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25th International Meeting on Organic Geochemistry IMOG 2011

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P-397<br />

Impact of different operating modes <strong>on</strong> the indigenous microbial<br />

ecosystems in energy storage systems in the North German<br />

Basin: Compositi<strong>on</strong>al changes and membrane phospholipid<br />

adaptati<strong>on</strong><br />

Alexandra Vetter 1 , Kai Mangelsdorf 1 , Stephanie Lerm 1 , Mashal Alawi 1 , Andrea Seibt 2 ,<br />

Markus Wolfgramm 3 , Hilke Würdemann 1 , Andrea Vieth-Hillebrand 1<br />

1 GFZ German Research Centre for Geosciences, Potsdam, Germany, 2 BWG Geochemische Beratung GbR,<br />

Neubrandenburg, Germany, 3 Geothermie Neubrandenburg GmbH (GTN), Neubrandenburg, Germany<br />

(corresp<strong>on</strong>ding author:vetter@gfz-potsdam.de)<br />

The compositi<strong>on</strong> of microbial communities was<br />

examined in three geothermal energy storages in the<br />

North German Basin. These aquifer thermal energy<br />

storages (ATES) differ in depth (20 to 1250 m), in fluid<br />

chemistry (freshwater, brine), and functi<strong>on</strong>ality<br />

(heat/cold storage). To investigate the microbial<br />

ecosystems the bacterial membrane phospholipid<br />

fatty acid (PLFA) compositi<strong>on</strong> and the fluid chemistry,<br />

especially, of potential nutrient for the indigenous<br />

microorganisms such as sulfate, nitrate, low<br />

molecular weight organic acids and DOC as well as<br />

its carb<strong>on</strong> isotopic compositi<strong>on</strong> was evaluated.<br />

A solar assisted heat storage located in a quaternary<br />

freshwater aquifer in 15 to 30 m depth was m<strong>on</strong>itored<br />

c<strong>on</strong>cerning its microbial compositi<strong>on</strong> with respect to<br />

the seas<strong>on</strong>al changes of charge and discharge of<br />

heat. The plant stores the surplus heat with<br />

temperatures of 50°C from the solar energy<br />

producti<strong>on</strong> during summertime (charge mode).<br />

Therefore, water is pumped from the cold side with<br />

temperatures of 8 to 20°C, loaded with heat in a heat<br />

exchanger and re-injected into the warm well.<br />

Discharge of heat is carried out in wintertime, when<br />

heat demand increases for space heating and<br />

domestic hot water preparati<strong>on</strong> in multi-family houses.<br />

In wintertime, the PLFA compositi<strong>on</strong> of the indigenous<br />

microbial community, mainly 16:1, 16:0, 18:1, 18:0,<br />

and branched fatty acids (FA) with 15 and 17 carb<strong>on</strong><br />

atoms, showed an adaptati<strong>on</strong> of the cell membrane<br />

during the discharge mode, when temperature<br />

decreases from 50 to 13.7°C during time of heat<br />

extracti<strong>on</strong>. This is reflected by a shift of 13.4 %<br />

towards more unsaturated fatty acids (FA) and of 10.8<br />

% towards more FAs with shorter chain length.<br />

Moreover, the anteiso/iso ratio was higher at cooler<br />

temperatures indicating a membrane temperature<br />

adaptati<strong>on</strong> of these microorganisms.<br />

World‘s deepest heat storage in the North German<br />

Basin (1250 m depth) stores surplus heat from a gas<br />

and steam cogenerati<strong>on</strong> plant in summertime, which<br />

is used in wintertime for district heating. The fluid is<br />

NaCl dominated with high sulfate c<strong>on</strong>centrati<strong>on</strong> (ca. 1<br />

g/L) and the DOC can account for 18 mg C/L.<br />

Temperature ranges <strong>on</strong> the warm side from 90 to<br />

65°C and <strong>on</strong> the cold side from 50 to 45°C. PLFA<br />

profiles are dominated by iso- and anteiso-15:0 <strong>on</strong> the<br />

cold side, while <strong>on</strong> the warm side 16:0 is the major<br />

compound. Moreover, the PLFA patterns indicate<br />

different compositi<strong>on</strong>s of the microbial communities<br />

<strong>on</strong> the warm and cold side.<br />

In c<strong>on</strong>trast to shallow and deep heat storages,<br />

another system, located in 30 to 60 m depth, in the<br />

North German Basin is used as a cold storage for air<br />

c<strong>on</strong>diti<strong>on</strong>ing of buildings in summertime (discharge<br />

mode). In wintertime (charge mode) the freshwater<br />

from the warm side is pumped up, cooled down by an<br />

air cooler and subsequently re-injected into the cold<br />

side. Temperature ranges <strong>on</strong> the warm side from 14<br />

to 30°C and <strong>on</strong> the cold side from 6 to 10°C. Within a<br />

four years m<strong>on</strong>itoring, two clogging events occur<br />

during the discharge phase and the injecti<strong>on</strong> rates <strong>on</strong><br />

the warm side was reduced. PLFA pattern clearly<br />

reveals changes in the microbial community<br />

compositi<strong>on</strong> during the clogging events. During these<br />

events the 16:1�7 fatty acid and 18:1�7 significantly<br />

increase compared to the normal operating mode.<br />

These fatty acids are known to be main c<strong>on</strong>stituents<br />

of the ir<strong>on</strong> oxidizing bacterium Galli<strong>on</strong>ella [1] and the<br />

sulphur oxidizing bacterium Thiothrix [2]. Both<br />

bacteria are known to be involved in clogging events.<br />

Microbiological analysis c<strong>on</strong>firmed the occurrence of<br />

these species during the disturbance time in the<br />

storage system and inorganic investigati<strong>on</strong>s reveal<br />

ir<strong>on</strong> scales in the plant.<br />

The study shows clearly that microorganisms are<br />

capable to adapt to specific c<strong>on</strong>diti<strong>on</strong>s within short<br />

times and can influence the working reliability of<br />

geothermal energy storages.<br />

[1] Sahl et al. (2008) Appl. Envir<strong>on</strong>. Microbiol., 74(1),<br />

143-152.<br />

[2] Zhang et al. (2005) Appl. Envir<strong>on</strong>. Microbiol.,<br />

71(4), 2106-2112.<br />

526

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