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. 10. Miyoshi , T , Pascui , O , Reichert , D 2004 Slow chain dynamics in isotactic-poly(4-methyl-1-pentene) crystallites near the glass transition temperature characterized by solid-state C-13 MAS exchange NMR
diiodobis(acridine)palladium(II), PdI 2 (C 13 H 9 N) 2 . Z. Kristallogr . NCS . 2010 ; 225 : 693 – 694 . 40. Halligudi , SB , Bhatt , KN , Khan , NH , Kurashy , RI , Venkatsubramanian
(about 9%) up to 160 °C. The adsorbed water content of CS and PS- g -starch copolymer determined by TG measurements is in the agreement with the literature data obtained in air-oven drying at 105 °C [ 13 ]. It refers to the highly hygroscopic nature of CS
Study of thermal properties of intumescent additive
Pentaerythritol phosphate alcohol
C 13 H 14 1,4,5-Trimethylnaphthalene 20 15.88 184 C 14 H 16 1,2,3,4-Tetramethylnaphthalene
, Lentz , A , Rastatter , S . Thermal gravimetry, mass spectrometry and solid-state C-13 NMR spectroscopy—simple and efficient methods to characterize the inclusion behaviour of p -tert-butylcalix[ n ]arenes . J Chem Soc Perkin Trans . 1998 ; 2 : 75
the procedure was in both cases comparable, amounting to approximately 2 °C [ 13 ]. Burr et al. applied thermistor sensors in their research to measure temperature changes under the influence of sonotherapy in the interior structures of the
transition from the variety of regular structure (C–In 2 (MoO 4 ) 3 , a = 13.34 ± 0.07 Å) [ 9 ] to the variety of orthorhombic structure (R–In 2 (MoO 4 ) 3 , a = 9.447 Å, b = 9.597 Å, c = 13.29 Å) [ 10 ]. The authors of the study [ 10 ] gave the
layer and one component was observed. Yield: % 71, 3.31 g. Anal. calcd. for C 13 H 19 N 3 O, (233.31 g/mol): C 66.9; H 8.2; N 18.1%. Found: C 66.7; H 8.4; N 18.3%. FTIR (KBr, cm −1 ): 3057 ν(Ar–CH), 2949–2812 ν(R–CH), 1648 ν(CH=N). 1 H NMR (δ, ppm, CDCl
microbiological analysis Water content (WC) was determined by drying an aliquot of soil (2×) until constant weight at 105 °C [ 13 ]. Field capacity humidity (FCH) was determined by the graduated cylinder method [ 14 ]. The pH was measured with a glass
of T h from −1.8 (a), −1.7 (b), −1.5 (c), −1.3 (d) to −1.1 °C (e), indicating that the amount of ice nuclei in the equilibrium sample decreased accordingly. Recrystallization of the melted part started immediately after the temperature dropped, and
