Dataset: Field Sampling: Hydrologic data

Sampling summary:
Discrete samples were all obtained from ~0.2m using a diaphragm pump and weighted, marked hose. All containers were kept in dark coolers at ambient temperature during transport to the laboratory.  All filtration was done within a few hours of collection and when conditions permitted, on board the research vessel.

Water sampling was conducted bi-weekly. When the collection was split over two days, a single date was used based on the upstream or majority stations.

Methodology summaries corresponding to data columns in the dataset:

In-situ YSI sampling (YSI_* columns):

In situ measurements were performed at discrete depths on the sunlit side of the research vessel using a Yellow Springs Instruments (YSI Incoporated, Ohio) multiparameter sonde (Model 6600 or 6600 EDS-S Extended Deployment System) equipped with a YSI conductivity/temperature probe (Model 6560), a YSI chlorophyll probe (Model 6025), a YSI pH probe (Model 6561 or 6566), a YSI pulsed dissolved oxygen probe (Model 6562), a self cleaning YSI turbidity probe (Model 6026 or 6136), and beginning on the 07/30/2003 sampling date, a flat Li-Cor sensor (UWQ-PAR 6067).  The YSI sonde was coupled to a either a YSI 610 DM datalogger or a YSI 650 MDS Multi-parameter Display System datalogger. The data were stored on the datalogger and downloaded to Ecowin software upon return to the laboratory.

"PAR" column:

The diffuse light attenuation coefficient, Kd, was calculated from depth profiles of photosynthetically active radiation (PAR, 400-700 nm).  Prior to the 07/30/2003 sampling date, PAR measurements were performed with a spherical underwater quantum sensor (LI-COR LI-193SA) coupled to a LI-COR LI-1000 datalogger.  Beginning on the 07/30/2003 sampling date, a flat underwater quantum sensor (LI-COR LI-193SA) attached to a Yellow Springs Instruments YSI 6600 or YSI 6600 EDS-S sonde was used to measure PAR.  Measurements of PAR were performed on the sunlit side of the research vessel in 0.5 meter depth increments, beginning just below the water surface.  The diffuse attenuation coefficient is the slope of the linear regression between natural log transformed PAR data and depth. 

"POC" and "PN" columns:

Particulate organic carbon (POC) and Particulate Nitrogen (PN) concentrations were determined by elemental analysis of material collected on pre-combusted Whatman GF/F glass fiber filters.  Carbonates were removed from the filters by vapor phase acidification using concentrated hydrochloric acid (HCl).  After drying at 60 0C, the filters were rolled in tin disks and injected into a PE 2400 Series II CHNS/O Analyzer calibrated with acetanilide ending in June 2014.  Starting on the Neuse River sample date of June 2, 2014, a Costech Analytical Technologies, Inc. Elemental Combustion System CHNS-O ECS 4010 was used for elemental analysis by "flash combustion/chromatographic separation and multi-detector techniques".  The Costech Instrument utilizes EAS Clarity Software.  Atropine standards are used to develop a calibration curve (C 70.56%, N 4.84%, and carbon response ratio of 0.025 +/-0.003).  NIST Buffalo River Sediment Reference Material 8704 (C 3.351% +/-0.017, N 0.20% +/-0.04) and/or Acetanilide Bypass (C 71.09%, N 10.36%, carbon response ratio of 0.055 +/- 0.003) may used for calibration or a check standard.

"DOC" column:

Dissolved organic carbon (DOC) concentration was measured using a Shimadzu TOC-5000A Analyzer:  Water samples were vacuum filtered (less than 25 kilopascal) using pre-combusted Whatman glass microfibre filters (GF/F).  The filtrate was stored in pre-combusted glass scintillation vials with Teflon closures and frozen at -20 degrees Celsius until analysis.  The Shimadzu TOC-5000A Analyzer uses high temperature catalytic oxidation followed by non-dispersive infrared analysis of the CO2 produced.  Samples were acidified to a pH less than 2 and sparged with air before they were analyzed for non-volatile organic carbon.  

"DIC" column:

Dissolved inorganic carbon (DIC) was measured on samples held overnight in research pond by acidification followed by infrared analysis of carbon dioxide (CO2) on a Shimadzu Total Organic Carbon Analyzer (TOC-5000A) in IC mode and calibrated with sodium carbonate standards.  Previously run ModMon samples resulted in standard error analysis measurement (RSD) of DIC +/- 0.94%.  

"NO3_NO2" column:

Nitrate/nitrite (NO3- / NO2-) concentration was determined using a Lachat/Zellweger Analytics QuikChem 8000 flow injection autoanalyzer (Milwaukee, WI, USA) using method FIA 31-107-04-1-C:  Water samples were vacuum filtered (less than 25 kiloPascals) using pre-combusted Whatman glass microfibre filters (GF/F).  The filtrate was stored in high-density polyethylene bottles and frozen at -20 degrees Celsius until analysis.  Two replicates were run from the same bottle.  Method detection limits (MDL, µg L-1) were 0.71 on 1/25/2020.

"NH4" column:

Ammonium (NH4+) concentration was determined using a Lachat/Zellweger Analytics QuikChem 8000 flow injection autoanalyzer (Milwaukee, WI) using method FIA 31-107-06-1-A/B:  Water samples were vacuum filtered (less than 25 kiloPascals) using pre-combusted Whatman glass microfibre filters (GF/F).  The filtrate was stored in high-density polyethylene bottles and frozen (-20 degrees Celsius) until analysis.  Two replicates were run from the same bottle.   Method detection limits (MDL, µg L-1) were: 6.99 on 1/25/2020.

"TDN" column:

Total dissolved nitrogen (TDN) was measured by in-line digestion using the Lachat/Zellweger Analytics QuikChem 8000 flow injection autoanalyzer (Milwaukee, WI, USA) using method FIA 31-107-04-3-B for low total nitrogen for brackish/fresh waters (detection level: 0.1 - 5.0 milligrams nitrogen per liter):  Water samples were vacuum filtered (less than 25 kiloPascals) using pre-combusted Whatman glass microfibre filters (GF/F).  The filtrate was stored in high-density polyethylene bottles and frozen at -20 degrees Celsius until analysis.  Two replicates were run from the same bottle.  Total dissolved nitrogen by in-line digestion works by oxidizing all the nitrogen compounds to nitrate by heating to 100 degrees Celsius and adding energy via UV light.  The pH is dropped from 9.1 to 3 during the decomposition.  The entire digestion occurs prior to the injection valve.  The nitrate/nitrite concentration is then determined using standard colorimetric techniques similar to the strict nitrate/nitrite manifold. Method detection limits (MDL, µg L-1) were 11.75 on 1/25/2020. 

"DON" column:

Dissolved organic nitrogen (DON) was calculated by subtracting dissolved inorganic nitrogen (DIN) from total dissolved nitrogen (TDN).  If the DIN value used in the calculation was below the detection limit, it was taken to be zero for this calculation.  At one point DON was determined by high temperature oxidation using the Antek 7000N or Antek 7000V analyzer.

"PO4" column:

Orthophosphate (PO43-) was determined using a Lachat/Zellweger Analytics QuikChem 8000 flow injection autoanalyzer (Milwaukee, WI) using method FIA 31-115-01-1-F/G:  Water samples were vacuum filtered (less than 25 kiloPascals) using pre-combusted Whatman glass microfibre filters (GF/F).  The filtrate was stored in high-density polyethylene bottles and frozen at -20 degrees Celsius until analysis.  Two replicates were run from the same bottle.  Method detection limits (MDL, µg L-1) were 6.56 on 1/25/2020.

"SiO2" column:

Silicic acid (SiO2) was measured after vacuum filtration (< 25 kPA) of the collected water samples through pre-combusted (3-4 hours at 450 0C) Whatman GF/F glass fiber filters.  The filtrate was stored in high-density polyethylene bottles and frozen (-20 0C) until analysis.  Two replicates were run from the same sample bottle.  Nitrate plus nitrite concentrations were determined using a Lachat QuikChem 8000 flow injection autoanalyzer (Milwaukee, WI, USA).  Method detection limits (MDL, µM) were 1.17 on 1/25/2020.

"PPR" column:

Primary Productivity rate was measured using an adaptation of Steeman Nielsen's (1952) 14C bicarbonate method (Paerl et al. 1998).  This method of measuring primary productivity allows direct measurement of carbon uptake and measures only net photosynthesis:  Water samples were stored in 10 Liter high density polyethylene containers overnight in the research pond, a flow through system that receives water from the adjacent Bogue Sound, thereby simulating ambient water temperatures.  The following morning the water samples were removed from the pond and transported to the laboratory for analysis.  Water samples (76 milliliters) were added to three clear plastic square bottles to determine light uptake of carbon in triplicate and to 1 dark bottle to determine dark uptake of carbon.  A solution of radioactive carbonate (300 microliters) was added to each bottle.  The bottles were incubated for 4 hours in the pond.  The light bottles were incubated underneath a field light simulator, while the dark bottles were incubated in a covered perforated bucket that was submerged in the pond.  The FLS was used to simulate the ambient light conditions that phytoplankton are exposed to in the estuary (mixing conditions).  The FLS is comprised of a rotating wheel with varying levels of screening.  During the incubation period, photosynthetically active radiation (PAR) measurements were performed using a 2 pi Li-Cor LI-192SA spherical quantum sensor attached to a Li-Cor data logger.  After the incubation period, the samples were returned to the laboratory, shaken and the entire contents were gently vacuum filtered (less than 25 kilopascals) using 25 mm Whatman glass microfibre filters (GF/F).  The filters were placed in wooden drying trays and treated with concentrated hydrochloric acid fumes for 40 minutes to an hour to remove inorganic 14C.  The filters were folded in half and placed in 7 milliliter plastic scintillation vials.  Five milliliters of liquid scintillation cocktail (ecolume or cytoscint) was added to the vials.  The vials were capped, shaken, stored in the dark for 3-24 hours and then assayed for radioactivity using a Beckman liquid scintillation counter.  In addition to the samples, triplicate voucher samples were used to quantify the radioactivity of the 14C added.  Voucher samples consisted of 100 microliter of 14C and 100 microliters of phenylethylamine.  These vials also received 5 milliliters of liquid scintillation cocktail.  A background vial and two 14C background standards were used.   The quantity of carbon fixed is proportional to the fraction of radioactive carbon assimilated.  (Paerl, H.W., J.L. Pinckney, J.M. Fear, and B.L. Peierls 1998. Ecosystem responses to internal and watershed organic matter loading: consequences for hypoxia in the eutrophying Neuse River Estuary, North Carolina, USA. Marine Ecology Progress Series 166: 17-25; Steemann Nielsen, E. 1952. The use of radio-active carbon (C14) for measuring organic production in the sea. Journal du Conseil permanent international pour L'Exploration de la Mer 18: 117-140).

"Correct_Chla_IV" column:

Chl a concentration was measured using the modified in vitro fluorescence technique in EPA Method 445.0 (Welshmeyer 1994, Arar et al.  1997): Each water sample was vacuum filtered (less than 25 kilopascals) in duplicate at low ambient light conditions using 25 mm Whatman glass microfibre filters (GF/F).  The filters were blotted dry, wrapped in foil and frozen immediately at -20 degrees Celsius until analysis.  Chlorophyll a was extracted from the filter using a tissue grinder and 10 mL of 90 percent reagent grade aqueous acetone (v/v with deionized water, Fisher Scientific NF/FCC Grade). The samples remained in the acetone overnight at -20 degrees Celsius.  The extracts were filter-clarified using a centrifuge and analyzed on a Turner Designs Trilogy fluorometer.  The value reported is the average chlorophyll a concentration measured from the two filters. MDL 0.025 ug/l.  7200-046 Chl a extraction non acid module, 436 EX/685 EM (460 LED). The fluorometer was calibrated with a known concentration of pure Chl a that was determined using a Shimadzu UV-160U spectrophotometer and the extinction coefficients of Jeffrey and Humphrey (1975).  The calibration was checked daily against a solid secondary standard (Turner Designs, proprietary formula).   

Diagnostic phytoplankton photopigments were identified, separated and quantified by high performance liquid chromatography (HLPC) coupled to an in-line photodiode array spectrophotometer (Jeffrey et al.  1997). See "Related Datasets" section for the HLPC data and methods).