Transports of Organic Carbon and Nutrients in the Kaoping River-Sea System J.-J. Hung, H.-M. Yang, E.-T. Yeh, Y.-C. Yeh, C.-M. Ho and I..-J. Lai Institute.

Slides:



Advertisements
Similar presentations
Chesapeake Bay Environmental Model Package A coupled system of watershed, hydrodynamic and eutrophication models The same package used for the 2002 load.
Advertisements

Geographical Information System & Modelling LIFE02/ENV/P/
Paleolimnology as a Tool for Interpreting Ecosystem Changes within Freshwater Lakes Heather Burgess1, Andrea Lini1, Milt Ostrofsky2, Suzanne Levine3, Neil.
Biogeochemical Tracers in Arctic Rivers: Linking the Pan-Arctic Watershed to the Arctic Ocean (The PARTNERS Project)
Lecture Goals To discuss why nitrogen and phosphorus are important nutrients in freshwater systems. To trace how nitrogen and phosphorus move through freshwater.
Transport of nitrogen and phosphorus from Rhode River watersheds during storm events David Correll, Thomas Jordan, and Donald Weller Water Resources Research,
Estuarine Chemistry/Physical: Estuaries are where rivers meet the sea - the exact nature of the chemical processes occurring in an estuary generally depends.
THE STUDY OF BIOGEOCHEMICAL CYCLES AND RELATED SEDIMENT FLUXES: THE IOC-BSRC PROJECT PROPOSAL Could such a project idea be developed into an EC FP Integrated.
European Nitrogen Assessment: Supplementary Material: Powerpoint Graphics to Chapter 5. Source: Sutton, M.A., Howard, C.M., Erisman J.W., Bealey J.W.,
Chapter 12 Chapter 12 The Global Cycles of Nitrogen and Phosphorus Copyright © 2013 Elsevier Inc. All rights reserved.
Michael J. Brayton MD/DE/DC Water Science Center Hydrologic Controls on Nutrient and Pesticide Transport through a Small Agricultural Watershed, Morgan.
Suspended particle property variation in Gaoping Submarine Canyon Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry, National Sun Yat-sen.
Chemistry and Biogeochemical Cycling: Chemicals dissolved in water Abundant Less Abundant (not trace)
Preliminary Measurement of Submarine Groundwater Discharge in Taiwan Yi-Jie Lin*,Chen-Tung Arthur Chen, Meng-Chia Chen Institute of Marine Geology and.
FATES-COMARC 1 Riverine transport of polycyclic aromatic hydrocarbons from Kaoping River (Taiwan) to coastal ocean Chon-Lin Lee 1 *, Bing-Sian Lin 1, and.
Marine Chemistry and Biological Oceanography 海洋化學與生物海洋.
Sybil P. Seitzinger International Geosphere-Biosphere Program (IGBP) Stockholm, Sweden Modeling global river export: N, P, C, Si E. Mayorga A.F. Bouwman.
The Interplay between a Mountainous River and Nearby Submarine Canyon in Southern Taiwans Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry,
Weathering Sources in the Kaoping River Catchment, Southwestern Taiwan: Insights From Major and Trace Elements, Sr Isotopes and Rare Earth Elements C.-F.
Particulate scavenging and lateral transport processes in the Kaoping River-Sea System based on 210 Po and 210 Pb distributions and disequilibrium Hung.
Principles of Mass Balance
Suspended particle property variations in Gaoping Submarine Canyon Ray T. Hsu and James T. Liu Institute of Marine Geology and Chemistry, National Sun.
Effects of global warming on the world’s oceans Ashley A. Emerson.
Carbon metabolism in marine ecosystems C.M. Duarte and S. Agusti (1998) J.-P. Gattuso, M. Frankignoulle and S.V. Smith (1999) J.-P.Gattuso, M. Frankignoulle.
LOICZ Biogeochemical Budgeting Procedures and Examples V Dupra and SV Smith Department of Oceanography University of Hawaii Honolulu, Hawaii 96822
NSF - CREST Center for the Integrated Study of Coastal Ecosystem Processes and Dynamics in the Mid-Atlantic Region Sub – Theme #1 Land Use and Climate.
Ecosystem Energetics Limits on primary production Relationship between primary and secondary productivity Trophic efficiency Nutrient Cycles.
Reconsidérer les flux continent-océan Catherine Jeandel& Eric Oelkers (2014) CNRS, LEGOS, Observatoire Midi-Pyrénées, Toulouse University CNRS, GET, Observatoire.
Nutrient Cycling Biogeochemical Cycles Energy vs. Matter  Energy flows throughout an ecosystem in ONE direction from the sun to autotrophs to heterotrophs.
Land Ocean Coupling Coupling riverine fluxes of nutrients to a Global Biogeochemical Ocean General Circulation Model Christophe Bernard,
Export and metabolism of carbon in urban watersheds: Climate implications Rose M. Smith 1, Sujay S. Kaushal 1 1 University of Maryland College Park Motivation.
Ecological Impact of Nutrients from Shrimp Farms Mark O’Donohue, Adrian Jones, Simon Costanzo, Michele Burford, Pat Glibert, Judy O’Neil, Cindy Heil &
The Non-tidal Water Quality Monitoring Network: past, present and future opportunities Katie Foreman Water Quality Analyst, UMCES-CBPO MASC Non-tidal Water.
Inputs to shelf seas- an overview Materials are introduced into coastal and shelf seas primarily through: rivers, atmosphere, groundwaters, ice processes.
Nitrogen inorganic nitrogen: NH 4 (ammonia) NO 2 (nitrite) NO 3 (nitrate)
Fig. 5 showed the ratio of DON:DOP in the TS. Different slopes and their corresponding locations were marked with the same color. The average ratio of.
 Prior to the 1930’s, the natural microbial processes of nitrification and denitrification were at equilibrium in the environment and nitrogen availability.
Biophysical and Socioeconomic Assessments: The LOICZ* Approach Liana Talaue-McManus Rosenstiel School of Marine and Atmospheric Science University of Miami.
Fig. 4. A framework configured to calculate a P budget. Shelf ( 1000 m )
LTER Science Council 2015 Instructions Address question: “How is LTER advancing our understanding of the dynamics and controls of inorganic nutrients?”
BIOSOPE CRUISE Laboratoire d’Océanographie et de Biogéochimie Campus de Luminy Marseille cedex 09 Patrick RAIMBAULT Nicole GARCIA Gerd SLAWYK Main.
Working Group 3: What aspects of coastal ecosystems are significant globally? Coastal Zone Impacts on Global Biogeochemistry NCAR, June 2004 Contributed.
Nutrient Cycling 3.3. Energy vs. Matter  Energy flows throughout an ecosystem in ONE direction from the sun to autotrophs to heterotrophs  Matter is.
Impact of Watershed Characteristics on Surface Water Transport of Terrestrial Matter into Coastal Waters and the Resulting Optical Variability:An example.
1 Regional Data Review : What have we learned in eight years? Lester McKee Sources Pathways and Loadings Workgroup Monday December 8 th 2008 San Francisco.
Kaijun Su a, Jinzhou Du a, *, Mark Baskaran b and Jing Zhang a State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai.
*Minagawa M, Usui T, Miura Y, Nagao S, Irino T, Kudo I, and Suzuki K, Graduate School of Environmental Science, Hokkaido University, Sapporo ,
Food Systems in the Coastal Zone: A LOICZ Perspective L. Talaue-McManus Rosenstiel School of Marine & Atmospheric Science University of Miami.
Implications of C/N Ratios from Two USGS Sediment Trap Samples Recovered from the Kaoping Canyon Saulwood Lin, Institute of Oceanography Natioanal Taiwan.
Announcements in class 2/5/07 Movie Wed. Don’t miss it! Material will be on the exam. Only one showing. Problem Set 4 is posted online. Print it out yourself.
Abstract Man-made dams influence more than just the flow of water in a river. The build up of sediments and organic matter, increased residence times,
Introduction to Biogeochemical Cycles
Life depends on recycling chemical elements
Nitrogen Budgets for the Mississippi River Basin using the linked EPIC-CMAQ-NEWS Models Michelle McCrackin, Ellen Cooter, Robin Dennis, Jana Compton, John.
– NUTRIENTS 2 Chapter 3.4 in Chapman et al. Gretchen Gettel/Peter Kelderman UNESCO-IHE Institute for Water Education Online Module Water Quality.
Nitrogen loading from forested catchments Marie Korppoo VEMALA catchment meeting, 25/09/2012 Marie Korppoo, Markus Huttunen 12/02/2015 Open DATA: Nutrient.
The Global Oxygen Cycle
Atmospheric depositions Ocean University of China
Denitrification in Delaware Bay Tidal Marshes and Creeks
Elizabeth River PCB TMDL Study: Numerical Modeling Approach
222Rn, oxygen, nutrients (nitrate, ammonia, phosphate)
James River PCB TMDL Study: Numerical Modeling Approach
Jim McClelland Rae Mooney University of Texas at Austin
Ecosystems and the Physical Environment
How do small dam removals affect reach-scale nitrogen exports?
Ocean Water Chemistry.
Ocean Chemistry.
Baltic Sea Research Institute Warnemünde
Results and discussion
Presentation transcript:

Transports of Organic Carbon and Nutrients in the Kaoping River-Sea System J.-J. Hung, H.-M. Yang, E.-T. Yeh, Y.-C. Yeh, C.-M. Ho and I..-J. Lai Institute of Marine Geology and Chemistry, National Sun Yat- Sen University Kaohsiung, Taiwan

Outlines Riverine fluxes of suspended sediment, and dissolved and particulate carbon, nitrogen and phosphorus Meterological conditions vs. riverine fluxes Transformation of riverine CNP in the Kaoping Estuary (net fluxes) Coastal CNP budgets (on-going studies)

Dadson et al., 2003 Kaoping River

里嶺大橋 Sampling period: Aug/1999-July/2000 ( La Nina event) 2002 ( El Nino event) Historical

Sampling locations in the Kaoping River

Sampling locations and their elevations and discharge contributions

Sediment Yield (Kaoping watershed)  1999/2000: 3.6*10 3 g/m 2 /yr  2002: 0.656*10 3 g/m 2 /yr  World’s rivers (mean): 150 g/m 2 /yr  Island’s rivers (mean): 3*10 3 g/m 2 /yr # derived from suspended load only

Particle size vs. river discharge (water elevation) Pabuk Typhoon Wutip Typhoon Sepat Typhoon Krosa Typhoon Dry season Wet season

Particulate organic carbon (POC) Particulate inorganic nitrogen (PON)

Particulate organic phosphorus (POP) Particulate inorganic phosphorus (PIP)

Chemical Yield ( Ca, Mg, K, Na, Cl, SO 4, HCO 3, Si)  1999/2000: 1.14*10 3 g/m 2 /yr  2002: 0.416*10 3 g/m 2 /yr  World’s rivers (ave): 33~40 g/m 2 /yr

Transport of C and N in the Kaoping River

Kaoping River Industrial wastewater Others Domestic Animal wasterwater

Foot and Mouth Disease

Nitrogen Fluxes (Anthropogenic contributions) Estimated from wastewater discharge : 5.6*10 4 kg/day Estimated from difference between baseline and in-situ measurements: 6.5*10 4 kg/day (Particulate nitrogen: 4.8 *10 3 kg/day) EPA(ROC) report: 5.7 *10 4 kg/day Anthropogenic contributions to total fluxes: 89% (64715/72977=89%)

Phosphorus Fluxes (Anthropogenic contributions) Estimated from wastewater discharge: 4.7 *10 3 kg/day Estimated from the difference between baseline and in-situ measurements: 7.4 *10 3 kg/day(Particulate P: 4.4 *10 3 kg/day) EPA(ROC) report: 1.3 *10 4 kg/day Anthropogenic contributions to total fluxes: 61% (7399/12124=61%)

Carbon and nutrient yields from the Kaoping Watershed 08/ /2000 (a) 2002 (b) a/b Discharge (cms) POC (g/m 2 /yr) PIC (g/m 2 /yr) DOC (g/m 2 /yr) DIC (g/m 2 /yr) PN (g/m 2 /yr) DIN (mol/m 2 /yr) DIP (mmol/m 2 /yr) DSi (mol/m 2 /yr)

Meterological conditions primarily determine the material fluxes and proportions of natural and anthropogenic contributions

119°E122°E 26° N Taiwan Strait 24° N 22° N Kaoping River 121°E

Dec./2003 DO

July, 2003 Salinity

1.Dissolved inorganic nutrients (except for DIP-addition in high S range) and DOC were transported conservatively through the estuary during the wet season. 2.Nitrate reduction/denitrification occurred in the low S range during the dry season 3.Non-conservative transports - for particulate phases of carbon and nutrients 4.Using Biogeochemical (box) model to derive net fluxes

Dissolved CNP Budgets

Particulate CNP Budgets

Kaoping Watershed Kaoping Estuary ● Addition ● Removal River Dissolved Particulater matter Net fluxes Coastal Zone ● Primary production ● Recycling Sediments ● Recycled ● Preserved Settling Dissolved Release Denitrification Carbon, Nitrogen and Phosphorus Budgets On-going studies