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30 protocols using toc vcph analyzer

1

Measuring Organic Carbon and Nitrogen

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Concentrations of total organic carbon and total nitrogen were measured by the high-temperature catalytic oxidation (HTCO) method using a commercially available automatic TOC-VCPH analyzer (Shimadzu, Japan). Samples were filtered through 0.45 μm filters and used for analysis. One blank deionized water and positive control of known TOC and TN concentration were analyzed along with the samples. The TOC-VCPH analyzer with a TNM-1 add-on is routinely used in conjunction with a Shimadzu ASI-V autosampler in non-purgable organic carbon (NPOC) mode, following the methodology recommended by Shimadzu. For flow cytometric analysis on Accuri C6 flow cytometer (BD Biosciences, San Jose, CA), 700 μL of water samples were stained with 7 μL of SYBR Green I (1:100 dilution in DMSO) (Invitrogen, Carlsbad, CA), and incubated in the dark for 10 min at 35°C before measurement. Where necessary, samples were diluted accordingly to achieve less than 4000 events/s at a pre-set flow rate of 35 μL/min.
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2

Comprehensive Water and Sediment Analysis

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Samples for measurements of various ions (F, Cl, SO42−, Na+, K+, Ca2+, Mg2+), dissolved organic carbon (DOC) and total nitrogen (TN) were gathered in 125 mL low-density polyethylene (LDPE) bottles after being filtered from the water through 0.45 μm PES syringe filters and stored at −20 °C until laboratory analysis [57 (link)]. Samples for dissolved inorganic carbon (DIC) measurements were gathered in 125 mL brown, gastight, glass bottles (precleaned using ultrapure water). To prevent biological degradation and photodegradation, DIC samples were poisoned with a 0.2% saturated HgCl2 solution and stored at 4 °C in the dark [51 (link)]. DIC, DOC, and TN were analyzed with a SHIMADZU TOC-VCPH analyzer (Shimadzu Corp, Kyoto, Japan). The pH and conductivity of sediment were determined using a soil parameter meter (STEPS COMBI5000, Nuremberg, Germany) with a sediment/water (1:5) suspension. The sediment moisture content was gravimetrically measured by drying the 5 g sediment samples with an oven to a constant weight at 105 °C. Approximately 50 g homogenized sediment was freeze-dried with a Labconco FreeZone 2.5 A freeze-dried system (Kansas City, MO, USA), and then sieved by 100 mesh sieves to analyze the total organic carbon (TOC). Finally, we analyzed the TOC of the sediment with the SHIMADZU TOC-VCPH analyzer (Shimadzu Corp., Kyoto, Japan).
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3

Dissolved Organic Carbon Measurement

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Duplicate samples for DOC measurements were unfrozen at room temperature, acidified with 18 μL of phosphoric acid (H3PO4; pH < 3), and analyzed in triplicate by high-temperature catalytic combustion on a Shimadzu TOC-VCPH analyzer with an ASI-V auto-sampler. All inorganic carbon and purgeable organic carbon was removed by a sparging process of acidified samples.
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4

Environmental Monitoring and Analysis

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Environmental variables such as pH, temperature, and dissolved oxygen were measured with a multiparameter sonde YSI 6600 V2 (YSI, Yellow Springs, OH, USA). Chlorophyll-a was extracted following the methods of Marker et al. (1980) and Nusch (1980) , and quantified in a spectrophotometer as described by Lorenzen (1967) (link).
Dissolved organic carbon and total nitrogen were quantified using a Shimadzu TOC-V cph analyzer, equipped with a Total Nitrogen analyzer module following the manufacturer protocol. Free phosphate and sulfate were analyzed by ion chromatography using a Dionex ICS – 1,100 system (Thermo Scientific). Water transparency was measured using a Secchi disc. All environmental variables are summarized in Supplementary information 1.
We performed a principal component analysis (PCA) with standardized environmental parameters to explore the spatial structure of environmental conditions in both rainfall periods.
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5

Biochar Mineral and Elemental Analysis

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The mineral elements (e.g., K, Mg) present in the biochar were determined by ICP (PlasmaQuant PQ9000, Germany). The N content in the biochar was determined by a TN analyzer (SHIMADZU, Japan). The total carbon (TC) content and total organic carbon (TOC) contents were determined by a TOC-V CPH analyzer (SHIMADZU, Japan).
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6

Comprehensive Elemental Analysis by ICP-MS

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The concentrations of Th, Zr, Be, As, Ca and K and other elements were analyzed using an inductively coupled plasma mass spectrometer (ICP-MS) (Elan DRC II, PerkinElmer SCIEX, USA). Th, Zr, Be and As were determined using a standard model, argon (Ar) as reaction gas with a method detection limits (MDL) of 0.009, 0.05, 0.02 and 0.006 ppb, respectively. Ca and K were determined using dynamic reaction cell (DRC) model, ammonia (NH3) as a reaction gas with MDLs of 2.2 and 0.4 ppb, respectively. The relative standard deviations (RSD) were estimated to be <10% for Th and Be, and <5% for Zr, As, Ca and K from five replicates for the concentrations determined >MDLs. Dissolved organic carbon (DOC) were determined using a TOC-VCPH analyzer (Shimadzu Corporation, Japan) with a RSD of <3% estimated from three to five replicates. DOC was analyzed as non-purgeable organic carbon (NPOC) by purging acidified samples with carbon-free air to remove DIC prior to measurement. Anions including NO3, SO42- and Cl were measured using an ion chromatograph (Dionex ICS‐2100, Thermo Scientific, USA) with a RSD < 5% for the reported values.
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7

Seawater Physicochemical Parameter Analysis

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The common physicochemical factors of seawater, including temperature and salinity, were measured in situ with an EXO1 Multiparameter Sonde (EXO1, YSI, USA). The pH value was measured using FiveEasy Plus™ (Mettler Teledo, Zurich, Switzerland). Chlorophyll a was measured using a Chlorophyll Fluorescence System (Phyto-PAM, Walz, Germany). Phosphate phosphorus (PO43−), nitrate nitrogen (NO3), nitrite nitrogen (NO2), and ammonium nitrogen (NH4+) were measured using a Discrete Chemistry Analyzer (CleverChem Anna, DeChem-Tech, Germany). TOC was measured using a Shimadzu TOC-VCPH analyzer (Japan).
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8

Sediment Nutrient Analysis Protocol

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Salinity and pH were measured in fresh sediments, whereas nutrients were measured in air-dried sediments. The interstitial water of the fresh sediment was collected by centrifugation, and the salinity and pH were measured using an automatic compensation salinity refractometer (ATAGO Co., Japan) and a pH meter (Mettler-Toledo Instruments Co., China). Sediments were air-dried for multiple days until their weight remained unchanged. Each sample was then thoroughly mixed after passing through a 2-mm sieve to remove roots and stones. Sediment ammonium, nitrite and nitrate were extracted from air-dried sediments (10 g) with 100 mL of 1 M KCl by shaking at 180 rpm for 60 min. The concentrations of NH4+, NO2 and NO3 were determined using a continuous segmented flow analyzer (SEAL AutoAnalyzer 3 HR, Maquon, WI, USA). A Shimadzu TOC VCPH analyzer (Shimadzu, Japan) was employed to analyze the TN, TC and TOC as reported previously (50 (link)).
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9

Characterization of g-C3N4/Bi12O17Cl2 Composite

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The X-ray diffraction (XRD) patterns of all as-made samples were measured by an X-ray diffractometer (Bruker D8 Advance). Fourier transform infrared spectra (FTIR) of all as-prepared samples were detected by Thermo Fisher Scientific IS10. The X-ray photoelectron spectroscopy (XPS) of g-C3N4/Bi12O17Cl2 (3 wt%) composite was recorded on Thermo Fisher Scientific Escalab 250. The microtopographies of g-C3N4, Bi12O17Cl2 and g-C3N4/Bi12O17Cl2 (3 wt%) composite were observed using JEM-2100F transmission electron microscope (TEM). The UV-vis diffuse reflectance spectra (DRS) of as-made samples were collected by an UV-vis spectrometer (Agilent Cary 5000). BET surface areas of all as-made samples were collected using a Micromeritics Tristar 3020 analyzer. Samples were outgassed at 150 °C for 12 h prior to measurements. Transient photocurrent properties of g-C3N4, Bi12O17Cl2 and g-C3N4/Bi12O17Cl2 (3 wt%) were measured by a CHI760 electrochemical system (China) in a three-electrode quartz cells. Pt wire was the counter electrode, and the saturated calomel electrode was the reference electrode. The sample films coated on ITO glasses were applied as the working electrode was. A 300 W Xe lamp with 400 nm filters provided the light source, and the electrolyte was 0.1 M Na2SO4. The total organic carbon (TOC) assays were investigated by using a Shimadzu TOC-VCPH analyzer.
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10

Quantification of TOC, DOC, and Nutrients

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TOC and DOC concentrations were measured by high temperature (680°C) catalytic oxidation (HTCO) using a Shimadzu TOC-VCPH analyzer (Shimadzu, Kyoto, Japan) (68 (link)). Samples were defrosted and acidified to pH 2 with phosphoric acid. Then, the samples were standardized using potassium hydrogen phthalate and all measurements were quality controlled using Consensus Reference Material (Hansell Organic Biogeochemistry Laboratory, University of Miami, FL, USA) (2 (link)). Concentrations of dissolved inorganic nutrients, including nitrite (NO2) and nitrate (NO3), were measured via spectrophotometric methods (69 ) using a Technicon AA3 auto analyzer (Bran+Luebbe GmbH, Hamburg, Germany). Indophenol blue (IPB) spectrophotometric methods were used to analyze the ammonium (NH4+) concentration in samples (70 (link)). However, it is notable that the concentrations of DOC were slightly higher than those of TOC after day 7 in treatments, indicating the possible introduction of extra DOC by sampling.
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