J
Jianxi Zhu
Researcher at Chinese Academy of Sciences
Publications - 282
Citations - 12526
Jianxi Zhu is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Adsorption & Montmorillonite. The author has an hindex of 54, co-authored 254 publications receiving 9673 citations. Previous affiliations of Jianxi Zhu include Zhejiang University & Center for Excellence in Education.
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Fabrication of layered double hydroxide/carbon nanomaterial for heavy metals removal
TL;DR: In this article, the composites were directly prepared by in situ formation of carbon nanosheets via hydrothermal or high-temperature carbonization of organic double hydroxide (LDH)/sheet-shaped carbon composites.
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TiO2/Schwertmannite nanocomposites as superior co-catalysts in heterogeneous photo-Fenton process.
TL;DR: Novel photo-Fenton catalysts are developed by simply milling commercially available TiO2 with Schwertmannite (Sh), a natural iron-oxyhydroxysulfate nanomineral to support the hypothesis that the photo-generated electrons could migrate fromTiO2 to Sh on the composites.
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In situ sequentially generation of acid and ferrous ions for environmental remediation
Lingya Ma,Suramya I. Rathnayake,Hongping He,Runliang Zhu,Jianxi Zhu,Godwin A. Ayoko,Jihong Li,Yunfei Xi,Yunfei Xi +8 more
TL;DR: In this article, a heterogeneous Fenton composite material was developed by grafting acid precursors and nano zero-valent iron particles on an acid leached diatomite, which can sequentially generate acid and ferrous ions in situ.
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Effects of solid acidity of clay minerals on the thermal decomposition of 12-aminolauric acid
TL;DR: In this paper, the effects of four types of clay minerals on the thermal decomposition of 12-aminolauric acid (ALA) were investigated, and the derivative thermogravimetry results indicated that all clay minerals exhibited catalytic activity on the decomposition.
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Kaolinization of 2:1 type clay minerals with different swelling properties
TL;DR: In this article, the authors investigated the specific behavior of 2:1 type swelling and non-swelling clay minerals during kaolinization and showed that the size and stacking order of the newly formed kaolinite strongly depend on the morphology and property of the precursor minerals.