Difference between Petrol and Diesel Engine Difference between Physical and Chemical Change Difference Between Physical and Chemical Properties Difference Between Polar and Nonpolar Difference between primary cell and secondary cell Difference Between Pure Substance and Mixture Difference Between Rusting and Corro...
Ferrocene is an organometallic compound and it is an antiknock agent that is used in fuel for petrol engines. It is a toxic element when it is swallowed. Answer and Explanation: Learn more about this topic: Acetylation of Ferrocene | Definition & Mechanism ...
What is petrol's melting point? What metal has the lowest melting point? Which halogens are gases at STP? What is promethium's freezing point? What group are the noble gases in? What state is argon at room temperature? What is carbon's state of matter at room temperature?
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Petrol – gasoline (for sniffing) P.F. – crack cocaine in aspirin-sized tablets as a disguise P.G. – paregoric Phennies – phenobarbital Phenos – phenobarbital Phillies Blunt – cigar hollowed out and filled with marijuana Picked up – smoked marijuana Pin – thinly-rolled marijuana cigare...
View Solution From a tank of petrol, which contains 200 litres of petrol, the seller replaces each time with kerosene when he sells 40 litres of petrol(or its mixture). Everything he sells out only 40 litres of petrol(pure or impure). After replacing the petrol with kerosene 4th time, ...
Example: Water, milk, kerosene, petrol, alcohol are the examples of the substance which exist in the liquid state. The Gaseous StateOut of the three states of matter, the interparticle spaces are the maximum in the gaseous state. It is because the interparticle forces which hold the different...
the materials that are produced by the chemical industry, and the equipment that is used to produce them, vary very widely—from pig iron made in blast furnaces and petrol in refineries to pharmaceuticals made in glassware and precious metal salts at the bench; (3) the chemical industry supp...
Carbonate mud is crucial in the global carbon cycle and serves as a key sedimentary archive for paleoclimate reconstruction. Understanding the mechanisms behind its formation is crucial for explaining long-term carbon storage, including atmospheric carbo
aqua, aquamarine, azure, Cambridge blue, cerulean, clear blue, cobalt blue, Copenhagen blue, cyan, duck-egg blue, electric blue, gentian blue, heliotrope, indigo, lapis lazuli, midnight blue, navy blue, Nile blue, Oxford blue, peacock blue, periwinkle, perse, petrol blue, pewter, royal blue...