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Gel phase in hydrated calcium dipicolinate
Author(s) -
Pankaj Rajak,
Ankit Mishra,
Chunyang Sheng,
Subodh Tiwari,
Aravind Krishnamoorthy,
Rajiv K. Kalia,
Aiichiro Nakano,
Priya Vashishta
Publication year - 2017
Publication title -
applied physics letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.182
H-Index - 442
eISSN - 1077-3118
pISSN - 0003-6951
DOI - 10.1063/1.5000394
Subject(s) - dipicolinic acid , bacterial spore , chemistry , thermal diffusivity , phase diagram , phase transition , endospore , chemical engineering , phase (matter) , ion , spore , analytical chemistry (journal) , materials science , thermodynamics , chromatography , organic chemistry , botany , physics , engineering , biology
The mineralization of dipicolinic acid (DPA) molecules in bacterial spore cores with Ca2+ ions to form Ca-DPA is critical to the wet-heat resistance of spores. This resistance to “wet-heat” also depends on the physical properties of water and DPA in the hydrated Ca-DPA-rich protoplasm. Using reactive molecular dynamics simulations, we have determined the phase diagram of hydrated Ca-DPA as a function of temperature and water concentration, which shows the existence of a gel phase along with distinct solid-gel and gel-liquid phase transitions. Simulations reveal monotonically decreasing solid-gel-liquid transition temperatures with increasing hydration, which explains the experimental trend of wet-heat resistance of bacterial spores. Our observation of different phases of water also reconciles previous conflicting experimental findings on the state of water in bacterial spores. Further comparison with an unmineralized hydrated DPA system allows us to quantify the importance of Ca mineralization in decreasi...

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