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Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems
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Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems

Published on: October 29, 2016

Tendencias del carbono orgánico disuelto resultantes de cambios en la química de la deposición atmosférica

Donald T Monteith1, John L Stoddard, Christopher D Evans

  • 1Environmental Change Research Centre, UCL, London, WC1E 6BT, UK. dmonteit@geog.ucl.ac.uk

Nature
|November 23, 2007
PubMed
Resumen

El carbono orgánico disuelto (COD) en los lagos y arroyos está aumentando debido a la disminución de la deposición ácida, no al cambio climático. Esto indica la recuperación del ecosistema de la acidificación e impacta los balances regionales de carbono.

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