荧光原位杂交技术对土壤石油降解菌的检测

从辽河油田样品中筛选出一株高效石油降解菌,经鉴定为地衣芽孢杆菌。针对其16SrRNA设计寡核苷酸探针。荧光原位杂交(FISH)技术利用寡核苷酸探针检测特定细胞内的互补核苷酸序列。通过对纯菌和泥浆中地衣芽孢杆菌的FISH进行优化,得到泥浆中地衣芽孢杆菌的荧光原位杂交实验条件:样品固定时间17h,杂交温度46℃,杂交时间3h,杂交液中去离子甲酰胺浓度35%,冲洗缓冲液中与去离子甲酰胺对应的NaCl的浓度88mmol.L-1。运用上述FISH技术监测生物泥浆反应器中地衣芽孢杆菌量的变化,并与泥浆中含油率的变化进行比较,二者的变化情况符合微生物降解石油的趋势,为监测含油污泥中微生物的变化提供了一种可行的技术。

Investigation of Degradation Behavior of Polymer on Surface of Film Due to the Existence of Monochromatic X-ray

Degradation and its temperature dependence of poly(methyl methacrylate) (PMMA) in the blend film of PMMA/SAN were investigated via ire-situ X-ray photoelectron spectroscopy(XPS). The results show that thermal degradation of PMMA takes place at 185, 130, 80 degrees C and even room temperature due to the existence of monochromatic X-ray. Furthermore, the degradation rate depends crucially on the experiment temperature.

DEHYDROGENATION OF ORGANOLANTHANIDE ALKOXIDES AND X-RAY CRYSTAL-STRUCTURE OF REACTION-PRODUCT [(C5H-5)2YB(MU-OCH=C=CH2)]2

[Cp3Yb] reacts with HOR (Cp = C5H5; R = CH2CH=CH2, CH2CH2Me) in thf (thf = tetrahydrofuran)at room temperature to give complexes [{Cp2Yb(mu-OR)}2], which are dehydrogenated to yield the new complex [{Cp2Yb(mu-OCH=C=CH2)}2] in refluxing thf solution; the X-ray crystal structure shows that the new complex is dimeric with oxygen atoms as bridging groups.

高寒草甸不同土地利用格局土壤CO_2的释放量

分析高寒草甸不同土地利用格局下土壤CO2的释放量大小表明,在植物生长季的5～9 月,土壤CO2 释放量大小排序为:金露梅灌丛草甸(1871.40g/ m2) > 矮嵩草草甸(1769.63g/ m2) > 退化金露梅灌丛草甸(1495.60g/m2) > 退化矮嵩草草甸(1191.26g/ m2) ；而在植物非生长季的10月到翌年4月,其土壤CO2 释放量大小与植物生长季略有差异, 表现出矮嵩草草甸(661.46g/ m2 ) > 金露梅灌丛草甸( 550.90g/ m2 ) > 退化矮嵩草草甸(502.50g/ m2) > 退化金露梅灌丛草甸(384.50g/ m2) 的特点;全年内表现为矮嵩草草甸(2431.09g/ m2 ) > 金露梅灌丛草甸(2422.30g/ m2) > 退化金露梅灌丛草甸(1880.10g/ m2 ) > 退化矮嵩草草甸(1694.06g/ m2 ) . 高寒草甸地区不同土地利用格局土壤CO2 释放数量的差异及季节变化,不仅与各利用格局的土壤生物活性及土壤物理化学性状有关,而且与气象条件(特别是温度) 及其土壤冬季冻结期长短关系极为密切。

Identification of phenolics and nucleoside derivatives in Gastrodia elata by HPLC-UV-MS

An HPLC-UV-MS method for simultaneous identification of predominant phenolics and minor nucleoside derivatives in Gastrodia elata was developed, which was based on their UV and MS characteristics summarized through a series of homemade reference standard experiments. Phenolics showed characteristic UV lambda(max) at 267 nm, [M + NH4](+) base peak in positive mode and [M - H](-) base peak in negative mode while nucleosides exhibited UV lambda(max) at 255 nm, [M + H](+), [M - H + 2H(2)O](-) or [M - H + CH3COOH](-). Phenolics conjugates mainly underwent the consecutive loss of gastrodin residue (- 268 U) and the combined loss of H2O and CO2 from the citric acid unit under negative MS/MS conditions whereas nucleosides simply lost the ribose (- 132 U) under positive MS/MS conditions. According to these characteristics, a special pattern under MS/MS conditions and reported compound data for G. elata in the literature, not only 15 phenolics were identified but also 6 nucleoside derivatives were identified. Among these compounds, seven phenolics and three nucleoside derivatives have not been reported yet from G. elata.

微地域搬运——碳酸盐岩红色风化壳形成过程的一种方式

由于差异溶蚀作用,由碳酸盐岩强烈风化形成的红色风化壳通常表现出独特的剖面构型:风化壳发育深厚、下伏基岩面强烈起伏波动、溶沟和石牙相间展布。以黔中岩溶台地之上发育的红色风化壳——平坝剖面为例,通过宏观地质、地球化学、粒度分析以及矿物学等方法,并以邻近的两个石灰土剖面(罗吏剖面和龙洞堡剖面)作对比,对碳酸盐岩红色风化壳的形成过程进行了讨论,论证了微地域搬运是碳酸盐岩红色风化壳尤其是厚层红色风化壳形成过程的一种方式。溶沟部位的风化壳,从风化前锋向上的一定深度范围内,为原位残积风化的产物(残积层);在此深度以上的部分,为地势较高的相邻石牙部位不同风化程度的残积物的搬运堆积(堆积层),也是导致风化指标随深度呈锯齿状波动的直接原因。