Fumaric Acid
Question 1: Write a short note on fumaric acid.
Answer:
Fumaric acid consists of carbon. It is an organic compound. The chemical formula of fumaric acid is C4H4O4 . It is a white-colored solid. Fumaric acid has a fruit-like taste and odor. It is also known as Allomaleic acid.
Question 2: Explain the structure of Fumaric acid.
Answer:
The chemical formula fumaric acid is C4H4O4 . It is a dicarboxylic acid. The IUPAC name of Fumaric acid is (E)-Butenedioic acid. Fumaric acid is the trans-isomer of butenedioic acid.
Question 3: If a chemist wants to prepare Fumaric acid how can he do that?
Answer:
Fumaric acid can be produced by the isomerization of maleic acid. In this reaction, mineral acid is used as a catalyst. Fumaric acid can be prepared by heating dilute hydrobromic acid.
Question 4: List some uses of Fumaric acid.
Answer:
- The esters of Fumaric acid are used for the treatment of psoriasis due to the antioxidants and anti-inflammation properties.
- Fumaric acid is used as a food additive.
- Fumaric acid is used by pharmacies to produce ferrous fumarate and alexipharmic.
- Fumaric acid is used in the production of Tartaric acid.
Question 5: Is Fumaric acid completely safe?
Answer:
No, Fumaric acid is not safe if it is taken in large quantities. When Fumaric acid comes in direct contact with the eyes it causes irritation. Inhaling of Fumaric acid can cause irritation in the nose and throat which leads to cough. Continues Exposure to Fumaric acid over a long period of time may damage the kidneys.
Fumaric Acid Formula
Carbon is a nonmetallic, tetravalent element that is of great use to humans. Its name is derived from Latin carbo which means charcoal or ember. Even though carbon is only 0.025% of the earth’s crust and 0.03% in the atmosphere it is of great importance to mankind. Carbon’s abundance in the earth’s core and the atmosphere is high. The ability of carbon to form polymer at normal temperature is the reason it is commonly found in all living forms. The largest source of inorganic carbon is limestones, dolomite, etc.