t3i.ve Spurropeelrytitehse
should be vastly different, which they are not. If FC143 has a solubility of >20,000 mg/L, then Iwould expect no sorption. This value must be erroneous.
Recommendations:
1 Obtaining K, Ke, values on additional soils. Determine if K, is relatively constant.
2. Obtain a true mass balance by measuring "C-activity in soil and solution phase.
3. Interpret desorption datamorecautiously.
4 Get correct value of water solubility of FC 143.
000179
: Hi AoE
i.
` Forher1 IA
TECHNICAL REPORT SUMMARY
2/27/78
ee 5 70: TECHNICAL COMMUNICATIONS CENTER -- 201-208 (Inport. port seinndonbthios ofpp, ndtwo coprso 705) Co
R
Faattee of Fluorochea-hemicals
leew| |
_ _~
| GQ Fif
m &! ge ta , ory |i
| TFeoe gaoc. wmmeerCe |
secpten kein SEW de aii Adsorption of FC 95 and FC 143 on soil
-- hou D. L. Bacon
1| (1) (9a") peii
ove. Sa [5 Ging a
:
savs73, 47708
| PE rm sol14l
ny BO cova si rereier |REED
-
|
Eoewonrnoseaiomsa.w CunENT GRECTIVE:
>
To obtain an indication of FC 95'and FC 143 mobility in sandy loam
soil.
BE & PC - Div.
DFIUOROChemical Soil Adsorption Nobility
[merA on ATTCRAnCTn. (R0a2:50 ard Toeoat orator nna TeeCommnionsGrr
As a part of the Fate of Fluorochemicals Project, an indication
of mobility of FC 95 and FC 143 in sandy loam soil was desired.
Adsorption-desorption experiments (after Davidson, 1976, and Hamaker,
1975) along with water solubility data can provide such information.
The adsorption coeffi@nts for FC 95 and.FC 143 were deternined to be
0.99 and 0.38, respectively. For FC 95 adsorption and desorption
could be described by a single valued function while for FC 143,
they could not. Based on these data, both compounds would be
judged mobile in the sandy loam soil used in this study.
RE tomae SE)
.
00180
PERLE
2
TEE
a
D
CONCLUSIONS
'
Adsorption coefficient for FC 95 and FC 143 were 0.99 and 0.38,
respectively. For FC 95, adsorption and desorption could be described by a single valued function while for FC 143, they could not, Considering adsorption coefficients, desorption characteristics and water solubilities,
both compounds would be judged mobile in the sandy loam soil used in this study.
:
INTRODUCTION
+
As a part of the Fate of Fluorochemicals Project, an indication of
mobility of FC 95 and FC 143 in sandy loam soil was desired. Adsorptiondesorption experinents (after Davidson, 1976, and Hamaker, 1975) along with water solubility data can provide this indication of mobility. This approach yi usd by the Uo So EPA dn pesticide segistration requirements.
-
MATERIALS AND METHODS
Duplicate S-g samples of air-dried Brill sandy loam soil (57% sand,
36% silt, 7% clay, 2.5% organic matter, 1.5% organic carbon, with pH 6.5 and
C.E.C. of 15.3 meq./100g) were shaken with 25 ml of solution in 50 ml. poly-
propylene centrifuge fubes for 24 hours on a wrist action shaker at room temp.
(16-19C). Polypropylene tubes were used because they were found in separate
experiments (3M Tech Notebook #470673, C. H. Schrandt) to absorb less FC 95
and FC 143 than glass or polyethylene tubes. Solutions were made by diluting a stock solution of each chemical.
Concentrations of C-labeled FC 95 were 282 mg/1., 158 mg/1., 90 mg/1.,
$1 mg/1., 28 mg/1., (100%, 56%, 32%, 18%, 10%, 1% of stock). Concentrations
J of Mc.1abeled FC 145 were 523 ng/1., 293 mg/1., 167 ng/1., 94 mg/1., 52 mg/1.,
and 5.2 mg/1.
.
000181
TR
:
d
After shaking the initial solutions as well as the three
desorption extractions with deionized water, the samples Were centrifuged
at 5000 rpm for 10 min, and three aliquots of each supernatant solution
vere taken for scintillation comting.
After the adsorption step, 22.5 ml of solution were recovered, Therefore, it was assumed that 2.5 ml of liquid remained with the soil in
each step and this amount was accounted for in the desorption calculations
(see Results and Discussion section).
In the FC 95 experiment, the supernatant liquid was simply drained
:
Off at each step and the next 25 nl of 1iquid were put into the tubes.
In the FC 143 experiment, the supernatant liquid remaining after the
draining step was sbsorbed with a cotton swab before putting the next
)
25 n of liquid into the tubes.
The procedures for the FC 95 and FC 143 experiments were recorded
in 34 Technical Notebook #40673, p. 49 and p. S51, respectively.
From the raw counting data, disintegrations per minute (DPM) and
FC 95 and FC 143 concentrations were calculated for all of the supernatant
solutions.
Statistical analysis and plotting of the data was done with the
MINITAB package of the SM TRAC computer service.
RESULTS AND DISCUSSION FC 95
Adsorption data for FC 95 are presented in TABLE I and FIGURE 1.
Comparing the regression equation of the adsorption isothern (FIGURE 1)
)
x/B = -0,20 + 0.99C with the Freundlich equation x/m = Kc'/N, it could ve
seen that the adsorption coefficient, K, equaled 0.99 and the exponent, N,
equaled one. The linear shape of the adsorption isotherms (N=1) indicated
00018x%
KEELE
`
I
that FC 95 adsorption on soil would be independent of concentration. The
low adsorption coefficient (K=0.99) indicated that FC 95 would be mobile,
i.e., it vould move readily with the ground water through this sandy loam
soil.
TABLE 1
FC 95 ADSORPTION DATA
A
B
c
Initial Fe 95
Equi. Conc.
* Beaoued
.
Cone,. mg/l
C, mg/l.
(AF To
218528..20
90.0
28$1..00
)
2.8
213303..29
1157..11
7462..90
1174..86
22..10
2271.0
o Total FC 95 (IAnxIn0i.t0i2a5l lSiotelr'sn)
7.0500 23..29550000 10..27705000 0.0700
E SoTlo'tnalatFCEqu9i5l.i,n mg _(B x 0.025 liters)
35..3845755000 11..9025205000 00..5055205000
F onFCSo9i5l,Adxs/onr,bedug/g (--8) x 10 vy/eg
12490..08 4655..73 293..58
: Desorption data for FC 95 are shown in TABLE II and FIGURE 2. For comparison, desorption isotherns for the pesticide fluoneturon are given in FIGURE 3. For clarity FC 95 desorption isotherns are not drawn in FIGURE 2. However, all of the data points lie very close to the adsorption isotherms
)
indicating that adsorption and desorption could be described by a single-valued
function with desorption coefficients, K', equaling the adsorption coefficient,
*
00183
Ed SpE
3
Y
240
3g
180
Rr
&
120
Lo
3 b
i
60
0 o
A
:
A
,
A
Regression Eqn.:
R-Squared =
Y = -0,29
0,985
+
0,99
X
A = Actual Data Points
B = Predicted Y Values
@ 120 180 210
300
Equil, Cenc., C, mg/l
FIGURE 1
FC 95 Adsorption Isotherm
-
This, along with the observation that approximately all of the adsorbed
FC 95 was subsequently desorbed (TABLE II, Column H) indicated that
of FG 55. binding forces were weak and would be another indication of high mobility Material balance data for FC 95 are presented in TABLE III and these
data indicate
experiment,
that
all
of
the
chemical
was
accounted
for
throughout
the
*
000184
D
TABLE 11
'
ShPoei, T253i5ok.ri930000 a RT
2.000
FC s95 DESORPTION ISOTHERM cDATA*
Fives LBeeosoepeion sF2Lr.a7o000 2aS000
secondoDoesorpiion 1x o03F.-a350d0000
0.6000
0.2000
e Amouna t Adsorbed
v Ji OA
(C`rmuy a IEEE Desorption, ug/s
ANneovuenrt.sooncosmoit EE Desorption,
Thi fBosroention
b$52e00it0]0 psoeoo]0n
0.10000
Asopunrt uon soit bests Desorption, ug/,
) esio0
3.3000
Z16.7000
"23.9500
3rio 29.500
Yon 11.4000
too4.7000
bd 2.2500
ith corsaction for whe smoons oF FC.BS bo the 2s mh of semation momsining *Columns F, G, and H were calculated in the same way as Column F, TABLE I
from the previous step in each case (See Materials and Methods Section.)
:
:
ot
.
Sak
"~ Adsorption Isotherm
GETTER
95 DEfSFOiIRGPtUTRIEON2 NTA POINTS
Tiay 180TiERy
3J
%
vas
Pr fre
HA
Ca SOTION CONC (wphm)
000185
ABSORPTION AD BDESFEOIRGPUaRTnEIO:N3 11S3O0T0I.ERaSo,FOsRhore
LINES ARE BEST FIT FOR ADSORPTION AND
ET REIT
psp. on
Cn
,
4
y
TABLE TIT
FC 95 Material Balance*
Total AInitial (FCColu95mniDn,SToAluBtLiEonT,) mg.
73..0955000000 21..2257050000 00..07700000
FC 95 in8Solution (CaotluEmqnuilE.,,"TmAgB.LE I)
35..3854570500 1.1.909520500 00..0555020500
FC 95 con soil "ataE-quBil., ng.
10..2509255000 00..322275500 00..0124070500
Amount Reomoved by
Amount ReEmoved by Amount RFemoved by
First Desorption, mg. Second Desorption, mg.. Third Desorption, mg.
00..489674755000
00..217781070500
00..100554755000
00..311519000000
00..015050705000
00..002306225500
)
00..001910550000
00..000343050000
00..000122225500
Total GAmount DDeessoorrpbteidonbsy,Thnrgee (DEF) 10..27428430 00..24345703 00..10316738
Amount RemHaining on Stoiiolns,Aftmge.r 3 (DCes-or6)p-
--00..4152795000 -0-0..0111090705 00..01012225500
Amount1Desorbed as P(e6r/cCenxt1o00f)Amount Adsorbed
112015..688015 110346..454645 9828..377530
"Columns D, E, and F were obtained by first calculating the amount (ag)
ooff FsCo-l9u5tioinn 2i7n.5eamclh r(e25spmelctaidvdeedstpelpusand2.5thmeln rseumbatirnaicntginfgrotmhepraemvoiuonuts(nsgt)ep) in the 2.5 nl of solution remaining from the previous step.
:
000186
Te
2
: S=U LR
8
in ig
FC 143
)
Data for FC 143 are presented in TABLE IV and TABLE V and in FIGURE 4.
The adsorption isothern indicated FC 143 mobility similar to that of FC 95
with K=0.38 and Nel. Regression analyses were not perforned on the desorp-
tion isotherns, however, the graphed data (FIGURE 4) indicated that adsorption
and desorption could not be described by a single-valued function. That
is, the K' and N' values for desorption would not be the same as K and N for
adsorption. Subjective evaluation would indicate that the desorption coefficient
X', would be mich smaller than the adsorption coefficient, K, at solution
concentrations greater than about 25 mg/1, since the slope of the adsorption
isothern was much greater than the slopes of the desorption isotherns in
this Tange. At solution concentrations less than 25 mg/l., the desorption
coefficients would appear to be much greater than the adsorption coefficient.
)
Fron this it would appear that two or three different binding mechanisas
Were involved with stronger binding occuring at the higher concentrations and
the converse at lower concentrations. While this may indicate a tendency
for FC 143 to be immobile at high concentrations, it would be quite mobile
in any situations involving low concentrations.
.
Material balance data for FC 143 are presented in TABLE VI. While
the two concentrations resulting in 212%and 201% desorption (last column
in TABLE VI) were erratic, in general, the data indicated that all of the FC 143 vas accounted for throughout the experiment.
2
00187
Brkt
3
FEES
TLE Tv
FC 143 Adsorption Data
L
A
5
c
Initial FC 143
Conc., mg/l.
Equil. Conme.,
Cc, mg/l.
X Removed
By Soil
-
-
s22922..56
428759..81
(4x2x4 1000) C1406
1695742...213
14699020..932
4u2..s10
5.2
51
13
.
E
Ti5ongtaIlniFtCia1l43Sol'n, STonoltg'anl aFtC E1q4u3ili.n,
FG 143 Adsorbed
o0n-5S)oixl',10x/n, ug/g .
(Ax 0.035 liters) (Bx 0.025 liters)
)
71.3.30165205
162..91747550
18637..55
42.1..133850072055
124...230400757505
93142...550
0.1300
0.1275
0.5
3
.
000188
LER Vaart
T
on
LET
:
10
Tn
iE
5 TABLE V
FC 143 Desorption Isotherm Data
A
B
SEqouliult.ionC,oncC., fn iEnquFiilr.atCoDnecs.orp-
as/1
tion Solution, mg/l.
(CoB,lTaublmeInV)
485.800
126709..310000 92.200
49.900
5.100
47.6000
1728..28000000 10.7000
6.1000 0.6000
c
D
EiqnuiSle.conCodneD.esorp- EiqnuiTlh.irdConDce.sorption tion Solution, mg/l. solution, mg/l.
6.80000
34..4800000000 2.00000
0.80000 0.10000
3.50000
22..9000000000 0.50000
0.20000 0.01000
E
o
u
)
Amount Adsorbed aonsSoil, x/m,
Amount on Soil Aafltser First Desioonrp-
Amount on Soil
Adount on Soil
Afstlesr SectoinodnDesorp- Afgt/ger ThtiirodnDesorp-
/
(Colum , TABLE Tv)
183.500
67.500 34.500
9.500 12.000 0.500
164.600
50.850 20.050
=3.250 3.400 =0.250
151.000
38.650
9.950 ~8.900
2.050 ~0.500
135.150
25.100
0.650 ~10.650
1.350 ~0.505
#Columns 7, G, and H vere calculated in the same vay'ks Column , TABLE IV wfirtohm tchoerrpercetviioonusforstetpheianmoeuancth cofasFeC(1S4e3e Miantetrhieal2s.5amndl MoefthsoodlsutSieocntiroenm)a.ining
000189
SEE
un
200 D 1504pa-- -- TT
8
-- A
$
100
zX
A
---- = Zc
2
so
{
8c
-- --x
B
1
ol YF E
c%
2%
Y= 16.5 + 0.38 X
R-SQUARED = 0.936
2
:
-s0
0
100
200
300
400
500
Y
Equil. Conc., C, mg/l
FIGURE 4
FC 143 ADSORPTION AND DESORPTION ISOTHERMS
dSeosloirdptliionne iissotbheesrtmsf.it aA'dssoarprteioandsoirsoptthieornm,isoDtohtetreaddaltianesposinrtes.estBi,maCt,edD; E, and F are desorption data points for the respective concentrations.
GENERAL COMMENTS The FC 95 and FC 143 adsorption coefficientsfromthese experiments
my be converted to the analogous constants based on soil organic carbon content K, with the equation K,. = 100 K/(% organic carbon) giving a Ky of 45 for FC 95 and 17 for FC 143 (2.2% organic carbon for this soil). Comparing these values to those in TABLE VII, it can be seen that FC 95 and FC 143 are at the low end of the spectrum, again indicating high mobility of these compounds.
2
000190
R SREETRRE SA TTT ET TTT
TE
12
TEE
s
D
TABLE VI
FC 143 WATERIAL BALANCES
A
c
Total FC 143
Initially in Solution
(Comlgl.mn D, Table 1v)
FC 143 in Solution
at Equil., mg.
(Column E, TABLE IV)
FC 143 on Soil
at Equil., mg.
W - B)
13.0625
12.1450
0.0175
7.3150
6.9775
0.3375
42..13582080
4.2.03007550
00..10742755
10.13300705
10.22747s5
00.000620s0
e
v
FAmiorusntt.DeRseomropvteidonb,y ng. ASmeocuonntd RDeesmoorvpetdiobny, mg. TAhsiorudntDeRseomropvteidonb,y ag.
-D
00..0088432550 0.omazs
00..0066180000 0.05050
00..007686275500 0.046500
+ 000016337050
00..002086275
00..000083755000
0.00375
olon2s
0.000025
c
i
1
Total Amount De-
Gee) DseosrobrepdtiboynsT,hrmege
Amount Remaining on
: 55 tSoiiolns,Afmtge.r 3 Desorp-
Amount Desorbed as
pseorrcbeendt (oGf/CAmxou1n00t) Ad-
0.2418
000...211016020808 - 00.l00503s0
0.676750
0-0.0..100250533522055000 -00..000026572580
$
26.349
2651622...181110658 25081..705000
F*CCol1u4m3nsinD,27.E,5 malnd (F25wmelreadodbetdainpeldusby2.5fimrlst rceamlaciunliantginfgromthepreavmioouunst s(tmegp))of of solution in each respective step and then subtracting the amount (mg) in the 2.5 ml of solution remaining from the previous step.
000191
te
C R LUR E R
TABLE VIY
CofmopraraisSoenleocftedAdGsroorupptioonf CPoeesftfiicciideensts
N
(Hamaker and Thompson, 1972)
Chemical
Koo
(pobile) (ChFloCraSmbe=n= = ===2= 1712).8
2,C49-05 - vm m on = a352)
PrBoropmhaacnil
n51
SMionnauzrionne
1385
.
DPircohplaozbienneil
116542
ACthlroarzoipnreophan
21752
APrnoemtcrtyonne
330800
PDrioumrcotnryne
a51s3
PCahrlaoqruoaxturon
240,,908060
(imaobile) DOT
243,000
EAPRLORER
-
The small amounts adsorbed and ease of desorption is consistent with the relatively high vater solubility of FC 95 (300 mg/1) and Re 143 (520 g/1.)
and with the. chemical nature of the molecules - organic salts which
ionize in aqueous solution:
CgF 505K
5Fy 500,M,
FC 95
FC 143
000192
RET rm
GR ah EE
ee
jo
:
!'
1
pr
Cait
E
Terns
DPM - Disintegrations per minute
C - Concentration of chemical in solution at equilibrium
x/a - Concentration of chemical adsorbed on soil at equilibrium
R? - Coefficient of deternination
:
kK - Adsorption coefficient
K' - Desorption coefficient
:
N - Exponential term in Freundlich Equation
:
N' - Exponential term for desorption equation
Koc - Adsoiption coefficient based on soil organic carbon content
References
DavidPseosnt,iciJ.deM.M,oveemt.entalT.,hro1u97g5h,SoEUislePs,oAfU-.SoGilS. GEPP0aRr,a7meZte-rs7fo5r -De0sc0rib0in.g
DavidisnonS,oiJl.s,M".,pre1s9e76n,ted"VeatrtiScyamlpoMsoivuemmeonntNoannbdioDliosgtirciablutTiroannsporotf Orgaanndics OG TfranSastafnodrlanradtst i,on hof e Pollr utanstsWDh o.n,MuLaand yrand g 1-13, ,Wa1te9r7,6.at National Bureau
Hanakienr,thJe. SWo.i)anEdnvJi.roMm.enTth.ompsCo.n,A. 19I.72.Gor"iAndgsorapntdioJn." Wi.n HOarsgaakneicr C(hoedmsicalJrs farcel Dekker,Tnc., N. Y.
HamakCehrem,icJa.lsW,.,Hu1n9a75n,He"aIlnttherapnrdetatthieonEnovifroSnomielntL,eAachiCnogllEexcpteiroinmeonftsD,o"w Sicnienti-
fic Papers,VoT. 1, DowChemical USA,
Midlan, Wich. 8640 --
:
000193
he
LHR
it ~o
I
Attachedarecommentsonthe3M TechnicalReport "AdsorptionofFC 95and FC143onSoil. SX. Welsh, Project 9970612633 FateofFluorochemicals, Report No. 1, Feb. 27, 1978"`madeby
ProfessorStephenA. Boyd,MichiganStateUniversity, datedMay19, 1993.
:
000194
Lf
:
Reviewof Technical Report Summary Adsorption of FC 95 and FC 143 in Soil
Material and Methods
sSohrobusldlegsisvtehraencogvlaesrsieosonfpocloymetphoyulnendes,ibnubtldaoneks(nn'ot-sgoiivle) aexnpuemreirmiecnatls.vaSltuaet.es that polypropylene
"voTlhaetillairzgaetihoenadosrpascteic(ki2n5gmtlointhae 5t0ubteu,bew)iils uinndfelsaiterabtlhee;saonryptlioosnsecsooeffftihceien"tC-slianbceel,thee.g.m,etfhroodm ccaolnccuelnattreastitohnes.amAolusnot tshoer2b4edhobuyrdmiiffxeirnegncpeerbieotdweseenemtshearibniittriaarly.andWefrinealeexqpueirliimbernitusm dsoonleutifoonr differentperiods of time to establish that equilibrium was reached within 24 hours?
Details on the stock solution are lacking. What solvent was used and What is the specific activity and radiochemical purity of the "C-FC 95.
`The idea of using acotton swab aftethe draining step is unusual Hopefully this didn't remove asosilhiagshwaesllI'ads lwiakteetro. sTeeheit.~2A05%0%orolresgsredaetcerreadseecrienassoeluwtoeuclodncbeentbreatteiro.n due to sorption isn't
`This section generally lacks detail that would normally be required for publication.
Results and Discussion
dTehmeonlsinteraartietytohafttthheeiesnottihreerimsohtahsebremeins slihnoewarn, otvheerlitnheearciotnycemnutsrtateixotnenrdantgoeeuqsueidl.ibrHiouwmesvoelru,tiotno coofnFceCn9t5ratoiroFnsC1t4ha3t:apIpfrnooatc,hhtohewwwaetrere tsohleubiiniltiitaylosfoltuhteiocnomcponocuenndt.ratDioonsyosuelkecntoedw?the solubility
`Thesorptioncoefficient(K) ofFC 95appearstobeabout 1asindicated. Theorganicmatter
ins asooilrsorpsmtoiropantciooelnfcfoiiecfifeinzctiiennette(rdKmeedia=teKbe/twfeies,nKbo)ennz=ene1/a0n.d0t2o5lu=er4i0e,,oIrtw 10g Koobyeu =wo1r.l t6h.whTdihlies
`to ecxaominwneitshvoinmeaefaadrcdtitogiroonfea2l stooils3ftoorcdoinfffierremnttshoiislKs.osTvhailsuwe.ouGlednienrcarlelay,sethmeyKc.uo,nvafliuedseishnnotcuhled
accuracyofthe one measured value.
:
TexvpeersipmoetntcshaencdkeIdgettheesssoeinltiaclolnycetnhterastaimoensvaolfuesF.C-T9h5efcoarlcbuolatthiotnhselosoorkptgiooond.and desorption
`soTlhuebiKlitvya.luTehs efohrysFteCrsi1s43in itshelodweesorrptthiaonnFiCsot9h5erimndiiscsautripnrgistihnagt,itanpdrohbaasblbyeehnasoaver-hiingtheerrprweattede.r `"Tthhereseordpitfifoenrenitsobtihnedrimngismleicnheaarniisndmisca.t.i.ngwiathsisntgrloengsoerrpbtiinvdeipnrgocaetshsi.ghTehrecocnocnecnltursaitoinonrsegaanrdditnhge ceoxnavmeirnsees actolluowmenrIc*oAncmeonutnrattDieonsso"rbiesdvaesryasPpeerccuelnattiovfeAbmaosuendtoAndsthoerbseindgletheexvpaelruiemsenrta.ngIeffornoem.
060195
26 10212 percent, so it's pretty inconclusive. There is a fairly good discussionof hysteresis in J. Environ, Qual, 12:325-330 by Koskinen and Cheng who observed this phenomena for the weak acid pesticide 2,4,5-T. The causes of hysteresis are varied and complicated and may include microbial degradation ofthecompound during desorption, and changes in the physical `and/or chemical properties of the soil-solution system. For example, desorption using distilled `water(asisthecasehere)couldresultinsoil dispersionsothat aclearsupernastolautniotn `could notbeobtained. This can cause quenchingofradioactivity in solution and other problems leading to error.
`The "material balance as presented in the report is a little misleading. To obtain a material `abdadlaintcteoytohue smheoausludrmeedassoulruetitohne caomnoceunnttroatfio"nCs-.activity in soil at the endofthe .experiment, and
GeneralComments. TheK,,valuescalculated hereuseanorganiccarbon contofe2n.2t% whereasthevaluestatedintheMaterialsandMethodis 1.5%?
`Thewatersolubilitiesarecitedas 300 mg/L for FC 95 and > 20g/LforFC 143. Surely the Iatter value is wrong. Ifthe solubilities are truly that different, then the sorptive properties should be vastly different, which they are not. If FC143 has a solubility of >20,000 mg/L, then I would expect no sorption. This value must be erroneous.
Recommendations:
1. Obtaining K, K., values on additional soils. DetermineifK., is relatively constant.
2. Obtain a true mass balance by measuring "C-activity in soil and solution phase.
3. Interpret desorption data more cautiously.
-
4. Get correct valueofwater solubility of FC 143.
00196
"Pomerar 11a
TECHNICAL REPORT SUMMARY
TO: TECHNICAL COMMUNICATIONS CENTER -- 201.2CN {important Ifreport ispinotnbeodt siodfpaepesr,sand twocopiets0 TCC.)
EE PC Fate of Fluorochemicals Adsorption of FC 95 and FC 143 on soil
2/21/78
0222 9970612633
1
Stephen x. nes SEW
73583
140673, #47708
14
ssonmvp LO0conier tosiaRunoriaton) |HEGRE
aE
werwaonmos:rom am CURRENT GRsECTIVE:
"
=
pe
To obtain an indication of FC 95 Co and FC 143 mobility in sandy loam
soil.
EE BC - Div.
FluorochemicaC l [a meron ABSTCRoACmTe. (R080705.0wore Tris sovract informationsdaburedby he Techical Commrications Contr 1
Soil
As a part of the Fate of Fluorochemicals Project, an indication
Adsorption
of mobility of FC 95 and FC 143 in sandy loam soil was desired.
Nobility
AMdsorption-desorption experiments (after Davidsoxn, 1976, and Hamaker,
1675) along with water solubility data can provide such' information.
The adsorption coeffifnts for FC 95 anFdC 143 were determined to be 0.99 and 0.38, respectively. For FC 95 adsorption and desorption could be described by a' single valued function while for FC 143, they could not. Based on these data, both compounds would be Judged mobile in the sandy loam soil used in this study.
rmation ton
00197
"
2
concLUSTONS
Adsorption coefficient for FC 95 and FC 143 were 0.99 and 0.38, respectively. For FC 95, adsorption and desorption could be described by a single valued function while for FC 143, they could not, Considering adsorption coefficients, desorption characteristics and water solubilities, both conpounds would be judged mobile in the sandy loam soil used in this study.
INTRODUCTION
As a part of the Fate of Fluorochenicals Project, an indication of
mobility of FC 95 and FC 143 in sandy loam soil vas desired. AMdsorptiondesorption experiments (after Davidson, 1976, and Hamaker, 1975) along with water solubility data can provide this indication of mobility. This approach is used by the U. S. EPA in pesticide registration requirements.
MATERIALS AND METHODS
Duplicate S-g samples of air-dried Brill sandy low soil (S7% sand, 364 silt, 7% clay, 2.5% organic matter, 1.5% organic carbon, with pH 6.5 and C.E.C. of 15.3 meq./100g) were shaken with 25 ml of solution in 50 ml.' poly-
Propylene centrifuge tubes for 24 hours on a wrist action shaker at room temp.
(16-15C). Polypropylene tubes were used because they were found in separate
experiments (3M Tech Notebook #470673, `C. H. Schrandt) to sbsorb less FC 95 and FC 143 than glass or polyethylene tubes.
Solutions were made by diluting a stock solution of each chemical.
Concentrations of '4C-labeled FC 95 were 282 mg/1., 158 mg/1., 90 mg/1.,
S1mg/l., 28 mg/l., (100%, S6%, 323, 18%, 10%, 1% of stock). Concentrations
of 14C-1abeled FC 165 were 525 ng/1., 295 mg/L, 167 ng/l., % mg/l., 52 ng/l.,
and 5.2 ng/1.
000198
Ba
3
After shaking the initial solutions as well as the three
desorption extractions with deionized water, the samples ere centrifuged at 5000 pm for 10 min., and three aliquots of each supernatant solution were taken for scintillation comnting.
After the adsorption step, 22.5 ml of solution were Tecovered, Therefore, it was assumed that 2.5 ml of liquid remsined with the soil in
each step and this amount was accounted for in the desorption calculations
(see Results and Discussion section). In the FC 95 experiment, the supernatant 1iquid was simply drained
Off at each step and the next 25 ml of liquid were put into the tubes. In the FC 143 experinent, the supernatant liquid remaining after the draining step was absorbed with a cotton swab before putting the next 25 m1 of liquid into the tubes.
"The procedures for the FC 95 and FC 143 experiments were recorded in 3 Technical Notebook #40673, p. 49 and p. 51, respectively.
From the raw counting data, disintegrations per minute (DPM) and
FC 95 and FC 143 concentrations were calculated for all of the supernatant solutions,
Statistical analysis and plotting of the dats vas done with the MINITAB package of the 3M TRAC computer service.
)
RESULTS AND DISCUSSION
FC 95
Adsorption data for FC 95 are presented in TABLE I and FIGURE 1.
Comparing the regression equation of the adsorption isotherm (FIGURE 1)
X/m = 0,29 + 0,99C with the Freundlich equation x/m = Kc/N, it could be
seen that the adsorption coefficient, K, equaled 0.99 and the exponent, N,00091!
equaled one, The linear shape of the adsorption isotherms (N=1) indicated
P
4
that FC 95 adsorption on soil would be independent of concentration. The low adsorption coefficient (K=0.99) indicated that FC 95 would be mobile, i.e., it would move readily with the ground water through this sandy loam
soll.
TABLE
FC 95 ADSORPTION DATA
.
A
5
c
) IniCtoinael., F5C8/915 --
21528..20 s0i.l0o 2820.08
: >
EqC,uilm.g/lC.onc., --_--
213334..92 a7z6..09 221010
E
A*Ehere E10
1175.11 1176.68 2271.10,
wd PY
In TIontiatlialFCSo9l5'n (Ax 0.025 liters) -
3.7.90550000 21..22570500 00..07700000
SoTlo'tnalatFECqu9i5l.i,n mg (Bx 0.028 liters)
55..8348755000 11..0952020500 0.00555020500
onFCSo9i5l,Adxs/oar,bedba/g (0-E) x 10
C
um oil
2109..80 a653.7 23s8
Desorption data for FC 95 are shown in TABLE II and FIGURE 2. For comparison, desorption isotherns for the pesticide fluometuron are given in FIGURE 3.
For clarity FC 95 desorption isotherms are not drawn in FIGURE 2.
However, all of the data points lie very close to the adsorption isotherms
.
indicating that adsorption and desorption could be described by a single-valued
function with desorption coefficients, K', equaling the adsorption coefficient,
000200
DU
s
240
BE
A
-
i 180
.
.
3 120 E
i3o
DZ
X
EE Regression Eqn.: Y = -0.29 + 0,99 X R-Squared = 0,985 oC
A)
5
[I]
120
180
240
300
Equil. Conc., C, mg/l
FIGURE 1
FC 95 Adsorption Isothern
.
This, along with the observation that approximately all of the adsorbed
FC 95 was subsequently desorbed (TABLE IT, Column H) indilated that
binding forces were weak and would be another indication of high mobility
of EC 95.
tL
Material balance data for FC 95 are presented in TABLE III and these
data indicate that all of the chemical was accounted for throughout the
experiment.
000201
iy
o
.
A Equil. Conc. in
Solution, C, mg/l.
213334..920000 427.6.090000
22.100 2.000
TABLE 11
FC 95 DESORPTION
5 Equil. Conc. in
First Desorption mg/l.
3502..73000000 189..36000000
5.3000 0.6000
ISOTHERM DATA*
c Equil, Conc. in
Second Desorption mg/l.
194..05000000 25..33000000
1.7000 0.2000
}
0 Equil. Conc. in
Third Desorption
mg/l.
52..2800000000
|
11..8000000000
0.60000
0.10000
:
E
\mount Adsorbed
on Soil,
x/m ug/g
Col1u12m94n0..03F0,000TABLE I) 462595...357000000 3.800
F
Amount on Soil
- After First Desorption, ug/g
6179..64050000 11313...243000000000 1.7000
[I
Amount on Soil
After Second Desorption, ug/g
-1412..50000000 126..07500000 4.0.79000000
H
Amount on Soil
After Third Desorption, ug/g
-2-59..81050000 2"32..90500000
02..42550000
*Columns F, G, and H
with correction for
wtehreeacmaolucntulaotfedFCin95thine
tshaeme2w.a5ymlasoCfolsuomlnutiF,onTATBeLmEainIing
from the previous step in each case (See Materials and Methods Section.)
el
:
:
:
ne
"
oi<3 3
"~ Adsorption Isothern
TR
.
"
FIGURE 2
FCC 9955DEDESSOORRPPTTIIONDATAPPOoInNtTs
3 aon
%
ase ce
Pe som ean
PY
oF
sean TM
ony 5 0 2,
soumon conc ream 000202
ADSORPTION
AND
Frou 3 DESORPTION
ISOTHERYS
FOR
OE a chy, "SOANLDBIROKDEN
PR
7
TABLE 111 FC 95 Material Balance*
Total AInitial' (FCCol9u5mniDn;SToAluBtLiEon1,) mg.
37..9055000000 12..2257050000 00..70070000:
FC 95 in8Solution (aCtolEuqmunilE.,,"TmAgB.LE I)
35..3854570500 11..909520500 00..5055020500
FC 95 con soil aAt-EBqu)il., mg.
01..5290520500 00..232257050 0.14750 0.02000
Amount ReDmoved by First Desorption, mg.
00..489674755000 00..311519000000 00.001910550000
TotalGAnount DDeessoorrpbteidonbsy, Tnhgree (DEF) 01..27428430 0.0.24345703 00..10316738
Anount REemoved by Second Desorption, mg..
00..127718705000 00..015050705000 00..003034500000 Amount RemHaining on tSoiiolns,Aftmge.r 3 (DCes-o6r)p-
AmountFRemoved by Third Desorption, mg.
00..015045570500 0.036250 00..001220225500 0.002250 Amount1Desorbed as P(e6r/cCenxt1o0f0)Amount Adsorbed
--00..1425970500 --00..1011807050 00..01012225500
112013..688015 113064..454645 8982..755703
o*fColFuCa-n9s5 Di,n 2E,7.5anmdlF (w2e5rneloabdtadiendedplubsy 2f.ir5stmlcarlecmualiantiinnggfrtohme parmeovuinotus(mgs)tep) oinf tshoelut2i.o5nmlinofeacsholurteisopnecrtievmeainsitnegp farnodmtthheen psruebvtiroaucstinsgtept.he amount (mg)
000203
IE
.
*
FC 143
Data for FC 143 are presented in TABLE IV and TABLE V and in FIGURE 4.
The adsorption isothern indicated FC 143 mobility similar to that of FC 95
"With K=0.38 and Nel. Regression analyses were not perforned on the desorp-
tion isotherms, however, the graphed data (FIGURE 4) indicated that adsorption and desorption could not be described by a single-valued function. That
is, the K' and N' values for desorption would not be the same as K and N for
adsorption. Subjective evaluation would indicate that the desorption coefficients
x', would be much smaller than the adsorption coefficient, K, at solution
concentrations greater than about 25 mg/l, since the slope of the adsorption
- isothern was mich greater than the slopes of the desorption isotherns in
this range. At solution concentrations less than 25 mg/l., the desorption
coefficients would appear to be much greater than the adsorption coefficient.
From this it would appear that two or three different binding mechanisms
were involved with stronger binding occuring at the higher concentrations and
the converse at lower concentrations. While this may indicate a tendency
for FC 143 to be imnobile at high concentrations, it would be quite. mobile
in any situations involving low concentrations.
:
Material balance data for FC 143 are presented in TABLE VI. While
the two concentrations resulting in 212%and 201% dsorption (last column
in TABLE VI) were erratic, in general, the data indicated that all of the
FC 143 was accounted for throughout the experiment.
000204
RE.
El
TABLE TV
:
FC 143 Adsorption Data
a
3
c
.
|
CInointci,.almg/Cl.143 Ec,qumigl/.1.Conc.
By2 SRoeimloved
.
(452x100
To2s92s.6
247859..81
E4Y.)6
1697.1.2
16902..32
42.10
. 52s.a3z
495.19
a19s
:
>
E
.
iTnotIalniFtCial143Sol'n, TSootla'ln aFtC E1q4u3ili.n, oFnG S1o4i3l,Adsxfomr,beudg/g
u(Agx 0.025 11ters) (Bngx 0.025 liters) ( ) X10 1 :
173..30165205
162..91747550
183.5 67.5
4.1800 2.3525
4.0075 2.3050
"3o.l5s
. 01..13300750
01..12247755
12:0 0.5
060205
ZF.
We
10
`TABLE V
:
FC 143 Desorption Isotherm Data*
A
ESqouliult.ionC,oncC., in
=e/1
5
iEnqufiilr.etCoDnecs.orp-
tion Solution, mg/l.
(Column3,Table IV)
+
485.800 279.100 160.300
92.200
495..910000
47.6000 28.8000 17.2000 10.7000
06..61000000
c
iEqnuiSle.coCnodncD.esorp-
tion Solution, mg/l.
E{iqnuiTlh.irdConDce.sorption
_solution, mg/l.
6.80000
4.80000 3.40000 2.00000
00..8100000000
.
3.50000
2.90000 2.00000 0.50000
00..2001000000
E
Amount Adsorbed Amount on Soil
on Soil, x/m, After First Desorp-
u(eC/oglum 7, TABLE IVu)g/g tion
183.500 67.500
349..550000
12.000 0.500
164.600 50.850
-320..205500
3.400 ~0.250
c
u
Azount on Sol Asount_on Soil
After Second Desorp- After Third Desorp-
ng/g tion
ug/g tion
151.000 38.650
89..990500
2.050 =0.500
135.150
25.100
100..665500
-
1.350
=0.505
*Colums F, G, and H vere calculated in the same way as Colum , TABLE IV
with
from
correction for the amount
the previous step in each
of FC 143
case (See
in the 2.5 ml
Materials and
of solution remaining
Methods Section).
000206
co
u
200
.
150k 57 _-- -- 8
J--
A
'
>
100
22
A
Zc
1 efx g3
so La
A
s
-- --%
B
:
E
5
2K
2
YR-=SQU1A6R.E3D += 00..93368
.ca
-
-s0
o
100
200
300
400
EN
Equil. Conc., C, mg/l
FIGURE 4
FC 143 ADSORPTION AND DESORPTION ISOTHERMS
:
Sdeosloirdptliionne iissobtheesrtmsf,it Aa'dssoraprteioandsoirsoptthieornm,isoDtohtetremddaltianepsoianrtes.estBi,maCt,edD, E, and F are desorption data points for the respective concentrations.
GENERAL COMMENTS
The FC'95 and FC 143 adsorption coefficients from these experiments
may be converted to the analogous constants based on soil organic carbon
content K,., with the equation K,. = 100 K/(% organic carbon) giving
a Ky. of 45 for FC 95 and 17 for FC 145 (2.2% organic carbon for this soil); Comparing these values to those in TABLE VII, it can be seen that FC 95 and FC 143 are at the low end of the spectrum, again indicating high mobility of these compounds.
:
000207
Co
12
TABLE VI FC 143 MATERTAL BALANCE*
A
5
c
InTiottiaalllyFCin143Solution (Cmoglu.mn D, Table 1v)
FCat 1E4q3uiiln.,Somlgu.tion (Column E, TABLE IV)
FatC 1E4q3uilo.n,Somgi.l (A .- B)
13.7.03612550
162..91747550
0.o33o75
:
-
2.4.31582050
42..03007550
00..10742755
1.031037050
1.0.21027755
00..00062050
E
or
AFmiorusntt.DeRseomropvteidonb,y mg. ASmeocuonntd RDeesmoorvpetdiobny, mg. ATmhoiurndtDeRseomropvteidon,by mg.
00..0083342550 0.00:067327255 00..004037050
00..0066810000 00..0052085205 00..0000617255
00..007696275500
00..004068570500
00..000030500205
.
G
sToortbaeld AbmyouTnhtieDee(DDe+sEoSrFp)tions, ng
0.0.22142108 00..11609038 00..00503550
H
SoAimlounAtftRerema3iDneisnogrpo-n'. tions:, 6ng).
00..617265755000 00..000533225500 -00..000062572550
1
:
ApmeorucnenttDoefsoArmboeudntasAd-
sorbied (6/C x 100)
2626..831459 . 29128..110186
28081..705000
"FCCol2u4m3nsinD,27E.,5 amlnd(F25wmelreadodbetdaipneldusby2.5fimrlstrceamlaciunliantginfgrotmhepraevoiuonuts s(taeg)p)of oifn tshoelut2i.o5nmlinofeacsholruetsipoenctrievmeainsitnegp afnrdomthtehne psruebvtiroauctsinsgtept.he amount (mg)
000208
. oF
: =
-
gr
s
TABLE VIT
CofmorpaariSseolnecotfedAdsGorroputpioofn PCeosetfifciicdieesnts (Hamaker andThompson]1872)
Chemical
Koo
(mobile) (immobile)
C(hFlCo1r4a3mbon = 2(,C495 -- ooo PBrroompahcainl SWiomnauzrionne DPircohplaozbienneil ChAltroarzoipnreophan APnreotmreytonne DPrioumreotnryne CPhalroarqouxautron DOT
oo2. 1712).8
voogn3s2)
7s1
13835
152
116742
234050
34880s ou-
513 4,986
i
24230,,000000 71
. e. n
The small amounts adsorbed and ease of desorption is consistent with the
Telatively high water solubility of FC 95 (300 mg/1) and Kc 143 (>20 g/1.)
end with the chemical nature of the molecules - organic salts which ionize in aqueous solution:
.
N
CaF,3505 K
CF 50, NH,
k
FC 95
FC 143
:
C0209
i
14
/
Terns
DPM - Disintegrations per minute
-
- Concentration of chemical in solution at equilibrium
x/m - Concentration of chemical adsorbed on soil at equilibrium
RZ - Coefficient of deternination
.
KX - Msorption coefficient
K' - Desorption coefficient
N - Exponential term in Freundlich Equation % N' - Exponential term for desorption equation i
Koc - Adsorption coefficient based on soil organic carbon content
References
.
DavidPseosnt,icJi.deM.M,oveetm.entalT.,hro1u97g5h,SUosielosfU,.ESoPiS.lA-PaGErPAa,Gme0te7rs2-foTr 8De-sc0r0ib0i =,
+DavidTisrnoannS,sofioJl.rsm,aM".tp,iroen1s9e7o6nf,tPeod"lVlaeutrttaiSncytamlspooMsionuvmemLindeonntNsndoamnbdioWDlaiotsgetirrciabalurtTiroorantnosoipfooTrOtrgaaPnndiocus C Of Sa tandlardst, hersWDb.,Muayr 11-g 13,,1976.
Hamaker, J. in the
'SWo.ilaEnndvJi.roMm.enTth.ompsC.on,A.
191.72.Gor"iAndgsoarrpdtiJo.n
Wi.nHOarmgaakneicr
C(heemfiscagls
FarceT Dekker, Tnc., N. Y.
HanakCehre,micJa.lsW,.,Hu1m9a75n,He"aIlnttherapnrdettathieonEnvoifroSnomielntL,eacAhiCnoglleEcxtpieornimoenftDso,w" SicnientiFic Papers, Vol. 1, Dow Chemical USA, Midland, Wich. 48640
00210