The effects of high levels of polycyclic aromatic hydrocarbons on sediment physicochemical properties and benthic organisms in a polluted stream

The effects of high levels of polycyclic aromatic hydrocarbons on sediment physicochemical properties and benthic organisms in a polluted stream

Chemosphere, Vol.16, No.5, P r i n t e d in G r e a t B r i t a i n pp 1053-1063, 1987 0045-6535/87 $ 3 . 0 0 + .OO P e r g a m o n J o u r n a l ...

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Chemosphere, Vol.16, No.5, P r i n t e d in G r e a t B r i t a i n

pp

1053-1063,

1987

0045-6535/87 $ 3 . 0 0 + .OO P e r g a m o n J o u r n a l s Ltd.

THE EFFECTS OF HIGH LEVELS OF POLYCYCLIC AROMATIC HYDROCARBONS ON

+ SEDIMENT PHYSICOCHEMICAL PROPERTIES AND BENTHIC ORGANISMS IN A POLLUTED STREAM

William J. Catallo III

(I) and Robert P. Gambrell (2)

(I) Division of Chemistry and Toxicology, Virginia Institute of Marine Science, Gloucester Point, VA

(2) Laboratory for Wetland Soils and Sediments, Center for Wetland Resources, Louisiana State University, Baton Rouge LA

ABSTRACT The effects of polycyclic aromatic hydrocarbons on benthic micro- and meiofaunal biomass was determined and related to selected sediment properties such as redox potential and organic matter content in a contaminated environment. INTRODUCTION

Bayou Bonfouca is a palustrlne, mlxed-forested, ecosystem in the Lake Pontchartrain Basin near Slidell, Louisiana (I).

As a result of a fire at a wood products treatment plant

in 1970, approximately 9 hectares of the bayou and surrounding drainage areas have been heavily contaminated with polycyclic aromatic hydrocarbons (PAHs) in a coal tar mixture known as creosote.

PAHs in the environment, food, water, and the workplace are of concern

because of the mutagenlcity and/or carclnogenlclty of several of the compounds in this class (2-5).

+ VIMS

Contribution

No.

1355 1053

105 ~

Creosote

is formed as a by-prOduct

of coal and is characterized

with CI-C 4 alkyl homologs also present used as a sealant and "non-leachable" railroad

during the high temperature

by concentrated

ties, and pilings.

(> 900°C)

mixtures of predominantly

in limited amounts

(6-8).

carbonization

unsubstituted

This material commonly

bioclde for wood products such as telephone

Normally,

PAHs is

poles,

wood is pressure treated at elevated temperatures

to

ensure that organisms already present are killed and that the creosote has thoroughly permeated

surface layers.

arsenates

may be employed when severe fouling

encountered

(7,8).

Adjunct treatments

Creosoting

operations

with pentachlorophenol

is expected or when creosote

tend to be spill-prone

PAHs, PCP, and various metals have been detected preservation

facilities

(9,10).

in environments

PAH compounds organisms

there is growing biochemical

and mixtures

and biota near wood-

to neoplasia

and proliferative

(11-14).

However,

literature

disorders

effects and the physicochemical

properties

in workers and human populations

there is little work dealing specifically

of sediments

The purpose of this work was to examine properties

biomass estimates hypothesized

in contaminated

of benthic bacteria,

control.

properties

protozoans,

Superfund

It was

PAH toxicity would be observed in blomass reductions

in all trophlc and changes

in

such as redox potential and organic matter content relative

the reader is referred to references

is the only published Louisiana

and meiofauna.

For more extensive reviews of PAHs, creosoting operations,

Bayou Bonfouca,

between these

in natural systems.

the effects of PAHs on selected sediment

levels examined and that this would be manifested related sediment

with

areas of Bayou Bonfouca and to relate these with

fungi,

that concentration-dependent

linking various

in exposed aquatic

the effects of PAHs on benthic micro- and melofauna and the relationships

physicochemlcal

of

poles (9).

and epidemiological

as well as to increases of certain cancers

exposed to these materials

"bleed" is

and high concentrations

Smaller amounts of these substances have been identified

near point sources such as wharf structures and telephone At present

(PCP) and copper

6-9, and 15-17.

and the situation

to a at

To our knowledge,

this

study of the Bayou Bonfouca spill site, which was placed on the

Cleanup List in 1982.

MATERIALS AND METHODS

Four sites were established pollution

at Bayou Bonfouoa along an apparent gradient of creosote

and were assigned numbers as follows:

2 = "moderately

contaminated",

contaminated".

This gradient

were characterized

site I - control or "uncontaminated",

slte 3 = "heavily contaminated",

was later verified by analysis of sediment samples.

by soft bottoms,

m), similar vegetation

and shading,

and similar proximity

to the Slidell

gentle surface-water approximately

flows,

equivalent

site

site 4 = " extremely

shallow depths

litter input

urban area and its associated

All sites

(0.6 - 1.2

(visual estimate),

sources of pollution.

Sediment Characterization:

Bulk surface

(-10 cm) sediment samples for particle size analysis were collected

each site wlth a shovel and were stored

in plastic buckets with llds.

Sediments

to be

from

1055

analyzed for metals were collected with acid-rinsed teflon scrapers and placed in glass jars with teflon caps.

Redox potential (Eh) measurements were taken in situ using commercially

available platinum electrodes and saturated calomel reference electrodes.

Sediment pH was

determined using a calibrated combination pH electrode and values for both pH and Eh were obtained with a portable pH/millivolt meter (Orion Model 399A). Particle size distributions were determined via a standard hydrometer method (18), and readily oxidizable organic matter content by the potassium chromate/acidlc oxidation method of Jackson (19).

Sediment metals were extracted using the hot HCI/HNO 3 method of Anderson

(20) and analyzed by inductively coupled argon plasma emission spectrometry (ICAP).

PAH Extractions:

All PAH extractions were accomplished using highly purified reagents of "HPLC grade" (Curtin Matheson, Houston, TX), "Pesticide Grade" (Sargent Welch, Dallas, TX), or "Nanograde"

(Malllnekrodt, St. Louis, MO).

reagent grade.

Anhydrous Na 2 SO 4 and KOH were of analytical

The PAH standards phenanthrene, pyrene, l-methyl fluoranthene,

benzo(k)fluoranthene,

benzo(e)pyrene,

dibenzo(a,h)anthracene,

dlbenzo(a,i)pyrene were

donated by the NCI Chemical Carcinogen Reference Repository (NIH, Bethesda, MD). Naphthalene, anthracene, chrysene, pyrene, and benzo(a)pyrene Scientific) were of 98 % purity or better.

(Aldrich Chemical and Fischer

A mixture of 16 PAH standards

(Supelco Inc.,

Bellefonte, PA) also was used for standardization. All solvents, column packings, drying agents, and standards were assayed via high pressure liquid chromatography (see below) for impurities eluting in the range of interest. All sediment and water samples for PAN analyses were collected using solvent-rinsed glass or metal equipment and were stored in glass or metal containers with foil-lined caps. Care was taken to avoid contamination and exposure of standards, samples, and extracts to light was minimized.

Sediments were extracted using the method of Farrington et al. (21)

with the addition of ultrasonic disruption prior to alkaline reflux extraction, and the substitution of cyclohexane for benzene as the primary solvent.

Other modifications

included the use of centrlfugation instead of filtration, with extract volume reductions being accomplished where necessary by evaporation under a dry stream of nitrogen while sample containers were held in a controlled-temperature water bath (< 4°C) rather than in a rotary evaporator.

Surface water samples were extracted via the method of Sorrell et al

(22). PAHs were identified and quantified using a Waters Associates Model 480 Isocratic HPLC with the following specifications:

6000a pump; U6KA injector; a 480 L.C. detector; and a

Waters Associates RCM Bondapak column with a precolumn filter. acetonltrile:water at I ml/mln.

The solvent system was 86:14

Seperated compounds were scanned at 254 nm and absorbance

was recorded on a Hewlett Packard 3390a integrator with quantification accomplished by referencing sample peak heights to standard curves for each compound identified. The following criteria were utilized for PAH identification: compound was required to match that of a standard, upon the addition of an appropriate "spike",

I) retention time of the

2) detector response had to increase

3) the compound had to exhibit its documented

absorbance maximum as well as several lesser absorbance peaks.

The ratios of the absorbance

1056

maximum to the corresponding

lesser peaks were required

to match those determined

using

standards.

Microbiological Assays:

ATP was determined

photometrically

At each site, approximately scintillation

vials containing

following

the method of Portier

(pers. comm., 23).

one gram of sediment was placed in preweighed,

9 ml of pH 7.4

phosphate buffer.

sterile,

These were stored on ice

until analysis

which occurred no more than 12 hours after collection.

to equilibrate

at room temperature

Samples were allowed

for three hours prior to analysis at which time the

sample vials were dried and weighed to determine

the actual weight of sediment collected.

100 ~i of sample was reacted with 100 ~i of a releasing agent in a 5 ml glass tube and placed

in an ATP phtometer.

specific

for bacterial

The releasing agents

(Lumac Systems,

(23).

100 ~i of luciferin/luciferase

ATP-dependent

and the resultant

detected and recorded as relative standard and background to calculate

corrected

protoctists,

The mixture was then treated with evolution of light was

For each run, "quench"

determinations

in the results.

The corrected

was conferred

culture exclusively

to the linear range of an ATP standard curve and were Conversion

of RLU to cell

is neither required nor usually employed.

(24) and Jensen's

(25) media were used in pour plate procedures

fungi and bacteria respectively.

~g/ml to Jensen's media to inhibit overgrowth Meiofauna

community

by the releasing agents.

for the purposes of biomass comparison between sites.

Both Martin's

RLU values

of total ATP of a specific microbial

fungi) and this specificity

number or cell density

of a known ATP

These values as well as sample weight were used

RLU which are reported

All RLU values were referenced appropriate

light units (RLU).

RLU were recorded.

direct photometric

(bacteria,

FL) were

or somatic cells and allowed for permeable release of nucleotides

without cell lysis or action by cellular enzymes

represent

Titusville,

Cycloheximide

by filamentous

to

(Sigma) was added at 40

fungi

(23).

(sediment biota retained on a 500 ~m sieve after passing through a I mm

sieve) were collected

from each site using a 3-cm corer.

cm which was expected

to contain over 95 % of the total meiofauna

treated with a formalin/rose

bengal solution,

wet-sieved,

all meiofauna were counted with a Nikon dissecting

Samples were taken to a depth of 8 (26).

Core samples were

rinsed with distilled water,

and

microscope.

RESULTS AND DISCUSSION

The concentrations presented

in Table I.

of PAHs in sediment and water samples These data are in general agreement

analyses of Bayou Bonfouca creosote Sediment presented

characterization

in Tables

by Laseter

from Bayou Bonfouca are

with the GC-mass spectrometric

(27).

data are presented

in Tables 2 and 3.

2, 4, and 5 were generated by Duncan's Multiple

a 0.05 experimentwise

error.

indicated highly significant

All statistics

Range Tests

(DMRT) with

The DMRTs were conducted after analysis of variance differences

(P < 0.01) between the reference

(ANOVA)

(site I) and the

1057

spill areas (sites 2-4).

All non-significant ANOVAS (P > 0.05) were reflected by non-

significance in the DMRTs which are presented in the tables.

Table

1.

Concentrations o f PAHs i n S e d i m e n t s a n d W a t e r f r o m B a y o u Bonfouca, Slidell, Louisiana (Parts per million)

Site

PAH Compound

Surface Water

Sediments

I

............

3 unknowns

3-5 unknowns

2

Naphthalene Fluorene Phenanthrene Anthracene Fluoranthene Pyrene Benzo(J)fluoranthene/ benzo(k)fluoranthene*

3

4

Naphthalene Fluorene Phenanthrene Anthracene Fluoranthene Pyrene Benzo(J)fluoranthene/ benzo(k)fluoranthene Benzo(a)pyrene

Naphthalene Fluorene Phenanthrene Anthracene Fluoranthene Pyrene Benzo(j)fluoranthene/ benzo(k)fluoranthene Benzo(a)pyrene

* Isomers not resolved.

8.3 7.6 28.7 14.7 27.1 18.3

1380 358 435 107 608 178

4.9

75

0.7 0.6 2.3 0.4 1.2 2.1

7720 7720 17670 1110 3360 800

nd** 0.3

940 40

14.1 12.3 155.O 39.7 110.0 85.0

7117 29310 1650 6580 1660

5.5 6.6

2280 610

** Not detected.

As can be seen from examination of Tables I-3, the most prominent differences between sites were creosote content, organic matter (OM), redox potential (Eh), pH, Zn, and Ca concentrations.

The particle size distributions indicated closely related sediment types

with sites I and 2 bordering between "silt loam" and "sandy loam", and sites 3 and 4 being "silt loam" (Table 3).

The OM contents varied considerably between sites and the presence

of poorly degraded plant material in the vertical sediment profiles of sites 2-4 suggested that this was the result of low saprophytic activity.

Since site I had low OM and no

detected creosote, the increasing presence of OM in sites 2-4 was likely the result of creosote toxicity to saphrophytlc organisms.

1058

T a b l e 2.

Sediment C h a r a c t e r i s t i c s Site

1

2

3

4

Organic Matter (%)

x- 3.4a si 0.2

9.5b 0.06

16.4c 0.7

32.3d 0.66

pH

x- 7.4a sI 0.2

7.6ab 0.2

8.2b 0.3

I0.4c 0.7

Eh (mV)

xi -214a s- 115

-I04b 52

-99b 63

-35b 57

NI 3, s- standard deviation. Means (x) followed by the same letter on a horizontal line are not significantly different at pI 0.05.

The Eh values for each site appeared to be related to the creosote concentrations as well.

At site I, Eh values showed strongly reduced conditions resulting from limited oxygen

flux to the sediments (as a result of flooding) and metabolically active microbial communities.

At sites 2, 3, and 4, the redox potentials were progressively less reducing as

creosote levels increased.

This Eh trend may be interpreted in two ways: (I) microbial

metabolic processes were limited in the spill areas, or (2) higher energy redox systems (ie., NO 3_ -> NH3/NH4 + , or Mn(III, IV) -> Mn(II)) predominated in these areas.

Since all

sites were permanently flooded, well supplied wlth OM, similar in grain size, and comparable in terms of Mn and Fe concentrations,

T a b l e 3.

the latter interpretation is unlikely.

S e l e c t e d Sediment P r o p e r t i e s Site

I

Clay (%) Silt (%) Sand (%) Creosote (%) * Cu (~g/g) Zn Cd Pb Ni As Fe Mn Ca Mg Mo A1

10 68 22 0 2 30 4 30 4 35 5590 51 714 900 8 9700

2

3 49 48 0.8 10 80 6 80 2 25 6200 73 1900 580 6 10300

3

4

4 66 30 10

5 46 49 25

12 115 10 52 16 135 7320 193 23400 3080 8 10600

8 80 13 32 4 37 4300 117 49000 1340 5 6660

Estimated from phenanthrene concentrations in samples and source creosote.

In the absence

1059

of biolimiting factors it would be expected that all sites would demonstrate strongly reducing conditions similar to site I. Sediment pH values at some sites were surprisingly high initially.

Upon further

investigation, the trend of increasing pH at sites 2-4 was thought to be related to the the progressively higher levels of Ca, probably introduced by runoff of lime from a local concrete plant (Table 3).

It is also probable that the high levels of creosote in the

sediments of sites 3 and 4 caused electrode interference and artificially high pH values. Further, although the pH values were in some cases "significantly different" from the control, there was a difference of less than I pH unit between sites I, 2, and 3, and this was not considered to be biologically important.

Site 4, however, had higher pH values and

this may have had an impact on benthic organisms, but relative to the high creosote concentrations also found at this site, the pH was thought to be of minor importance, particularaly with respect to microorganisms. soils and sediments are influenced by pH.

It should be mentioned that measured Eh in

A pH correction on measured Eh is difficult to do

in natural environments though it is known that increasing pH is accompanied by decreasing Eh values.

Thus it is important to point out that if appropriate pH correction factors

could be applied to the Eh values presented in Table 2, the more contaminated sites would indicate an even greater difference relative to the control area. The metals concentrations reported in Table 3 represent "potentially bioavailable', levels, ie., not including metals contained within the lattice structure of clay minerals. These metals were most likely tightly bound to sediment constituents and not readily available, hence not significantly bioinhibitory relative to other sources of toxicity. The results of the ATP analysis of the mlcrobenthos and direct counts of meiofauna are presented in Tables 4 and 5 respectively.

These data show that the abundances of viable

bacteria, fungi, and protozoa at sites 2, 3, and 4 were much lower than site I.

DMRTs of

all communities from site I against sites 2, 3, and 4, showed significant decreases in these communities with the means of each site decreasing with increasing creosote.

Meiofauna

counts show analogous reductions in response to increasing levels of creosote and this may be related to depressed microbenthic activity as well.

Table 4.

Microbenthic Community Analysis RLU/g sediment

I

Bacteria

x-

Site 2

3

4

s-

22619a 7768

9117b 2710

5501bc 6686

95c 28

Protozoa

xs-

19911a 5731

5857b 1715

4951bc 5690

78c 31

Fungi

~s-

6983a 6792

327b 552

136b 207

N= I0, s- population std. dev. at P- 0.05.

3b 6

Means (2) with same letter are not significantly different

1060

Table 5. Meiobenthic Community Analysis Organisms/10 cm Site

1

2

3

4

Nematodes

x= s=

91a 20

14b 21

Ob 0

Ob 0

Oligochaetes

x= s=

20a 13

16ab 15

Ob 0

Ob 0

Other

x= s=

7b 8

Ob 0

Ob 0

38b 38

Ob 0

Ob 0

Total Melofauna

22a 7

x= s=

133a 20

N=3, s= population

std. dev.

Means wlth the same letter are not significant

at P= 0.05.

Viable plate count results are given in Table 7 and support the interpretations preceedlng

sections

in that there is a creosote-dependent

fungal colony forming units

decrease

of

in both bacterial

and

(CFU).

Table 6.

Summary of P l a t e Count Results CFU/Plate Slte

I

Bacteria

xs=

TNTC --

Fungi

x= s=

58 9

2

3

351 118

116 47

40 6

39 6

4

71 22 0.25 0.40

N= 12, s= std. dev. Colonies

too numerous

to count. Count stopped at CFU= 500 in all samples.

CONCLUSIONS

The results of this study indicate that the high levels of PAHs in the sediments of large areas of Bayou Bonfouca adversely was manifested creosote levels more oxidizing.

at all of the trophic increased,

detrital

affected micro- and melobenthlc

communities

and this

levels studied as well as in sediment properties. accumulations

also increased and redox potentials

These phenomena were related to a reduction of saprophytic

As became

biomass relative

106 1

to the control area.

The removal of fungi in polluted sites was probably the major factor

in detrital accumulation since fungi are of primary importance in terms of litter degradation (28).

The reduction of bacterial biomass was thought to be the primary cause of

increasing redox potentials.

The association of measured high levels of PAHs with

alterations of the physical-chemical characteristics of the sediments is considered to be the primary finding of this research.

Attention is drawn to the biochemical findings in

hopes that the methods described in this work will be applied and expanded in future research and that the concept of employing trophic biomass measurements for the evaluation of pollutant impacts in natural systems will be subjected to further study.

ACKNOWLEDGEMENTS

The authors thank Walter B. Sikora, Jean P. Sikora, and Samuel P. Meyers for advice, materials, and critical review of this research.

Thanks are extended to Michael Bender,

Richard Wetzel, John Zeigler, and Ruth Hershner for further review and support as well as to the Virginia Institute of Marine Science for extending facilities and editorial services for the final preparation of this manuscript.

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