Sampling and Analysis for Mercury of Steam Collected from Geothermal

Sampling and Analysis for Mercury of Steam Collected from Geothermal

Proceedings World Geothermal Congress 2005 Antalya, Turkey, 24-29 April 2005 Sampling and Analysis for Mercury in Steam Collected from Geothermal Wells and Fumaroles Edward Mroczek and Duncan Graham Institute of Geological and Nuclear Sciences, Wairakei Research Centre, PB 2000 Taupo, New Zealand [email protected] Keywords: sampling, analysis, mercury, steam, of mercury in the environment has resulted in numerous geothermal, wells, fumaroles. studies on the occurrence and behaviour of Hg in geothermal areas (Christenson and Mroczek, 2003; and ABSTRACT references therein). 0 Elemental mercury (Hg ) is the predominant form of Steam and gas discharged from geothermal power stations mercury found in chemical surveys of wells at New contain trace amounts of mercury and considerable effort is Zealand’s geothermal fields. Mercury is an environmental being expended internationally to develop technologies for pollutant and in New Zealand, resource consents limit the mercury removal in both geothermal and coal-fired power discharge to atmosphere. Unacceptable variation in plants (e.g.Vitolo and Pini, 1999; Vitolo and Seggiani, analyzed “total” mercury in steam within duplicate samples 2002; Peltier, 2003; Schofield, 2004). and between sampling rounds at various geothermal fields has led to a reassessment of the sampling methodologies. Previous studies by Robertson et al., (1977, 1978) and However the cause of the problems was poorly understood. backed up by experience in New Zealand (Christenson and It was thought the variability was due primarily to sampling 0 Mroczek, 2003) show that essentially all the mercury in artifacts caused by the high volatility of Hg or perhaps to geothermal steam and gases is Hg0 which is unreactive, an inadequate sample preservation and digestion prior to 0 even at high H2S levels. Hg also has a high vapour analysis. pressure and is consequently highly volatile. This means that in New Zealand geothermal power stations with direct In this study we evaluate the effect of sampling contact or binary condensers most of the mercury leaves via methodology (sampling vessels) and preservative the power station cooling towers and offgases. The (permanganate and dichromate) and digestion procedures exception is at Wairakei with its complex arrangement of used on the final result. It appears that sampling condensers and coolers (Timperley and Hill, 1997). methodology has the greatest effect on the variability Modeling showed that the estimate of mercury discharged observed. to the river in the condensate could be accounted for by assuming an equilibrium distribution of Hg0 between The direct collection of steam into evacuated glass vapour and liquid in all parts of the Wairakei power station ampoules containing acid dichromate preservative with no (Taylor et al., 2001). Hence Operators undertake regular subsequent hot digestion is the most convenient and monitoring of mercury in the incoming steam to estimate simplest procedure for obtaining good analytical agreement emissions to the atmosphere. between replicates. Samples collected using acid permanganate preservative, which is a stronger oxidizing Prior to the commencement of regular monitoring at one agent than acid dichromate, with or without hot digestion power station, duplicate test samples were collected on the prior to analysis, also gave comparable results. In this same day and also on the different days (Glover Pers. situation dichromate appears to be as equally effective as 0 Comm., 2000). Total steam mercury varied considerably permanganate for converting Hg to a fixed but reducible between the samples, the worst difference was when form. The exception is in the presence of native sulphur, duplicate samples gave 94 and 15 µg/l of condensed steam. This was of great concern given that power stations in New Ampoule sizes can be increased to accommodate high NCG Zealand have to observe mercury discharge limits as part of which would otherwise limit the sample size. Alternatively, their operational consent. where a sufficiently large sample cannot be conveniently collected into an evacuated ampoule, the steam/gas can be Based on this test, the results of Timperley and Hill (1997) passed (natural over-pressure or a pump on the outlet) and unpublished work of Timperley at the Wairakei Power through a two flask train containing dichromate Station, Glover (Pers. Comm., 2000) conjectured that: preservative. This can also give comparable results to samples collected in ampoules but requires much greater • acid permanganate seems to be the more reliable care in sample collection. reagent to use as a preservative since acid dichromate may not oxidize all the Hg0 It is recommended that careful evaluation of sampling and analysis methodologies for mercury in steam, best suited to • bubbling through acid permanganate as a collection the steam composition under study, be undertaken prior to technique would be better than through acid the commencement of an ongoing routine sampling and dichromate as less Hg would be lost. analysis programme. This will save time, effort and may also considerably reduce expensive analytical costs. • collection into acid permanganate in a closed ampoule will ensure no Hg is lost during collection. 1. INTRODUCTION The ubiquitous presence of Hg in hydrothermal • hot digestion prior to analysis is necessary environments and the concern due to the bioaccumulation 1 Mroczek and Graham The sampling procedure was subsequently modified which hour but is often left soaking overnight. Protective clothing successfully improved the repeatability and reproducibility and eye protection must be worn when using chromic acid. of the total mercury in steam analyses. However it is not Vigor-Brown and Timperley (1981) also noted that mercury clear whether the adopted procedure, discussed below, is is condensed to metallic mercury when steam is condensed the simplest yet most reliable method of collecting and in tubing to the sampling flask. This leads to particulate analyzing Hg in geothermal steam or whether it is mercury entering the sampling flask which is likely to limit preferable to use a closed ampoule or a bubble through reproducibility. To minimize this possibility, an insulated method of sample collection. Teflon hose (with a stainless steel over-braid) is used to transport the hot steam (after the T piece) to the sampling In this study we evaluate the effect of sampling flask without condensation. The hose is cleaned by filling methodology (ampoules or flasks), the use of preservative with 10% v/v of nitric acid as are other fittings unable to be (permanganate and dichromate) and digestion procedures cleaned in chromic acid. Butyl rubber hoses, normally used on the final result. to sample steam, are a source of mercury contamination and are difficult to clean. 2. REFERENCE METHOD FOR MERCURY Two types of sampling bottles were used in this study, a ~ Analytical methods applicable for analyzing mercury in 350 cc glass ampoule (Giggenbach, 1975) and two 150 ml steam are based on the reference methods APHA 3112B Erlenmeyer flasks in series with B24 ground glass joints (Clesceri et al., 1998) and EPA Method 245.1 (EPA 1982). each fitted with a Dreschel head with a stem length Both are very similar and comprehensively describe the sufficient to place the coarse sinter just off the bottom of instrumental analytical procedures for analysing total the flask. Teflon clips keep the heads firmly in place (as mercury by cold vapour atomic absorption. well as stoppers, air condensers etc) and the flasks are In the reference method, an aliquot of a water sample is connected with a short piece of silicone tubing. transferred to a BOD bottle or equivalent closed-system Steam enters the evacuated glass ampoule and is condensed container. The sample is digested with a dilute potassium by cooling the outer surface, usually by a stream of cool permanganate-potassium persulfate-nitric acid solution for water or dunking in a bucket of water. Non-condensable two hours at 95 oC. The digestion oxidizes all forms of gases limit the amount of condensed steam that can be mercury to Hg(II). The Hg(II) in the digested water sample collected in this manner, typically 10 – 20 ml depending on is reduced with stannous chloride to elemental mercury NCG, but the volume of the ampoule may be increased to which is sparged from the sample and detected by atomic compensate. For example, at a high gas field such as absorption to a reporting limit of 0.2 µg/l. The Ngawha (average 18 wt % CO in steam), a 2 l ampoule, measurement step is now usually performed using an 2 with Teflon stopcock at either end, is used to sample for automated mercury analyser, which avoids the analysis of mercury in steam. Ampoules of this size are expensive, the entire digested sample. difficult to handle, clean and transport in the field. 3. STANDARD OPERATING PROCEDURE FOR In contrast to the ampoule, the flask train is placed in a COLLECTION OF STEAM SAMPLES FOR shallow tray of ice water mixture and steam is collected at a MERCURY slow rate, typically 1-2 ml of condensate per minute to a After the initial problems were identified, the following total volume between 20 and 30 ml in the first flask. The procedure for collecting geothermal steam for mercury was weight change in the second flask is negligible. The adopted. A steam sample is collected (via a T piece venting overpressure is adjusted until gas appears to “effervesce” at to atmosphere to reduce pressure) and condensed into an the sinter in the first

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