The largest database of trusted experimental protocols

Nah14co3

Manufactured by PerkinElmer

NaH14CO3 is a radioactive chemical compound used as a tracer in various scientific applications. It is a sodium salt of carbonic acid, with the carbon-14 isotope incorporated into the molecule. NaH14CO3 is commonly used in biochemical and metabolic studies to track the movement and incorporation of carbon compounds within living organisms or experimental systems.

Automatically generated - may contain errors

5 protocols using nah14co3

1

Protein Purification and Kinetic Assay

Check if the same lab product or an alternative is used in the 5 most similar protocols
Protein purification, assessment of purity, quantitation and assays for determining kinetic constants were done as described elsewhere [31 (link), 33 (link)]. Tritium-labeled RuBP, which was used for measuring CO2/O2 specificity factors, had been synthesized in the laboratory previously [31 (link)]. PRK activities were measured in cell extracts by the addition of NaH14CO3 (Perkin-Elmer), ribulose-5-phosphate (Sigma) and ATP (Sigma) as substrates, and coupling the reaction with excess RubisCO. All kinetic constants measured with either the histidine-tagged megaplasmid RubisCO (Table 2) or the untagged chromosomal version of the wild type and A380V single-mutant proteins (Table 3) were similar.
+ Open protocol
+ Expand
2

Measuring Photosynthetic Carbon Fixation

Check if the same lab product or an alternative is used in the 5 most similar protocols
The photosynthetic carbon fixation rates were estimated using the 14C incorporation method [30 ]. Water samples were analyzed in triplicates with dark and zero-time controls. Samples (50 mL) collected at 09:00 AM were added to polycarbonate bottles (Nalgene) containing 5 μCi of NaH14CO3 (Perkin Elmer) and incubated for 4–5 h under ambient natural illumination and temperature. To determine the quantity of the added radioactivity, 50 μL of each sample were immediately mixed with 50 μL of ethanolamine and stored for analysis. The incubations were terminated by filtering the spiked seawater onto GF/F filters in order to separate the total primary production or onto a 3-μm glass fiber filter in order to determine the contribution of nano-microphytoplankton to primary production at <50 mmHg. The filters were incubated overnight in 5 mL scintillation vials containing 50 μl of 32% HCl in order to remove excess 14C-bicarbonate. After adding 5 mL of scintillation cocktail (Ultima-Gold) to each vial, the radioactivity was measured using a TRI-CARB 2100 TR (Packard) liquid scintillation counter.
+ Open protocol
+ Expand
3

Measuring C Uptake and N2 Fixation in Chemostat Cultures

Check if the same lab product or an alternative is used in the 5 most similar protocols
Rates of short-term C uptake were determined at the end of the chemostat culturing. 100 µM NaH14CO3 (PerkinElmer) was added to 50 mL of cultures in the middle of the photoperiod, which was then incubated for 20 min under the growth conditions. After incubation, the samples were collected onto 3 μm polycarbonate membrane filters (Millipore), which were then washed with 0.22 µm-filtered oligotrophic seawater and placed on the bottom of scintillation vials. The filters were acidified to remove inorganic C by adding 500 µL of 2% HCl. The radioactivity was determined using a Tri-Carb 2800TR Liquid Scintillation Analyzer (PerkinElmer). Rates of N2 fixation (nitrogenase activity) were measured in the middle of the photoperiod for 2 h by the acetylene reduction assay49 , using a ratio of 4:1 to convert ethylene production to N2 fixation.
+ Open protocol
+ Expand
4

Quantifying Carbon Flux in Plant-AMF Network

Check if the same lab product or an alternative is used in the 5 most similar protocols
Two weeks after 33P and 15N tracer additions, plants were prepared for 14CO2 labelling, to allow movement of carbon from plant to fungus to be quantified. A 110 µl solution of NaH14CO3 (Perkin Elmer) containing 1.0175 MBq 14C (specific activity = 1.621 GBq/mmol) was added to a cuvette in each pot. The tops of all mesh‐windowed cores were sealed using gas‐tight rubber septa (SubaSeal) to minimize diffusion of 14CO2 into the cores. 14CO2 gas was liberated from the NaH14CO3 by addition of 10% lactic acid, generating a 1.0175 MBq pulse of 14CO2. Samples of 1 ml above‐ground gas and 1 ml below‐ground gas (via the glass wool‐filled core) were taken 1 hr after release of 14CO2 and every 4 hr thereafter to monitor the drawdown, respiration and flux of 14C through the plant–AMF network. Gas samples were injected into gas‐evacuated scintillation vials containing 10 ml Carbosorb® (Perkin Elmer), a carbon‐trapping compound. To this, 10 ml Permafluor scintillation cocktail (Perkin Elmer) was added, and 14C content of each sample was quantified by liquid scintillation counting (Tricarb 3100TR scintillation counter; Perkin Elmer).
Pots were maintained under cabinet conditions until detection of maximum below‐ground 14C flux (20–22 hr after 14CO2 liberation) at which point 3 ml 2 M KOH was added to cuvettes within each microcosm to capture remaining gaseous 14CO2.
+ Open protocol
+ Expand
5

Photosynthetic Carbon Fixation Rates

Check if the same lab product or an alternative is used in the 5 most similar protocols
Photosynthetic carbon fixation rates were estimated using 14C incorporation44 (link). Water samples were analyzed in triplicates with dark and zero-time controls. Samples (50 mL) collected at each time point were added to polycarbonate bottles (Nalgene) containing 5 μCi of NaH14CO3 (Perkin Elmer, specific activity 56 mCi mmol−1) and incubated for 4 h under ambient natural illumination and temperature. To determine the quantity of the added radioactivity, 50 μl of each sample was immediately mixed with 50 μl of ethanolamine and stored for analysis. The incubations were terminated by filtering the spiked seawater through GF/F filters (~0.7 μm nominal pore size) at low pressure (~50 mmHg). The filters were incubated overnight in 5-mL scintillation vials containing 50 μl of 32% HCl in order to remove excess 14C-bicarbonate. After adding 5 mL of scintillation cocktail (Ultima-Gold) to each vial, the radioactivity was measured using a TRI-CARB 2100 TR (Packard) liquid scintillation counter.
+ Open protocol
+ Expand

About PubCompare

Our mission is to provide scientists with the largest repository of trustworthy protocols and intelligent analytical tools, thereby offering them extensive information to design robust protocols aimed at minimizing the risk of failures.

We believe that the most crucial aspect is to grant scientists access to a wide range of reliable sources and new useful tools that surpass human capabilities.

However, we trust in allowing scientists to determine how to construct their own protocols based on this information, as they are the experts in their field.

Ready to get started?

Sign up for free.
Registration takes 20 seconds.
Available from any computer
No download required

Sign up now

Revolutionizing how scientists
search and build protocols!