Пориста кераміка та металогодридні матеріали для ефективного зберігання водню
Анотація
У цій роботі ми досліджували синтезовані пористі алюмосилікатні матеріали з вигораючими добавками, що утворюють однофазну кубічну структуру цеолітного типу (Fm3m, a = 4,056 Å). Пориста кераміка цеолітного складу за температури 200°C та тиску водню 12 атм демонструвала поглинання водню в кількості 11 мас.%. Також ми досліджували вихідний металевий літій (BCC, a≈3,507 Å), який піддавався гідрування в розробленому герметичному реакторі при 12 атм та 700 °C з утворенням гідриду LiH (FCC, типу NaCl, a ≈ 4,081 Å, d111 ≈ 2,356 Å). Середній розмір кристалітів LiH не перевищує 100 нм, а максимальна воднева ємність літію досягла 12,4 мас.%. Розроблений реактор дозволяє безпечно проводити гідрування за високої температури та високого тиску. Ці дані демонструють потенціал гідридів літію, титану та натрію, а також пористих алюмосилікатів для накопичення, зберігання та транспортування водню.
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Посилання
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Авторське право (c) 2026 М.С. Пайзуллаханов, О.Р. Парпієв, Ф.А. Гіясовa, С.У. Турапова, Е.З. Нодірматов, М.А. Юлдошев, О.Т. Ісманова, Ф.А. Гіясов, А. Егамбердієв, С.К. Абдіжалієв, М.А. Джалелов, С.А. Турсінбаєв, А.А. Абдувахобов
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Автори, які публікуються у цьому журналі, погоджуються з наступними умовами:
- Автори залишають за собою право на авторство своєї роботи та передають журналу право першої публікації цієї роботи на умовах ліцензії Creative Commons Attribution License, котра дозволяє іншим особам вільно розповсюджувати опубліковану роботу з обов'язковим посиланням на авторів оригінальної роботи та першу публікацію роботи у цьому журналі.
- Автори мають право укладати самостійні додаткові угоди щодо неексклюзивного розповсюдження роботи у тому вигляді, в якому вона була опублікована цим журналом (наприклад, розміщувати роботу в електронному сховищі установи або публікувати у складі монографії), за умови збереження посилання на першу публікацію роботи у цьому журналі.
- Політика журналу дозволяє і заохочує розміщення авторами в мережі Інтернет (наприклад, у сховищах установ або на особистих веб-сайтах) рукопису роботи, як до подання цього рукопису до редакції, так і під час його редакційного опрацювання, оскільки це сприяє виникненню продуктивної наукової дискусії та позитивно позначається на оперативності та динаміці цитування опублікованої роботи (див. The Effect of Open Access).
