Monitoring the crystallization of amylose–lipid complexes during maize starch melting by synchrotron x‐ray diffraction

Most starch granules exhibit a natural crystallinity, with different diffraction patterns according to their botanical origin: A‐type from cereals and B‐type from tubers. The V polymorph results essentially from the complexing of amylose with compounds such as iodine, alcohols, or lipids. The intensity and nature of phase transitions (annealing, melting, polymorphic transitions, recrystallization, etc.) induced by hydrothermal treatments in crystalline structures are related to temperature and water content. Despite its small concentration, the lipid phase present mainly in cereal starches has a large influence on starch properties, particularly in complexing amylose. The formation of Vh crystalline structures was observed by synchrotron x‐ray diffraction in native maize starch heated at intermediate and high moisture contents (between 19 and 80%). For the first time, the crystallization of amylose–lipid complexes was evidenced in situ by x‐ray diffraction without any preliminary cooling, at heating rates corresponding to the usual conditions for differential scanning calorimetry experiments. For higher water contents, the crystallization of Vh complexes clearly occurred at 110–115°C. For intermediate water contents, mixed A + Vh (or B + Vh for high amylose starch) diffraction diagrams were recorded. Two mechanisms can be involved in amylose complexing: the first relating to crystallization of the amylose and lipid released during starch gelatinization, and the second to crystalline packing of separate complexed amylose chains (amorphous complexes) present in native cereal starches. © 1999 John Wiley & Sons, Inc. Biopoly 50: 99–110, 1999     

Anaerobic/Aerobic Composting of Soil Contaminated with 2,4,6-Trinitrotoluene

A loam soil from Pennsylvania without a history of exposure to explosives was incubated with 5 g kg^-1 of ¹⁵N-labeled 2,4,6-trinitrotoluene (TNT) and 200 μCi kg^-1 of ¹⁴C-TNT for 3 days and then amended with compost at a 1:2 soil to compost ratio. The compost was prepared by mixing 40% alfalfa hay, 40% grass hay, 10% spent mushroom compost, and 10% municipal biosolids. The mixture of soil and compost was inoculated with methanogens from cattle manure, amended with glucose and starch, and incubated for 37 days under anaerobic conditions. The anaerobic incubation was followed by 26 days of forced aerobic incubation. At the end of the aerobic phase, most of the radioactivity was associated with organic matter; only 8.7% could be extracted with water and methanol, but no TNT was present in the extracts as determined by high-performance liquid chromatography. The unextractable radioactivity was associated with humic acid (40.0±1.0%), fulvic acid (14.3±1.4%), and humin (28.2±0.5%). Radioactive materials associated with humic acid and humin were analyzed by solid-state ¹⁵N-nuclear magnetic resonance (NMR) spectrometry. The NMR spectra indicated that nitro groups of TNT had been reduced to amino groups thatwere subsequently involved in the formation of covalent bonds with soil organic matter.     

Timing Light Treatment for Eastward and Westward Travel Preparation

Jet lag degrades performance and operational readiness of recently deployed military personnel and other travelers. The objective of the studies reported here was to determine, using a narrow bandwidth light tower (500 nm), the optimum timing of light treatment to hasten adaptive circadian phase advance and delay. Three counterbalanced treatment order, repeated measures studies were conducted to compare melatonin suppression and phase shift across multiple light treatment timings. In Experiment 1, 14 normal healthy volunteers (8 men/6 women) aged 34.9±8.2 yrs (mean±SD) underwent light treatment at the following times: A) 06:00 to 07:00 h, B) 05:30 to 07:30 h, and C) 09:00 to 10:00 h (active control). In Experiment 2, 13 normal healthy subjects (7 men/6 women) aged 35.6±6.9 yrs, underwent light treatment at each of the following times: A) 06:00 to 07:00 h, B) 07:00 to 08:00 h, C) 08:00 to 09:00 h, and a no-light control session (D) from 07:00 to 08:00 h. In Experiment 3, 10 normal healthy subjects (6 men/4 women) aged 37.0±7.7 yrs underwent light treatment at the following times: A) 02:00 to 03:00 h, B) 02:30 to 03:30 h, and C) 03:00 to 04:00 h, with a no-light control (D) from 02:30 to 03:30 h. Dim light melatonin onset (DLMO) was established by two methods: when salivary melatonin levels exceeded a 1.0 pg/ml threshold, and when salivary melatonin levels exceeded three times the 0.9 pg/ml sensitivity of the radioimmunoasssy. Using the 1.0 pg/ml DLMO, significant phase advances were found in Experiment 1 for conditions A (p?<?.028) and B (p?<?0.004). Experiment 2 showed significant phase advances in conditions A (p?<?0.018) and B (p?<?0.003) but not C (p?<?0.23), relative to condition D. In Experiment 3, only condition B (p?<?0.035) provided a significant phase delay relative to condition D. Similar but generally smaller phase shifts were found with the 2.7 pg/ml DLMO method. This threshold was used to analyze phase shifts against circadian time of the start of light treatment for all three experiments. The best fit curve applied to these data (R²?=?0.94) provided a partial phase-response curve with maximum advance at approximately 9–11 h and maximum delay at approximately 5–6 h following DLMO. These data suggest largest phase advances will result when light treatment is started between 06:00 and 08:00 h, and greatest phase delays will result from light treatment started between 02:00 to 03:00 h in entrained subjects with a regular sleep wake cycle (23:00 to 07:00 h).     

微生物协同Fe0氧化的环境修复作用研究进展

零价铁(Fe0)具有高效还原转化多种污染物的能力,但不能实现污染物的矿化作用。微生物与Fe0的协同作用过程,以微生物为主导,Fe0起促进作用,可有效提高多种污染物的降解效率,实现污染物的彻底脱毒与无害化,因此利用微生物协同Fe0氧化进行环境修复具有广阔的应用前景。本文从微生物协同Fe0氧化的作用机理、菌种多样性及其在环境修复中的应用等研究进展进行综述,提出微生物协同Fe0氧化的环境修复研究中存在的主要问题和重点研究方向,以期在更全面、深入地认识这一过程的基础上,充分发挥其在环境修复中的作用。     

Investigation of optical attenuation imaging using optical coherence tomography for monitoring of scars undergoing fractional laser treatment

We demonstrate the use of the near‐infrared attenuation coefficient, measured using optical coherence tomography (OCT), in longitudinal assessment of hypertrophic burn scars undergoing fractional laser treatment. The measurement method incorporates blood vessel detection by speckle decorrelation and masking, and a robust regression estimator to produce 2D en face parametric images of the attenuation coefficient of the dermis. Through reliable co‐location of the field of view across pre‐ and post‐treatment imaging sessions, the study was able to quantify changes in the attenuation coefficient of the dermis over a period of ～20 weeks in seven patients. Minimal variation was observed in the mean attenuation coefficient of normal skin and control (untreated) mature scars, as expected. However, a significant decrease (13 ± 5%, mean ± standard deviation) was observed in the treated mature scars, resulting in a greater distinction from normal skin in response to localized damage from the laser treatment. By contrast, we observed an increase in the mean attenuation coefficient of treated (31 ± 27%) and control (27 ± 20%) immature scars, with numerical values incrementally approaching normal skin as the healing progressed. This pilot study supports conducting a more extensive investigation of OCT attenuation imaging for quantitative longitudinal monitoring of scars.

En face 2D OCT attenuation coefficient map of a treated immature scar derived from the pre‐treatment (top) and the post‐treatment (bottom) scans. (Vasculature (black) is masked out.) The scale bars are 0.5 mm.     

治疗腹膜后血肿的临床探讨

目的:探讨治疗腹膜后血肿的临床疗效。方法:对腹膜后血肿106例分型、诊断及治疗进行了回顾性分析。结果:腹膜后血肿无特异性症状和体征,可通过休克、腹穿、放射、超声波、尿路及血管造影等提高诊断,手术79例,非手术19例,死亡8例。结论:对腹膜后血肿的早期诊断及救治是提高生存率的关键。     

2株耐低温微生物处理污水模拟试验初报

从下水管道的污泥中分离筛选到耐冷细菌H6和耐冷酵母菌J1,采用此2菌株进行模拟污水低温(8℃)处理试验。H6和J1菌株对模拟污水COD的去除率分别为66.6%和72.2%;H6、J1菌株对有机氮去除率分别为76.9%和64.5%;H6、J1菌株对总磷去除率分别为53.9%和14.0%。说明低温微生物在低温环境的污水处理具有广阔的应用前景。