Intercalation of carbamide to globular glauconite by chemical processing for the creation of slow-release nanocomposites; Applied Clay Science; Vol. 243

書誌詳細
Parent link:Applied Clay Science.— .— Amsterdam: Elsevier Science Publishing Company Inc.
Vol. 243.— 2023.— Article number 107075, 10 p.
その他の著者: Rudmin M. A. Maksim Andreevich, Maksimov P. N. Prokopy Nikolaevich, Dasi Evan Shvan Salo, Kurovsky A. V. Aleksandr Vasiljevich, Gummer Ya. Yana, Ibraeva K. Kanipa, Kutugin V. A. Viktor Aleksandrovich, Soktoev B. R. Bulat Rinchinovich, Ponomarev K. O. Konstantin Olegovich, Tararushkin E. V. Evgeny Viktorovich, Makarov B. I. Boris Igorevich, Ruban A. S. Aleksey Sergeevich
要約:Title screen
This article investigates the intercalation of carbamide within globular glauconite involving the chemical activation of glauconite with carbamide solution-gel at varying concentrations of total nitrogen (N). Mineral nanocomposites were prepared with a multitude of novel functions. As the N concentration of the initial solution increased, the proportion of intercalated N enhanced to 8%. A 20% of N concentration in carbamide solution maximizes intercalation. Intercalation occurs in the interlayer of smectite layers (micropores) in glauconite. In nanocomposites, the decrease in specific surface space, total volume pores, and average pore size reflect the absorption of carbamide in meso- and macropores of glauconite globules. Glauconite nanocomposites retain a spherical particle morphology and a distinct microlayer close to the surface. The increased proportion of nitrogen in the microlayers close to the surface indicates a high filtration capacity of the globules. The near-surface microlayer serves as a diffusion channel for the glauconite interior, where new substances are absorbed in the micro- (interlayer) and macropores. The stepwise kinetics of nutrient release, which supports the various forms of carbamide absorption in glauconite, distinguishes the nanocomposites. In addition to N-compounds, glauconite nanocomposites are mineral sources of the available potassium (K) in soils. As a result, chemically manufactured glauconite nanocomposites have some following advantages: the micro-granular mineral form, a permeable inner near-surface microlayer, incubated in micro-, meso-, and macropores N-compounds, and the available K
Текстовый файл
AM_Agreement
言語:英語
出版事項: 2023
主題:
オンライン・アクセス:https://doi.org/10.1016/j.clay.2023.107075
フォーマット: 電子媒体 図書の章
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=680333

MARC

LEADER 00000naa0a2200000 4500
001 680333
005 20251223160924.0
090 |a 680333 
100 |a 20250526d2023 k||y0rusy50 ba 
101 0 |a eng 
102 |a NL 
135 |a drcn ---uucaa 
181 0 |a i   |b  e  
182 0 |a b 
183 0 |a cr  |2 RDAcarrier 
200 1 |a Intercalation of carbamide to globular glauconite by chemical processing for the creation of slow-release nanocomposites  |f Maxim Rudmin, Prokopiy Maximov, Evan Dasi [et al.] 
203 |a Текст  |b визуальный  |c электронный 
283 |a online_resource  |2 RDAcarrier 
300 |a Title screen 
320 |a References: 100 tit 
330 |a This article investigates the intercalation of carbamide within globular glauconite involving the chemical activation of glauconite with carbamide solution-gel at varying concentrations of total nitrogen (N). Mineral nanocomposites were prepared with a multitude of novel functions. As the N concentration of the initial solution increased, the proportion of intercalated N enhanced to 8%. A 20% of N concentration in carbamide solution maximizes intercalation. Intercalation occurs in the interlayer of smectite layers (micropores) in glauconite. In nanocomposites, the decrease in specific surface space, total volume pores, and average pore size reflect the absorption of carbamide in meso- and macropores of glauconite globules. Glauconite nanocomposites retain a spherical particle morphology and a distinct microlayer close to the surface. The increased proportion of nitrogen in the microlayers close to the surface indicates a high filtration capacity of the globules. The near-surface microlayer serves as a diffusion channel for the glauconite interior, where new substances are absorbed in the micro- (interlayer) and macropores. The stepwise kinetics of nutrient release, which supports the various forms of carbamide absorption in glauconite, distinguishes the nanocomposites. In addition to N-compounds, glauconite nanocomposites are mineral sources of the available potassium (K) in soils. As a result, chemically manufactured glauconite nanocomposites have some following advantages: the micro-granular mineral form, a permeable inner near-surface microlayer, incubated in micro-, meso-, and macropores N-compounds, and the available K 
336 |a Текстовый файл 
371 |a AM_Agreement 
461 1 |t Applied Clay Science  |c Amsterdam  |n Elsevier Science Publishing Company Inc. 
463 1 |t Vol. 243  |v Article number 107075, 10 p.  |d 2023 
610 1 |a электронный ресурс 
610 1 |a труды учёных ТПУ 
610 1 |a Glauconite 
610 1 |a Carbamide 
610 1 |a Nitrogen intercalation 
610 1 |a Globules 
610 1 |a Potassium 
610 1 |a Slow-release fertiliser 
701 1 |a Rudmin  |b M. A.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of Geological and Mineralogical Sciences  |f 1989-  |g Maksim Andreevich  |9 16999 
701 1 |a Maksimov  |b P. N.  |c Geologist  |c Educational master of Tomsk Polytechnic University  |f 1998-  |g Prokopy Nikolaevich  |9 22828 
701 0 |a Dasi Evan Shvan Salo 
701 1 |a Kurovsky  |b A. V.  |g Aleksandr Vasiljevich 
701 1 |a Gummer  |b Ya.  |g Yana 
701 1 |a Ibraeva  |b K.  |g Kanipa 
701 1 |a Kutugin  |b V. A.  |c Chemical Engineer  |c Associate Professor of Tomsk Polytechnic University, Candidate of Technical Sciences  |f 1983-  |g Viktor Aleksandrovich  |9 18177 
701 1 |a Soktoev  |b B. R.  |c Geochemist  |c Associate Professor of the Department of Tomsk Polytechnic University, Candidate of Geological and Mineralogical Sciences  |f 1990-  |g Bulat Rinchinovich  |y Tomsk  |9 18268 
701 1 |a Ponomarev  |b K. O.  |g Konstantin Olegovich 
701 1 |a Tararushkin  |b E. V.  |g Evgeny Viktorovich 
701 1 |a Makarov  |b B. I.  |g Boris Igorevich  |f 1989-  |c geologist  |c Associate Scientist of Tomsk Polytechnic University  |y Tomsk  |9 88909 
701 1 |a Ruban  |b A. S.  |c geologist  |c engineer of Tomsk Polytechnic University  |f 1991-  |g Aleksey Sergeevich  |9 17590 
801 0 |a RU  |b 63413507  |c 20250526 
850 |a 63413507 
856 4 |u https://doi.org/10.1016/j.clay.2023.107075  |z https://doi.org/10.1016/j.clay.2023.107075 
942 |c CF