Environmental aspects of acid sulphate soils - ROOT of content

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Release of trace metalsSeveral trace elements may accumulate together with Fe in sedimentary pyrite, eithersubstituting for Fe in pyrite (notably Ni and Co), or in related sulfides (Cu, Zn, Pband As) (Deer, Howie and Zussman 1965). These elements will be released duringpyrite oxidation. Extreme acidification due to pyrite oxidation should also lead torelease of trace metals from other minerals. Research on the release of potentiallytoxic heavy metals during acid sulphate soil formation is rare. Satawathananont (1986)observed concentrations of water-soluble Cu, Zn, Mo, Cd, Pb, Ni and As that wereabout an order of magnitude higher in an aerated pyritic soil (pH 2.9) than in threewell-developed acid sulphate soils (pH 3.9-4.5) and one non-acid marine soil (pH 4.9)from the Bangkok Plain. Also, after incubation under controlled Eh-pH in acid oxidizedconditions for two weeks, water-soluble trace metals were higher in the pyriticsoil than in the older leached soils (Table 1). Palko and Yli-Halla (1988,1990) observedsimilar contents of total Cr, Cu, Zn, Co, and Ni in acid sulphate soils and non-acidsoils from Finland, suggesting that pyrite formation did not cause accumulation ofheavy trace metals. Levels of soluble trace metals, however, were highest in the acidsulphate soils. These data indeed suggest that pyrite oxidation and associated acidificationmay release significant quantities of soluble trace metals.Release of + Al3Interest in the concentration of dissolved Al3+ stems from its potential toxicity toplant roots and to fish at concentrations exceeding 0.02 mg I-' to 10-50 mg I-', dependingon variety or species and growth stage (Thawornwong and van Diest 1974, Singhet al. 1988). Virtually concurrent with the decrease in pH during acidification frompyrite oxidation, dissolved AI is released, presumably by dissolution of clay minerals.Over a wide range of conditions in Thai acid sulphate soils, from pH below 2 in oxidizingpyritic soil in the laboratory, to pH close to 5 in old leached acid sulphate soilsin the field, activities of Al3+ obeyed the relationship [A13+][S0,2-][OH-] = 17.3, suggestingcontrol of dissolved Al by equilibrium with a basic sulphate AIOHSO, (vanBreemen 1973). This relationship was confirmed for Thai acid sulphate soils (Mooreand Patrick 1991) and for Indonesian acid sulphate soils (Groenenberg 1990). It couldbe explained by equilibrium with the mineral jurbanite, A10HS0,.5H20 (Nordstrom1982). Jurbanite, however, has never been identified in acid sulphate soils. Nevertheless,the empirical relationship appears to be useful in predicting AI concentrations.Sulphate activities vary relatively little in most acid sulphate soils, so constant valuesof [AI3+][S0,2-][OH-] imply that the activity of Al3+ increases about tenfoldTable 1 Contents of water-soluble trace elements (mg I-') in stirred soil suspensions (200 g of soil, 800ml of water) maintained at Eh= 400 mV and pH=3.5 for two weeks. Bang Pakong is a pyriticsoil, the others are surface soils of well developed acid sulphate soils. Data from Satawathananont(I 986)Soil Zn Cu Cd Pb Cr Ni AsRangsit very acid 16 0.55 0.29 2. I 0.35 3.0 2.8Rangsit 19 0.34 0.15 I .2 0.30 4. I 2.4Mahapot 18 0.89 0.23 I .9 0.46 7.3 2. IBangPakong 42 1.12 0.75 6.6 0.69 10.5 9.9394

with a one unit decrease in pH. At pH < 4 the same relationship, approximately, holdsalso for the concentration of total dissolved Al. A roughly tenfold increase in theconcentration of dissolved AI per one unit pH decrease, indeed, follows from datapresented for acid sulphate soils by Satawathananont (1986) and by Hanhart andNi (1991) inVietnam.It remains to be seen whether [A13+][S0,2-][OH-] remains constant under evaporativeconditions, when highly soluble Al-sulphates (alum and pickeringite) precipitate, andin acidified surface waters. At least in open waters, Al3+ may simply behave conservatively,i.e. without regulation of its concentration by some solid phase, as shown byNordstrom and Ball (1986) for acid mine waters.Release of SO2Gaseous SO, is released during oxidation of sulphides and can be used in prospectingfor sulphide ores. The distinct sulphurous odour that can be noticed, sometimes, indrained mangrove marshes may also be attributed to SOz. There are indications fromacid-base budgets for whole soil profiles that a very large fraction of the potentialacidity present in pyritic sediments leaves the soil in unneutralized form as SO, (vanBreemen 1976). If this were true, oxidation of pyritic sediments is a source of air pollution,and could contribute to ‘acid rain’. In view of increasing SO, emissions fromindustrial sources e.g. in South East Asia (Rohde and Herrera 1988), a study of thebackground SO, concentrations and the possible contribution of acid sulphate soilsis relevant.Oxidation of Fe11The reactivity of Fe111 with pyrite (Equation 2) accounts for a high mobility of ironin zones of active pyrite oxidation, and for a failure of solid Fe111 to precipitate adjacentto pyrite, except at high pH or at exceptionally high rates of oxidation. WhereFeSO,,,, derived from pyrite (Equation 1) is transported before being oxidized to hydratedFe111 oxide, further acidification takes place at some distance from the pyriticzoneSuch ‘delayed’ acidification can be observed in shallower soil horizons, in pondedfields where FeSO,,,,, diffuses upward through cracks from the pyritic subsoil, in tubedrains and in open waters.Rapid oxidation of Fe2+, especially at low pH, is mainly due to autotrophic ironbacteria. In addition to acidification, clogging of drain tubes (Bloomfield and Coulter1973) and of fish gills (Singh et al. 1988) by FeIII(hydrous)oxide may be among theunwanted effects of reaction 4.In not-too-deeply-drained, highly organic acid sulphate soils in perhumid climates,oxidation of Fe2+ according to equation 4 seems to be hampered (Konsten et al., inpreparation). Restricted oxidation of Fe2+ may be due to insufficient aeration or toprotection of Fe2+ from O, by dissolved organic substances. Leaching of most of theiron derived from pyrite would explain the formation of acid sulphate soils with littleor no mottling from Fe111 oxide or jarosite. Such iron-poor acid sulphate soils395

differ from Fe-rich acid sulphate soils in their behaviour after flooding and reduction,as discussed below.Reduction processesReduction of redox elements that are common in soils, such as Fe, Mn, S, and N,consumes protons and is responsible for the increase in pH commonly observed inacid soils after waterlogging. Increased pH upon flooding is the main reason whywetland rice cultivation is succesful on acid sulphate soils. While the increase in pHand associated decrease in dissolved Al3+ are favourable for the crop, other changesfollowing reduction are not. These include the formation of other potentially toxicsubstances, such as Fe2+, organic acids and HzS, in the course of soil reduction. Moreover,soil reduction or pH increase following soil reduction are often limited in acidsulphate soils.Reduction of Fe111 and its chemical consequencesIn most moderately acid soils (pH 4-6), waterlogging causes an increase in pH to avalue between 6 and 7 after several weeks of flooding. Usually, reduction of Fe(ll1)to Fe(I1) is quantitatively the most important process involved in this rise in pH (Ponnamperuma1972, Patrick and Reddy 1978).Equation 5 illustrates that protons are consumed in the reduction of Fe(I1I) oxides,with organic matter (‘CH,O’) as the electron donorFe20~+ 1/2CH,O(,,) + 4H+(,,, + 2Fe2+Cdq) + 1/2COz,g,,,) + 5/2Hz0,,) (5)Hypothetical changes in pH and the concentration of Fe2+ upon reduction of soilswith various proton donors are indicated in Figure I. In acid sulphate soils, theseprotons can be derived from free sulphuric acid and desorption of adsorbed sulphate,producing soluble ferrous sulphate, according to pathway d. In acid soils with littlefree acidity and sulphate, hydroxylation of exchangeable Al3+ during reduction ofFeIII produces Al hydroxide plus exchangeable FeZ+ (pathway a). In slightly acidto near neutral conditions, CO, may serve as a proton donor, producing HCOq plussoluble Fe2+ (pathway c), part of which may be exchanged for other cations (pathwayb). The increase in pH and in the concentration of dissolved Fe2+ stops when saturationwith ‘Fe(OH),’ has been reached. By that time, acid sulphate soils have a somewhatlower pH and much higher levels of dissolved Fe2+ (pathway d-c) than acid ‘nonsulphate’soils (pathway a-c), and than slightly acid soils with appreciable amountsof exchangeable bases (pathway b). Sulphate reduction, which may follow reductionof FeIII, produces HzS and HCO). This causes a further increase in pH but tendsto decrease dissolved Fe2+ by precipitation of FeS so that, ultimately, pH and dissolvedFe in flooded acid sulphate soils may reach the same values as in ‘normal’ floodedsoils.In most moderately acid wetland rice soils, the pH rises to equilibrium values between6.5 and 7 within a few weeks of flooding. The same is true for many very youngacid sulphate soils, where an increase in pH from 3-3.5 to 5.5-6 is associated with‘Fe(OH)2’ is a proxy for the unknown Fell-containing hydroxide precipitates which form the bulk ofsolid Fe11 in most seasonally-reduced soils, with an apparent solubility product of about (van Breemenand Moormann 1978)396

1 o3[Fe2’]mg.1-‘1 o210’I I I4 5 61 iPH..Figure 1 Hypothetical changes in the concentration ofdissolved Fe2+ and pH in the course of soil reduction(van Breemen.1988). Dotted lines refer to H2S concentrations (mg 1-’) in equilibrium with Fe2+.Maximum concentrations Fe2+ are determined by the solubility of ‘Fe(OH)2’, as indicated bythe bold line. .Different arrows refer to different proton donors (exchangeable Al, CO2 andadsorbed SO4), with and without formation of exchangeable Fe2+, as follows:a FeOOH + 1/4CH@ + 2/3 Al3+(,,,,) + 1/4H2O +Fe2+(exctq + 2/3AI(OHh(s) + 1/4co2b FeOOH + 1/4CH20 + 7/4C02 + M2+(,,,h) + 1/4HzO +Fe2+(,xdlj + M2+(,,) + 2HC03-(,,)c FeOOH + 1/4CH20.+ 7/4co2 + 1/4H20 +Fe2+(,,) + 2HC0-3(,,)d FeOOH + 1/4CH20 S042-c,d,j + 1/4H20 +Fe2+(,,) + + 1/4co2 + 20H-(,dS)a steep rise in dissolved Fe2+. In most older acid sulphate soils, however, the pHincreases very slowly after waterlogging and, sometimes, does not reach the valuesbetween 5.5 and 6.5 indicated in Figure I (Ponnamperuma 1972, van Breemen 1976).The reasons for this behaviour have not been studied explicitly. A slow rise in pHcan be attributed to (i) slow reduction or (ii) appreciable reduction (fermentation)in the absence of inorganic reducable substances, e.g Fe111 oxides (Ponnamperuma1972, van Breemen 1976, Munch and Ottow 1982). In case (i), neither Eh nor pHwill change much after flooding. In case (ii), the Eh will drop without concomittantincrease in pH. Slow reduction has often been observed, and has been attributed toa low content of metabolizable organic matter (Kawaguchi and Kyuma 1968, Ponnamperuma1972, Van Breemen 1976), and/or to adverse effects of low pH, high dissolvedAI, and poor nutrient status on the activity of anaerobes (Kawaguchi andKyuma 1968, van Breemen 1976). The strong reduction, and associated increase inpH upon flooding of very young acid sulphate soils, suggests that the presence ofrelatively undecomposed organic matter from the original mangrove vegetation and397

high nutrient status may be more important for strong reduction than a low pH byitself.Some acid sulphate soils in Kalimantan, Indonesia, show or no increase in pH afterreduction following flooding. This has been attributed to low contents of Fe111 oxidesrelative to the base neutralizing capacity of the soil (mainly exchangeable acidity associatedwith organic matter) (Konsten et al., in prep.). Apparently, the combinationof highly organic parent material and perhumid climate limits oxidation of Fe11 andaccumulation of appreciable quantities of Fe111 oxides and jarosite. This would explainwhy the acid sulphate profiles typical of monsoonal climates, with horizons of accumulationof Fe111 oxide and jarosite at increasing depth as soils become older (van Breemenand Pons 1978), are lacking in Kalimantan, as well as in other highly organicacid sulphate soils perhumid climates. The strong leaching of iron thus appears tohave important consequences, agronomically as well as for soil genesis.Reduction of sulphate and fermentation reactionsSulphate reduction also consumes protons and helps to increase soil pHSulphate reduction is generally absent or very slow at pH values below 4 to 5 (BaasBecking et al. 1966, Connell and Patrick 1966, Nhung and Ponnamperuma 1966).Yet sulphate reduction often occurs in waterlogged young acid sulphate soils, andupon prolonged flooding in older acid sulphate soils. In acid sulphate soils, sulphatereduction is, probably, mainly a very local phenomenon, e.g. immediately adjacentto concentrations of fresh decomposing organic matter (Hanhart and Ni 1992). H2Sis highly toxic: O. 1 mg I-' of H,S may be toxic to rice in water culture (Mitsui 1964).Amorphous Fes probably regulates the concentrations of H2S in flooded soils (vanBreemen and Moorman 1978). Fig. 1 shows that high concentrations of both H2Sand Fe2+ can coexist in the presence of Fes at relatively low pH, which illustratesthe potential danger of sulphate reduction in acid sulphate soils. Hanhart and Ni (1992)attributed the positive effect of regular shallow drainage of acid sulphate soils thathad been flooded for a long time to the oxidation of H2S.A number of organic acids that form by fermentation in highly organic floodedsoils can be harmful to rice at concentrations in the order of 0.1-1 mmo1 I-'. Highconcentrations of reducing organic substances are common in peaty soils and chemicallypoor, sandy soils low in active iron, where the pH stays low after flooding (Okazakiand Wada 1976). Possibly, such substances are important, too, for rice growingon acid sulphate soils with a low pH during flooding.Measures to decrease acidificationCurtailing pyrite oxidationPyrite oxidation can be decreased by limiting the supply of O2 or by influencing therate of one or more of the intermediate steps in pyrite oxidation. For example, oxidationrates can be limited by decreasing the concentration of Fe3+, so that reaction2 is hampered. Pulford et aL(1988) slowed down oxidation of pyrite in coal mine wastein the laboratory by (i) decreasing the rate of oxidation of Fe2+ to Fe3+ (through398

Breemen, N. van 1976. Genesis and soil solution chemistry of acid sulphate soils in Thailand. Agric. Res.Rep. 848, Pudoc, WageningenBreemen, N. van 1987. Effects of redox processes on soil acidity. Neth. J. Agric. Sci. 35,271-279Breemen, N. van 1988. Effects of seasonal redox processes involving iron on the chemistry of periodicallyreduced soils. In J.W.Stucki et al. (editors) Iron in Soils and Clay Minerals, D Reidel Pub1 Co, Dordrecht797-809Breemen, N. van, and F.R. Moorman 1978. Iron-toxic soils. In: International Rice Research Institute:Soils and Rice. Los Baños 781 -800Breemen, N. and L.J. Pons 1978. Acid sulphate soils and rice. In: International Rice Research Institute:rice and soils. Los Baños 739-761Brinkman, R. and L.J. Pons 1968. A pedogeomorphological classification and map of the Holocene sedimentsin the coastal plain of the three Guyanas. Soil Survey Papers 4, Soil Survey Inst. WageningenConnell, W.E. and W.H. Patrick 1969. Sulphate reduction in soil: effect of redox potential and pH. Science159,86-87Deer, W.A., R.A. Howie and J. Zussman 1965. An introduction to the rock forming minerals. Longmans,LondonDent, D.L. 1986. Acid sulphate soils: a baseline for research and development. Publ. 39, InternationalInstitute for Land Reclamation and Improvement, WageningenDent, D.L. 1992. Reclamation of acid sulphate soils. Adv. Soil Science 17,79-122. Springer Verlag, New YorkDost, H. editor 1973. Acid sulphate soils: proceedings of the international symposium, Wageningen. Publication18, International Institute for Land Reclamation and Improvement, WageningenDost, H. editor 1988. Selected papers of the Dakar symposium on acid sulphate soils. Publication 44, InternationalInstitute for Land Reclamation and Improvement, WageningenGroenenberg, J.E. 1990. Modeling of solute transport and chemical processes in acid sulphate soils. In:AARD & LAWOO: Papers Workshop on Acid Sulphate Soils in the Humid Tropics, Bogor: 182-194Hamming, A.F.J., Kasdi Subagyono, and Tagus Vadari 1990. Soil permeability aspects in Pulau Petak,Kalimantan. In: AARD & LAWOO: Papers Workshop on Acid Sulphate Soils in the Humid Tropics,Bogor: 295-332.Hanhart, K. and Doung Van Ni 1991. The effect of water management treatments on the cultivation ofan irrigated dry season rice crop on a severe acid sulfate soils in Hoa An Station, Viet Nam. VH IOReprt, in prep.Holst, A.F. van and G.J.W. Westerveld 1973. Corrosion of concrete foundations in (potential) acid sulphatesoils and subsoils in the Netherlands. In H.Dost (ed.) Acid sulphate soils. Proceedings of the internationalsymposium Wageningen. Publication 18,11, 373-382, International Institute for Land Reclamation andImprovementKamerling, E. 1974. Bodemfysisch en agrohydrologisch onderzoek in de jonge kustvlakte van Suriname.Versl. Landb.k. Onderz. 825. Pudoc, Wageningen.Kawaguchi, K. and K. Kyuma 1968. Fertility characteristics of the lowland rice soils in some SouthernAsian countries. Transact. 9th Int. Congr. Soil Sci., Adelaide, Intern. Soc. Soil Sci. &Angus and Robertson,vol IV, 19-31Konsten, C.J.M., N. van Breemen and Supardi Suping, I.B. Aribawa and J.E. Groenenberg. Factors limitingthe rise of pH upon flooding in acid sulphate soils used for lowland rice in Kalimantan, Indonesia (inpreparation)Mensvoort, M.E.F. van, Duang Van Ni and J. van der Schans 1991. Improvement of acid sulphate soilsby leaching with salt or brackish water. In: P.Deturck and F.N.Ponnamperuma (editors). Rice productionon acid soils of the tropics. Inst. Fundamental Studies, Kandy p 219-224Mensvoort, M.E.F. van, and Le Quang Tri 1988. Morphology and genesis ofactual acid sulfate soils withoutjarosite in the Ha Tien Plain, Mekong Delta, Viet Nam. In H.Dost 1988. 11-15Mitsui, S. 1964. Inorganic nutrition, fertilization and soil amelioration for lowland rice. 2nd ed. Yokendo,TokyoMoore, P.A. and W.H. Patrick 1991. Aluminium, boron and molybdenum availability and uptake by ricein acid sulphate soils. Plant and Soil 136, 171-18 IMoormann F.R. and N. van Breemen 1978. Rice: soil, water, land. IRRI, Los BañosMunch, J.C. and J.C.G. Ottow 1982. Einfluss von Zellkontakt und Eisen(II1)-Oxidform auf die bakterielleEisenreduktion. Z. Pflanzenernaehr. Bodenk. 145,66-77Nae Joung Park, Joung Sun Park and Yung Sup Kim 1971. Effect of lime on growth of rice and changesin pH, Eh, Fe2+ and AI in an acid sulfate soil. J. Korean Soc. Soil Science and Fertilizer, 4: 167-175.40 1

.Nhung, M.M. and F.N. Ponnamperuma 1966. Effects of calcium carbonate, manganese dioxide, ferrichydroxide and and prolonged flooding on chemical and electrochemical changes and growth of rice ina flooded acid sulphate soil. Soil Sci. 102,29-41Nordstrom, D.K. 1982. The effect of sulfate on aluminum concentrations in natural waters: some stabilityrelations in the system AIZO,-SO3-HzO at 298 K. Geochim. Cosmochim. Acta 46,681-692Nordstrom, D.K. and J.W. Ball 1986. The geochemical behaviour of aluminum in acidified surface waters.Science 232,54-56Okazaki, M. and H. Wada 1976. Some aspects ofpedogenic processes in paddy soils. Pedologist 20,139-150Palko, J. and M. Yli-Halla 1988. Solubility ofCo, Ni and Mn in some extractants in a Finnish acid sulphatesoil area. Acta Agric. Scand. 38, 153-158Palko, J. and M. Yli-Halla 1990. Solubility of AI, Cr, Cn, and Zn in soils from a Finnish acid sulphatesoil area. Acta Agric. Scand. 40, I 17- I22Patrick, W.H. and C.N. Reddy 1978. Chemical changes in rice soils. In: Soils and Rice. IRRI, Los Baños361-379Ponnamperuma, F.N. 1972. The chemistry of submerged soils. Adv. Agron. 24,29-96Prokopovich, N. 1988. Engineering aspects of acid sulfate deposits in California, USA, In H.Dost (editor)Selected papers of the Dakar symposium on acid sulphate soils. Publ. 44, 49-58. International Institutefor Land Reclamation and Improvement, WageningenPulford, I.D., C.A. Backes and H.J. Duncan 1988. Inhibition of pyrite oxidation in coal mine waste. InH.Dost (editor) 1988,59-67Rohde, H. and R. Herrera (editors) 1988. Acidification in tropical countries. Scope 36. John Wiley &i SonsSatawathananont, S. 1986. Redox, pH and ion chemistry of acid sulfate rice soils in Thailand. PhD Dissertation.Louisiana State UniversitySingh, V.P., T. Poernomo and R. Brinkman 1988. Reclamation and management of brackish water fishponds in acid sulphate soils: Philippine experience. In H.Dost (editor) 1988,214-228Sterk, G. 1991. Leaching acidity from the topsoil of raised beds on acid sulphate soils in the MekongDelta, Vietnam. Techn. Rept. no 8, EEC Project STD-Vietnam, Department of Soil Science and Geology,WAU, WageningenThawornwong, N. and A. van Diest 1974. Influence of high acidity and aluminum on the growth of lowlandrice. Plant and Soil 41, 141-159402

Seasonally recurrent fish mortalities andulcerative disease outbreaks associated withacid sulphate soils in Australian estuariesR.B. Callinan', G.C. Fraser' and M.D. Melville2NSW Fisheries, Regional Veterinary Laboratory, Wollongbar AustraliaSchool of Geography, University of NSW, Kensington, AustraliaAbstractAcid sulphate and potential acid sulphate soils are now known to be widespread onthe coasts of Australia, particularly in northern and eastern areas. The onset of heavyrain in these areas causes a 'first-flush' runoff and drainage of phytotoxic water withproperties including low pH and high concentrations of dissolved aluminum. Thesewaters have caused massive fish kills. Recently, a new ulcerative fish disease, epizooticulcerative syndrome (EUS), has shown a pattern of seasonal recurrence in EasternAustralia also relating to these onset rains. However, the pattern of this disease'sspread through Australia and Southeast Asia strongly suggests involvement of an exoticinfectious agent. The oomycete'fungus, Aphanomyces sp. has been consistently isolatedfrom ulcers but it is unable to invade the intact skin of healthy fish. Early indicationssuggest that chemical properties associated with water draining from acidsulphate soil areas cause sublethal skin damage that can allow fungal invasion. Thereis a clear spatial and temporal association between onset rains, drainage from acidsulphate soil areas and outbreaks of EUS, although the details of the disease processhave yet to be established.This disease threatens a major protein resource for human consumption in the Asia-Pacific region, where population growth pressure and need for economic developmentare great.Our ongoing research intends to establish, through field and laboratory studies,the role of water quality and hydrological parameters in the pathogenesis of EUS.This will allow better management of acid sulphate soil areas, thereby enhancing sustainabilityof estuarine fisheries.IntroductionAcid sulphate soils and potential acid sulphate soils are widely distributed in tidalriver flood plains in eastern and northern Australia. The sulphidic layers in these soilsacidify periodically under natural conditions, as in prolonged periods of dry weather,or following changes to flood plain hydrology, when backswamps and freshwaterlagoons are drainend by natural processes or human intervention.Recent studies in Australia have demonstrated probable causal relationships betweenmajor rain events, the presence of significant areas of acid sulphate soil in riverfloodplains and certain seasonally recurrent fish mortalities. Studies of epizootic ulcerativesydrome (EUS), a new disease of freshwater and estuarine fish in Australia, have403

suggested similar water quality changes may be involved in its pathogenesis.In this paper we briefly review the findings of these studies and discuss possiblemechanisms responsible for death or ulceration in fish exposed to water derived fromareas of acid sulphate soil.Seasonally recurrent fish mortalitiesA fish kill may be defined as any unusual increase in mortality and morbidity, dueto infectious or non-infectious causes, in a fish population.There have been several reports of seasonally recurrent fish kills in the Magela Creeksystem, part of the East Alligator River system in northern Australia. These fish killstypically occur during the transition from the dry to wet season, when ‘first-flush’water enters lagoons and other permanent water bodies. Brown et al. (1983) describeda major fish kill in a freshwater lagoon on Magela Creek which they attributed tohigh levels of toxic aluminum (up to 0.5 mg 1-I), a consequence of natural acidic waterrunoff. Hart et al. (1987) studied water quality in the Magela Creek system duringa dry-to-wet season transition and found that ‘first-flush’ water flowing across thefloodplain was acidic (pH about 4-5) with high conductivity (about 750 pS cm-’) andhigh sulphate concentrations (about 200 mg 1-I). They concluded that the source ofthe acidity, dissolved salts and sulphate, as well as high concentrations of metals, particularlyaluminum, was groundwater brought to the surface by rising watertablesin acid sulphate soil areas of the floodplain.Massive fish kills following major rain events have also been associated with acidicwater and high concentrations of aluminum in major sections of the Tweed Riverin northern New South Wales. The acidic water is derived from runoff or drainagefrom the extensive areas of potential acid sulphate soil in the floodplain. In 1987,a fish kill on the Tweed River was associated with pH values as low as 3.6 and dissolvedaluminum concentrations of 2.5 mg 1-’ in major sections of the main stream (Fraser,unpublished).Low pH, below 3-4, is directly lethal to móst fish species, causing disturbances towater and ion regulation, as well as to oxygen transport mechanisms (WendelaarBonga and Dederen 1986). However, elevated concentrations of inorganic, cationicaluminum species (less than 0.1-5 mg 1-I) are thought to be primarily responsible forinjury and death of fish in naturally acidified waters. These increased aluminum concentrationsresult, under acid conditions, from mobilisation of aluminum from watershedminerals (Driscoll et al 1980, Langdon 1988). In acidic water, inorganic aluminumaccumulates in, and injures, fish gills, causing reductions in enzyme activity and lethalosmoregulatory disturbances (Staurnes et al 1984, Witters et al 1990). Other waterquality attributes modify the toxicity of inorganic aluminum to fish; there is evidencethat high calcium and silicon concentrations protect fish against aluminum toxicity(Brown 1983, Ingersoll et al 1990a, Birchall et al 1989). Humic substances (the endproducts of biological degradation of organic material) are also protective, bindingaluminum in a non-toxic, organic form (Witters et al 1990).In response to toxic acid/aluminum exposure, some fish species are able to acclimatize,via physiological changes, or undergo longer-term adaptation, via genetic selection(Mount et al 1990). These workers showed, however, that exposure to a 6-day ‘pulse’404

of acid water with high inorganic, monomeric aluminum and low calcium concentrations,caused significant mortalities in brown trout fry not previously acclimatizedto these conditions. It is likely that fish exposed to acid ‘first-flush’ water in Australianrivers are similarly unprepared, and that similar toxic mechanisms operate.Epizootic ulcerative syndromeEpizootic ulcerative syndrome (EUS), known colloquially in Australia as ‘red spotdisease’, is an ulcerative skin disease affecting estuarine and freshwater fish. EUS wasfirst reported in Australia from the Burnett River on the central Queensland coastin 1972 (McKenzie and Hall 1976). Since then, seasonally recurrent outbreaks havebeen recorded in many rivers on the East coast, from northern Queensland (Rodgersand Burke 1981) to southern New South Wales (Callinan, unpublished). Outbreakshave occured in southwest Western Australia since 1983 (Pass, unpublished) and inthe Northern Territory since 1986 (Pearce 1990). Serious outbreaks of the disease havealso occurred in Southeast and South Asia during the past decade (Anon 199 I).Losses due to EUS, primarily in cultured freshwater fish, were estimated at A$2.5million in Indonesia in 1980, A$ 10.9 million in Thailand in 1982 and A$4.2 millionin Bangladesh in 1988-89. EUS costs commercial estuarine fisheries on Australia’sEast coast approximately A$ 1 .million in discarded fish annually.Studies in North America have examined the possible long-term effect of ‘ulcerativemycosis’, a disease of estuarine species similar to EUS, on fishery sustainability (Merrinerand Vaughan 1987). Results suggested that an incremental decline of 0.5 percent per year in survival of young fish over a 30-year period would result in a reductionof 60 per cent of the normal expected biomass. Loss caused by EUS in Australianestuaries have not been accurately quantified but; assumming that up to IO per centof young fish of susceptible species die as a result of EUS outbreaks occuring onceevery 3 years, a similar long-term decline in biomass may result.The sudden appearance and pattern of spread of EUS in Australia and Asia is consistentwith the involvement of an exotic infectious agent. Studies examining possibleprimary causative roles for viruses, bacteria and metazoan parasites have, to date,produced negative results. However, in a study of the pathology of EUS, Callinanet al (1989) showed that massive invasion of the skin by oomycete fungi plays a centralrole in the induction of ulcers. Recently, Fraser et al (1992) recovered the oomycetefungus Aphanomyces sp. in apparantly pure culture from 27 of 28 early ulcers on 3estuarine fish species from 3 widely separated river systems in Australia. Histologicallyindistinguishable fungi are also consistently present in lesions of fish affected withEUS in Asia (Roberts et al 1989).These findings indicate that an Aphanomyces sp. is the causative infectious agentof EUS. However, attempts to induce typical lesions by exposing fish experimentallyto fungal spores were successful only when skin was abraded prior to exposure (Callinanand Fraser, unpublished). This finding suggests that factors other than simpleexposure to the fungus are necessary for EUS outbreaks to occur in wild fish populations.EUS outbreaks in eastern Australia typically begin about 2 weeks after periodsof prolonged heavy rainfall in lower river catchments. There is a growing body of405

evidence suggesting that these outbreaks occur only when susceptible fish are exposedto both Aphanomyces sp. propagules (spores and/or hyphae) and water having specificattributes. Further, there is an association between these water quality attributes andthe presence of significant areas of acid sulphate soils in the lower floodplains ofaffected rivers. Such areas are known to be present in floodplains of most rivers inAustralia from which EUS has been reported.Studies on the tidal floodplain of the Richmond River system in northern NewSouth Wales have demonstrated some relationships between major rain events andseveral water quality parameters. A submersible automatic water quality data logger,programmed to measure pH, dissolved oxygen concentrations, conductivity, temperatureand depth at 15-minute intervals, was placed in a tributary of the RichmondRiver immediately downstream of a typical, drained backswamp containing significantareas of acid sulphate soils. Water quality changes associated with a major rainevent are shown in Figure 1.The low pH of the water after the rain event was probably due to acidity leachedfrom acid sulphate soils in the catchment. The cause(s) of the low dissolved oxygenconcentrations are more difficult to explain; they may be associated with microbialdecomposition of suspended organic matter or from soil water from the active rootzone, but the clear temporal association between reductions in both pH and dissolvedoxygen concentrations suggests a common mechanism. One such mechanism involvesthe oxidation of iron IT (from pyrite oxidation) to ferrihydrite. Concentrations of toxicaluminum species were not measured but, given findings elsewhere, were likely to havebeen high. Following the pH decline, a moderate fish kill occurred at the study site.Related studies on the Richmond and Clarence Rivers have shown that, duringthe 2 weeks after major rain events, significant falls in dissolved oxygen concentrationsconsistently occur in most representative floodplain tributaries and at some main-22ODAYSFigure 1 Changes in pH, dissolved oxygen (D.O.) concentrations and depth in a tributary of the RichmondRiver, New .South Wales, downstream of an acid sulphate soils area. Data were recorded at15-minute intervals by a submersible automatic data logger. Rainfall at the site is also shown.406

stream sites. Falls in pH at mainstream sites may also occur. For example, on theRichmond River in May 1987 at Site 4 (Figure 2), dissolved oxygen concentrationsfell from 5.8 mg I-' to 3.3 mg I-' and pH fell from 7.2 to 5.6 within 9 days of a majorrain event. However, at Site 4 in April 1988, dissolved oxygen concentrations fell from5.0 mg 1-' to 1.2 mg I-' but pH fell only marginally, from 6.6 to 6.2, within 10 daysof a major rain event.Clearly, runoff or drainage from acid sulphate soil areas contributes to thesechanges, to an extent dependent on a complex of factors including rainfall patternspreceding the major rain event and the distribution of rainfall over the catchmentduring the major rain event. However, it is likely that a 'pulse' of acidic, deoxygenatedwater is discharged from these areas during the early stages of most major rain events.Experimental exposure of fish to water with low pH (Daye & Garside 1976, Linnenbachet al 1987) and high aluminum concentrations (Tngersoll et al 1990b, Tandjunget al 1982) results in alterations to epidermal structure and, in extreme cases, epidermalnecrosis. Low concentrations of dissolved oxygen may also injure fish epidermis.Plumb et al (1 976) described apparantly sterile haemorrhagic and necrotic lesions inskin and skeletal muscle of channel catfish Ictalurus punctatus, exposed to dissolvedoxygen concentrations of less than 1 mg I-' for several days. They suggested that thisepidermal damage allowed subsequent bacterial invasion and septicaemia. It is likelythat, in some sections of lower river systems, and for varying periods after major rainevents, 'first-flush' runoff water from acid sulphate soil areas causes sublethal waterFigure 2 Location on the lower Richmond River of mainstream sampling sites for EUS prevalence (1-14)and known areas of acid sulphate soils (A-D)407

Table 1 Prevalence of EUS in yellowfin bream (Acanthopagrus uusrrulis) and sand whiting (SiNago ciliuia)sampled at 14 mainstream sites on the Richmond River at 3-monthly intervals on 7 occasions during1988j89. Location of sites is shown in Figure 2Site Yellowfin Bream Sand WhitingTotal No. with Prevalence Total No. with Prevalenceexamined EUS % examined EUS Yo12345678910II12131427 114232019101561996380019433422022331157618123 I227I73216268813322OO2.212.711.422.427.922.43.24.12.45.914.36.4OO-34.845.042.534.331.0-------quality changes in tributaries and some mainstream sites. Epidermal structuralchanges may occur in exposed fish. Such changes may act in a manner similar to experimentalabrasion and allow invasion by Aphanomyces sp. propagules, leading to developmentof typical EUS lesions.The hypothesis that runoff or drainage from acid sulphate soil areas has a causalrelationship to EUS is supported by the findings of a survey in which EUS prevalencein two relatively sedentary estuarine fish species, sand whiting (Silfugo ciliata) andyellowfin bream (Acanthopagrus australis), was measured at 3-monthly intervals, on7 occasions, at specific mainstream sites on the Richmond River during 1988/89. Findingsof the survey are summarised in Table 1.There are several acid sulphate soil sites in the lower Richmond River floodplain;the total distribution of such areas remains to be determined. EUS prevalence in yellowfinbream was highest in the section of river between Sites 2 and 6, where thecumulative effects of run-off from known acid sulphate soil areas should be at theirgreatest (Figure 2). Prevalence in this river section was also high in sand whiting, whichhave a more restricted distribution in the estuary. Given that the species examinedare relatively sedentary, it is likely that the EUS lesions were induced at these sites.At Site 1, buffering and dilution with sea water during tidal exchanges would occur,and it is noteworthy that EUS prevalence at this site was low.A similar association between EUS outbreaks and acid sulphate soils has been notedat a coastal study site in the Philippines (Reantaso, Paclibare, Callinan and Singh,unpublished). Acid soils, including acid sulphate soils, are widespread in Southeastand South Asia and may play a similar role in EUS induction in those regions. Studiesin Southeast Asia have associated EUS outbreaks with water having low hardness(the characteristic of water which represents the total concentrations of calcium andmagnesium expressed as calcium carbonate equivalent), low alkalinity (the buffering408

capacity of water expressed as calcium carbonate equivalent) and fluctuating pH(Anon 1989, Anon 1990a, Phillips 1992). Fish exposed to these conditions are highlysusceptible to injuries caused by low pH and toxic metal ions (Anon 1990b).ConclusionsWhile there is a clear causal association between fish kills and ‘first-flush’ run-offwater from acid sulphate soil areas in some Australian estuaries, a similar causal associationfor EUS remains to be established. There is, however, experimental evidencethat water quality attributes such as low pH, high concentrations of inorganic aluminumand,low concentrations of dissolved oxygen which are present in this ‘first-flush’water, may injure skin of sub-lethally exposed fish; the putative infectious cause ofEUS, an Aphanomyces fungus, may then be able to invade these damaged areas andproduce the characteristic ulcers.In view of the potential of seasonally recurrent EUS outbreaks, as well as fish kills,to cause long-term damage to the sustainability of estuarine fisheries in the Asia-Pacificregion, it is essential that major causal factors are identified and appropriate controlmeasures, such as ameliorative drainage management practices, are put in place. However,given the complex interactions between rain events, acid sulphate soil areas, riverflow patterns, populations of susceptible fish and distribution of the pathogenic Aphanomycessp., considerable research effort will be required to elucidate thoroughly thepossible relationships.AcknowledgementsWe thank R. West and G. McLennan for kind permission to include EUS prevalencedata and water quality data respectively. We also thank C. Peak for generously assistingin the preparation of figures and A. Parrington for typing the manuscript. Thesestudies were funded, in part, by Land and Water Resources Research and DevelopmentCorporation.ReferencesAnon 1989. A report on the NACA workshop on the regional research program on ulcerative syndromein fish and the environment. Network of Aquaculture Centres in Asia-Pacific, BangkokAnon 1990a. Regional research program on relationships between epizootic ulcerative syndrome in fishand the environment. Network of Aquaculture Centres in Asia-Pacific, BangkokAnon 1990b. Water quality management for aquaculture and fisheries. Institute of Aquaculture, Universityof Stirling, ScotlandAnon 1991. Fish health management in Asia-Pacific. Report on a regional study and workshop on fishdisease and fish health management. Asian Development Bank Agriculture Department Report SeriesNo. I, Network of Aquaculture Centres in Asia-Pacific, BangkokBirchall, J.D., C. Exley, J.S. Chappell and M.J. Phillips 1989. Acute toxicity ofaluminum to fish eliminatedin silicon-rich acid waters. Nature 338, 146-148Brown, D.J. 1983. Effect of calcium and aluminum concentrations on the survival of brown trout (Salmotrutta) at low pH. Bulletin of Environmental Contamination and Toxicology 30, 582-587409

Brown, T.E., A.W. Morley, N.T. Sanderson and R.D. Tait 1983. Report of a large fish kill resulting fromnatural acid water conditions in Australia. Journal of Fish Biology 22,335-350Callinan, R.B., G.C. Fraser and J.L. Virgona 1989. Pathology of red spot disease in sea mullet, Mugilcephalus L. from eastern Australia. Journal of Fish Diseases 12,467-479Daye, P.G. and E.T. Garside 1976. Histopathologic changes in surficial tissues of brook trout, Salvelinusfontinalis(Mitchill), exposed to acute and chronic level of pH. Canadian Journal of Zoology 54,2140-2155Driscoll, C.T., J.P. Baker, J.J. Bisogni and C.L. Schofield 1980. Effect of aluminum speciation on fishin dilute acidified waters. Nature 284, 161-164Fraser, G.C., R.B. Callinan and L.M. Calder 1992. Aphanomyces species associated with red spot disease,an ulcerative skin disease of estuarine fish from eastern Australia. Journal of Fish Diseases. In press.Hart, B.T., E.M. Ottaway and B.N. Noller 1987. Magela Creek System, Northern Australia. I. 1982-83Wet-season quality. Australian Journal of Marine and Freshwater Research 38,261-288Ingersoll, C.G., D.R. Mount, D.D. Gulley, T.W. LaPoint and H.L. Bergman 1990a. Effects of pH, aluminiumand calcium on survival and growth of brook trout embryos (Salvelinusfontinalis). Canadian Journalof Fisheries and Aquatic Sciences 47,1580-1 592Ingersoll, C.G., D.A. Sanchez, J.S. Meyer, D.D. Gulley and J.E. Tietge 1990b. Epidermal response ofpH, aluminium, and calcium exposure in brook trout (Salvelinus fontinalis) fry. Canadian Journal ofFisheries and Aquatic Sciences 47, 1616-1622Langdon, J.S. 1988. Investigation of fish kills: I. History and causes. In: Fish Diseases Proceedings 106,168-194. Post Graduate Committee in Veterinary Science, University of SydneyLinnenbach, M., R. Marthaler and H. Gebhardt 1987. Effects of acid water on gills and epidermis in browntrout (Salmo trutta L.) and in tadpoles of the common frog (Rana temporaria L.). Anales de la SociétéRoyale de Belgique 117,365-374McKenzie, R.A. and W.T. Hall 1976. Dermal ulceration of mullet (Mugil cephulus). Australian VeterinaryJournal 52,230-231Merriner, J.V. and D.S. Vaughan 1987. Ecosystem and fishery implications of ulcerative mycosis. In: Proceedingsof the Workshop on Fishery Diseases for the Albemarle-Pamlico Estuarine Study, 39-46. Universityof North Carolina Water Resources Research Institute, RaleighMount, D.R., M.J. Swanson, J.F. Breck, A.M. Farag and H.L. Bergman 1990. Responses of brook trout(Salvelinusfontinalis) fry to fluctuating acid, aluminium and low calcium exposure. Canadian Journalof Fisheries and Aquatic Sciences 47, 1623-1630Pearce, M. 1990. Epizootic ulcerative syndrome technical report, December 1987 -September 1987. NorthernTerritory Department of Primary Industry and Fisheries No. 22, DarwinPhillips, M.P. 1992. Techical review of epizootic ulcerative syndrome. Network of Aquaculture Centresin Asia-Pacific, Bangkok. In press.Plumb, J.A., J.M. Grizzle and J. Defigueiredo 1976. Necrosis and bacterial infection in channel catfish(fctaluruspunctatus) following hypoxia. Journal of Wildlife Diseases 12,247-253Roberts, R.J., R. Wootten, I. MacRae, S. Millar and W. Struthers 1980. Ulcerative disease survey, Bangladesh.Final report to the Government of Bangladesh and the Overseas Development Administration.Institute of Aquaculture, StirlingRodgers, L.J. and J.B. Burke 1981. Seasonal variation in the prevalence of 'red spot' disease in estuarinefish with particular reference to the sea mullet, Mugil cephalus L. Journal of Fish Diseases 4,297-307Staurnes, M., T. Sigholt and O.B. Reite 1984. Reduced carbonic anhydrase and Na-K-ATPase activityin gills of salmonids exposed to aluminium-containing acid water. Experientia 40,226-227Tandjung, S.D., D.V. Rottiers and R.L. Herman 1982. Histopathological studies on the effects of acidstress to brook trout Salvelinus fontinalis (Mitchill) in the presence of sublethal concentrations of aluminium.In: Johnson R.E. (Ed.). Acid rain/fisheries. Proceedings of an international symposium on acidicrain and fishery impacts on Northeastern North America, 357. American Fisheries Soc., Bethesd?Wendelaar Bonga, S.E. and L.W. van Dederen 1986. Effects of acidified water on fish. Endeavour. NewSeries IO, 198-202Witters, H.E., S. van Puymbroek, J.H. Vangenechten and O.L. Vanderborght 1990. The effect of humicsubstances on the toxicity of aluminium to adult rainbow trout, Onchorhyncusmykiss (Walbaum). Journalof Fish Biology 37,43-53410