Submarine groundwater discharge and nutrient addition to the coastal zone of the Godavari estuary

Show simple item record

dc.contributor.author Rengarajan, R.
dc.contributor.author Sarma, V.V.S.S.
dc.date.accessioned 2015-03-31T10:59:09Z
dc.date.accessioned 2017-09-30T03:12:37Z
dc.date.available 2015-03-31T10:59:09Z
dc.date.available 2017-09-30T03:12:37Z
dc.date.issued 2015
dc.identifier.citation Marine Chemistry, vol.172; 2015; 57-69
dc.identifier.issn 0304-4203
dc.identifier.uri http://drs.nio.org/drs/handle/2264/7677
dc.description.abstract Submarine groundwater discharge (SGD) represents a significant pathway of materials between land and sea, especially as it supplies nutrients, carbon and trace metals to coastal waters. To estimate SGD fluxes to the Godavari estuary, India, we used multiple tracers: salinity, Si, <sup>223</sup>Ra, <sup>224</sup>Ra, <sup>228</sup>Ra and <sup>226</sup>Ra. Tracer abundances were elevated in groundwater from the unconfined coastal aquifer and in surface water from the near shore zone; these enrichments decreased to low levels offshore, indicative of groundwater discharge. A model based on the decay of <sup>224</sup>Ra relative to <sup>228</sup>Ra was used to determine apparent water ages of various bays within the estuary. These ages ranged from 2.6 to 4.8 d during November 2011. Knowing the water age, the distribution of radium in the estuary, and the radium isotopic composition of groundwater enabled us to calculate SGD fluxes to the estuary. These fluxes (in units of 10<sup>6</sup> m<sup>3</sup> d<sup>-1</sup>) were on the order of 5 in the Gautami Godavari estuary, 20�43 in the Vasishta Godavari estuary, and about 300 in Kakinada bay, where enhanced ion exchange processes and redox-controlled cycling in the mangrove ecosystem may contribute to higher fluxes. These estimates of water fluxes allowed us to determine the magnitude and seasonal variability in the nutrient fluxes to the estuary associated with SGD. These nutrient fluxes (in units of mmol m<sup>-2</sup> d<sup>-1</sup>) ranged from 1�19 (N), 0.6�2.6 (P), and 5�40 (Si) in Gautami Godavari; 19�40 (N), 2.6�5.5 (P), and 200 (Si) in Vasishta Godavari; and 120�140 (N), 10 (P), and 220 (Si) in Kakinada bay. The high SGD fluxes to Kakinada bay contribute significant nutrients to this bay; considerably lower SGD fluxes to Vasishta Godavari still contribute significant nutrients to this estuary. Thus SGD represents a major source of new nutrients to these coastal ecosystems. For the entire Godavari estuarine system, SGD fluxes contribute (48�88) � 10<sup>9</sup> mol DIC y<sup>-1</sup> and (51�94) � 109 mol TA y<sup>1</sup>. These fluxes represent ~ 54 and ~ 62% of the riverine DIC and TA fluxes to the Godavari estuarine system. This study provides baseline data against which future changes in nutrient and carbon fluxes due to urbanization and economic growth over this region can be compared.
dc.language en
dc.publisher Elsevier
dc.relation.ispartof Mar Chem
dc.relation.isreferencedby NON-SCI
dc.subject Law, Policy and Social Sciences
dc.subject Aquatic Pollution
dc.subject.other Nutrient cycles
dc.subject.other Trace metals
dc.subject.other ISW, India, Andhra Pradesh, Godavari Delta, Godavari Estuary
dc.title Submarine groundwater discharge and nutrient addition to the coastal zone of the Godavari estuary
dc.type Journal Article
dc.affiliation.author Physical Research Laboratory, Ahmedabad, Gujarat, India


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record

Search DRS


Advanced Search

Browse

My Account