Sources of common compounds: 705-24-8

These compound has a wide range of applications. It is believed that with the continuous development of the source of the synthetic route,705-24-8, its application will become more common.

705-24-8, In the chemical reaction process,reaction time,type of solvent,can easily affect the result of the reaction, thereby determining the yield and properties of the reaction product.An updated downstream synthesis route of 705-24-8 as follows.

To a solution of 1 -methylpiperidin-4-ol (35 mg, 0.30 mmol) in THF (0.5 mL) at 0C was added 60% NaH (12 mg, 0.30 mmol). After the mixture was stirred for 20 minutes, a solution of Intermediate 2 (42 mg, 0.10 mmol) in THF (0.5 mL) was added. Then the ice bath was removed, and the reaction mixture was stirred at room temperature for two hours. The reaction was quenched by water (0.1 mL), and concentrated. The residue was purified directly by MS-HPLC to afford Compound 39 (18 mg, 35%). LCMS (method A): m/z 503.4 (M+H)+. ‘H NMR (CDCI3) delta 8.50 (s, 1H), 77.44 (d, 2H), 7.17 (d, 2H), 5.72 (d, 1H), 5.31 (m, 1H), 4.60 (br, 1H), 3.60 (m, 1H), 3.40 (m, 2H), 3.24 (br, 1H), 3.03 (br, 2H), 2.92-2.77 (m, 4H), 2.40 (br, 1H), 2.25 (m, 3H), 2.1 1-1.88 (m,4H); Following procedure as described in Example 2, and replacing THF with DMF, piperidine-2,4-dione (249 mg, 2.20 mmol) was converted to Compound 3A. The crude material was purified by silica gel chromatography (0-90% EA/hexane) to afford Compound 3A (375 mg, 64%). LCMS (method A): m/z 294.3 (M+H)+. XH NMR (CDC13): delta 7.14 (s, 1H), 5.97 (br s, 1H), 5.83 (s, 1H), 3.60 (t, 2H), 2.72 (m, 2H).

These compound has a wide range of applications. It is believed that with the continuous development of the source of the synthetic route,705-24-8, its application will become more common.

Reference:
Patent; VENENUM BIODESIGN LLC; HUANG, Chia-Yu; MCGUINNESS, Brian F; XU, Xiaoqing; KULTGEN, Steven G.; MCMASTER, Ellen Sieber; BEASLEY, James R.; (356 pag.)WO2018/5794; (2018); A2;,
Pyrimidine | C4H4N2 – PubChem,
Pyrimidine – Wikipedia