MR弥散加权成像对鉴别诊断良恶性椎体压缩性骨折的临床价值研究

目的：探讨MR弥散加权成像（DWI）鉴别诊断良恶性椎体压缩性骨折的临床价值。方法：对57例经临床或病理证实的椎体良恶性压缩性骨折患者行矢状位T1M、T2WI、T2WI／FS及DWI扫描,研究其在常规序列和DWI序列上的表现,将常规MR序列和DWI序列检出率进行比较,测量正常椎体及病变椎体的表观弥散系数（ADC）值,并进行统计学分析。结果：（1）MR常规序列和DWI序列（b=500s／mm2）表现：良性椎体压缩性骨折呈长T1长或等T2改变,T2WI／FS呈高信号,DWI可以呈高信号、等信号及低信号;恶性椎体压缩性骨折呈长T1长T2信号,大部分病灶T2WUFS及DWI呈高信号,少数变现为低信号;（2）MR常规序列和DWI序列（b=500s／mm2）病灶检出率的比较：T1WI、T2WI／FS及DWI序列病灶检出率均高于T2WI序列,其间的差别有显著性意义（P〈0．01）,T1WI、T2WI／FS及DWI序列病灶检出率之间无显著性差异（P〉0．01）;（3）ADC值比较：在DWI（b=500s／mm2）上,良性组ADC值为（2．03±0．83）×10^3mm^2/s,恶性组ADC值为（1．37±0．75）×10^-3mm^2/s,正常组ADC值为（0．36±0．21）×10^-3mm^2／s,成像条件相同时,良性组高于恶性组,两组间有明显的统计学意义（P〈0．05）。结论：DWI可较好的反映椎体的弥散特征,ADC值作为量化指标可对良恶性椎体压缩性骨折进行可靠鉴别。     

模拟穿透雨减少对锐齿栎(Quercus aliena var. acuteserrata)树干液流密度的影响

降水格局变化是全球气候变化的重要特征之一,未来气候变化下,较为频繁和严峻的干旱将威胁地球中纬度部分地区的森林,但森林植被如何响应季节性干旱胁迫及其机制尚不清楚。北亚热带-暖温带过渡区分布着以锐齿栎(Quercus aliena var.acuteserrata)为优势树种的落叶阔叶林,研究其水分蒸腾代谢过程对干旱的响应是评估气候变化对过渡区天然落叶阔叶林生态系统水碳影响的关键科学问题。在典型的锐齿栎天然林中通过开展模拟穿透雨减少大型野外实验,采用Granier热扩散式探针技术监测锐齿栎树干液流密度的动态变化,研究了不同径级锐齿栎树干液流密度对模拟干旱的响应规律。结果表明:(1)穿透雨减少对树干液流密度的影响呈现季节变异。在7月份,林内穿透雨减少显著降低了锐齿栎的树干液流密度,但生长季后期的10月份林内穿透雨减少反而使锐齿栎树干液流密度显著升高。(2)不同径级的锐齿栎树干液流密度在生长季内对干旱有不同的响应,特别是小径级的树干液流密度与其他径级有较多的不同。小径级的锐齿栎树干液流密度在5、7月份表现为减雨样地显著小于对照样地,在9、10月份则表现为减雨样地显著大于对照样地。中径级的锐齿栎树干液流密度在5、10月份表现为减雨样地显著大于对照样地,在7月份则表现为减雨样地极显著小于对照样地。大径级的锐齿栎树干液流密度在6、7月份表现为减雨样地显著小于对照样地,在10月份则表现为减雨样地显著大于对照样地。     

Rates of root and organism growth, soil conditions, and temporal and spatial development of the rhizosphere

BACKGROUND: Roots growing in soil encounter physical, chemical and biological environments that influence their rhizospheres and affect plant growth. Exudates from roots can stimulate or inhibit soil organisms that may release nutrients, infect the root, or modify plant growth via signals. These rhizosphere processes are poorly understood in field conditions. SCOPE AND AIMS: We characterize roots and their rhizospheres and rates of growth in units of distance and time so that interactions with soil organisms can be better understood in field conditions. We review: (1) distances between components of the soil, including dead roots remnant from previous plants, and the distances between new roots, their rhizospheres and soil components; (2) characteristic times (distance(2)/diffusivity) for solutes to travel distances between roots and responsive soil organisms; (3) rates of movement and growth of soil organisms; (4) rates of extension of roots, and how these relate to the rates of anatomical and biochemical ageing of root tissues and the development of the rhizosphere within the soil profile; and (5) numbers of micro-organisms in the rhizosphere and the dependence on the site of attachment to the growing tip. We consider temporal and spatial variation within the rhizosphere to understand the distribution of bacteria and fungi on roots in hard, unploughed soil, and the activities of organisms in the overlapping rhizospheres of living and dead roots clustered in gaps in most field soils. CONCLUSIONS: Rhizosphere distances, characteristic times for solute diffusion, and rates of root and organism growth must be considered to understand rhizosphere development. Many values used in our analysis were estimates. The paucity of reliable data underlines the rudimentary state of our knowledge of root-organism interactions in the field.     

4种温带森林非生长季土壤二氧化碳、甲烷和氧化亚氮通量

中高纬度森林土壤在漫长的非生长季中对重要温室气体——二氧化碳(CO2)、甲烷(CH4)和氧化亚氮(N2O)的释放或吸收在碳氮年收支中作用很大,但目前研究甚少。采用静态暗箱-气相色谱法,比较研究东北东部4种典型温带森林土壤表面CO2、CH4和N2O通量在非生长季中的时间动态及其影响因子。结果表明:4种森林土壤在非生长季中整体上均表现为CO2源、N2O源和CH4汇的功能。红松林、落叶松林、蒙古栎林、硬阔叶林的非生长季平均土壤表面CO2通量分别为(65.5±8.1)mgm-2h-1(平均值±标准差)、(70.5±10.2)mgm-2h-1、(77.1±8.0)mgm-2h-1、(80.5±23.5)mgm-2h-1;CH4通量分别为(-17.2±4.6)μgm-2h-1、(-15.4±4.2)μgm-2h-1、(-31.5±4.5)μgm-2h-1、(-23.6±4.1)μgm-2h-1;N2O通量分别为(19.3±5.1)μgm-2h-1、(11.5±2.5)μgm-2h-1、(16.4±4.0)μgm-2h-1、(14.4±5.4)μgm-2h-1;其中非生长季土壤表面CO2总排放量分别为143.4gm-2、162.8gm-2、189.9gm-2、252.7gm-2,分别占其年通量的7.3%、10.6%、8.4%和8.5%。所有林型非生长季土壤表面CO2通量在春季土壤解冻前均维持在较低水平;在解冻进程中随温度升高而增大。土壤表面CO2通量与5cm深土壤温度(T5)呈极显著的指数函数关系。在隆冬时节出现CH4净释放现象,但释放强度及其出现时间因林型而异,其中以红松林的释放强度较大,高达43.6μgm-2h-1。土壤表面CH4通量与T5呈显著的负相关。土壤表面N2O通量的时间动态格局在林型间的分异较大,但在春季土壤解冻阶段均释放出N2O,而释放峰值和出现时间因林型而异。土壤表面N2O通量与0—10cm深土壤含水量呈显著的正相关(红松林除外)。研究展示了不同温带森林类型的土壤水热条件对其非生长季土壤CO2、CH4和N2O通量的重要影响,但这3种温室气体的林型间分异的生物学机理尚需进一步研究。     

新疆玛纳斯热气泉免培养土壤细菌多样性分析

【目的】了解新疆玛纳斯热气泉土壤免培养细菌群落组成及多样性。【方法】采用免培养法直接从土壤样品中提取总DNA,利用细菌通用引物对土壤总DNA进行16S rDNA扩增,构建细菌16SrDNA文库。使用HaeⅢ限制性内切酶对阳性克隆进行限制性片段长度多态性分析(restriction fragment length polymorphism,RFLP),挑选具有不同酶切图谱的克隆进行测序、比对并构建16SrDNA系统发育树。【结果】从土壤细菌16S rDNA文库中随机挑选了170个阳性克隆,共得到29个不同的分类单元(operational taxonomic unit,OTU)。系统发育分析归为6个门:酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)、拟杆菌门(Bacteroidetes)、厚壁菌门(Firmicutes)、变形菌门(Proteobacteria)和浮霉菌门(Planctomycetes)。其中厚壁菌门(Firmicutes)为绝对优势类群,占整个细菌文库的71%。29个OTUs中有14条序列与GenBank中相关序列的相似性低于97%(序列长度约1.5kb),占序列总数的48%。【结论】热气泉土壤细菌种群多样性较低,但存在大量潜在细菌新种。     

Characterisation of glucose transport in Saccharomyces cerevisiae with plasma membrane vesicles (countertransport) and intact cells (initial uptake) with single Hxt1, Hxt2, Hxt3, Hxt4, Hxt6, Hxt7 or Gal2 transporters

The yeast glucose transporters Hxt1, Hxt2, Hxt3, Hxt4, Hxt6, Hxt7 and Gal2, individually expressed in an hxt1-7 null mutant strain, demonstrate the phenomenon of countertransport. Thus, these transporters, which are the most important glucose transporters in Saccharomyces cerevisiae, are facilitated diffusion transporters. Apparent K(m)-values from high to low affinity, determined from countertransport and initial-uptake experiments, respectively, are: Hxt6 0.9+/-0.2 and 1.4+/-0.1 mM, Hxt7 1.3+/-0.3 and 1.9+/-0.1 mM, Gal2 1.5 and 1.6+/-0.1 mM, Hxt2 2.9+/-0.3 and 4.6+/-0.3 mM, Hxt4 6.2+/-0.5 and 6.2+/-0.3 mM, Hxt3 28.6+/-6.8 and 34.2+/-3.2 mM, and Hxt1 107+/-49 and 129+/-9 mM. From both independent methods, countertransport and initial uptake, the same range of apparent K(m)-values was obtained for each transporter. In contrast to that in human erythrocytes, the facilitated diffusion transport mechanism of glucose in yeast was symmetric. Besides facilitated diffusion there existed in all single glucose transport mutants, except for the HXT1 strain, significant first-order behaviour.     

Sulfide oxidation at halo-alkaline conditions in a fed-batch bioreactor

A biotechnological process is described to remove hydrogen sulfide (H(2)S) from high-pressure natural gas and sour gases produced in the petrochemical industry. The process operates at halo-alkaline conditions and combines an aerobic sulfide-oxidizing reactor with an anaerobic sulfate (SO(4) (2-)) and thiosulfate (S(2)O(3) (2-)) reducing reactor. The feasibility of biological H(2)S oxidation at pH around 10 and total sodium concentration of 2 mol L(-1) was studied in gas-lift bioreactors, using halo-alkaliphilic sulfur-oxidizing bacteria (HA-SOB). Reactor operation at different oxygen to sulfide (O(2):H(2)S) supply ratios resulted in a stable low redox potential that was directly related with the polysulfide (S(x) (2-)) and total sulfide concentration in the bioreactor. Selectivity for SO(4) (2-) formation decreased with increasing S(x) (2-) and total sulfide concentrations. At total sulfide concentrations above 0.25 mmol L(-1), selectivity for SO(4) (2-) formation approached zero and the end products of H(2)S oxidation were elemental sulfur (S(0)) and S(2)O(3) (2-). Maximum selectivity for S(0) formation (83.3+/-0.7%) during stable reactor operation was obtained at a molar O(2):H(2)S supply ratio of 0.65. Under these conditions, intermediary S(x) (2-) plays a major role in the process. Instead of dissolved sulfide (HS(-)), S(x) (2-) seemed to be the most important electron donor for HA-SOB under S(0) producing conditions. In addition, abiotic oxidation of S(x) (2-) was the main cause of undesirable formation of S(2)O(3) (2-). The observed biomass growth yield under SO(4) (2-) producing conditions was 0.86 g N mol(-1) H(2)S. When selectivity for SO(4) (2-) formation was below 5%, almost no biomass growth was observed.     

库布齐沙漠东部不同生物结皮发育阶段土壤温室气体通量

以流动沙地为对照,采用时空替代法分析库布齐沙漠东部固定沙地上不同发育阶段生物结皮藻类结皮和地衣结皮土壤温室气体通量特征及其与环境因子之间的关系,研究生物结皮发育对荒漠土壤温室气体通量的影响.结果表明: 荒漠土壤CO₂排放通量大小为地衣结皮(128.5 mg·m^-2·h^-1)>藻结皮(70.2 mg·m^-2·h^-1)>流动沙地(48.2 mg·m^-2·h^-1),CH₄吸收通量大小为地衣结皮(30.4 μg·m^-2·h^-1)>藻结皮(21.2 μg·m^-2·h^-1)>流动沙地(18.2 μg·m^-2·h^-1),N₂O排放通量大小为地衣结皮(6.6 μg·m^-2·h^-1)>藻结皮(5.4 μg·m^-2·h^-1)>流动沙地(2.5 μg·m^-2·h^-1).CO₂排放具有明显的季节变化,生长季显著大于非生长季;CH₄和N₂O季节变化差异不显著,前者生长季吸收大于非生长季,后者非生长季排放大于生长季.土壤有机碳和全氮含量、土壤微生物数量均是影响温室气体通量的重要因素,环境水热因子是影响土壤CO₂排放的关键因子,但CH₄和N₂O通量对水热因子的变化不敏感.随着植被恢复和生物结皮发育,荒漠土壤温室气体累积通量的不断增大导致其百年尺度的全球增温潜势亦显著提高,依次为地衣结皮(1135.7 g CO₂-e·m^-2·a^-1)>藻结皮(626.5 g CO₂-e·m^-2·a^-1) >流动沙地(422.7 g CO₂-e·m^-2·a^-1).     

Incentivising fire management in Pindan (Acacia shrubland): A proposed fuel type for Australia's Savanna burning greenhouse gas emissions abatement methodology

The Australian Government has sanctioned development of greenhouse gas emissions (GHG) abatement methodologies to meet international emissions reduction obligations. Savanna burning emissions abatement methodologies have been available since 2012, and there are currently 72 registered projects covering approximately 32 million ha. Abatement to date has exceeded 4 million tonnes of carbon dioxide equivalent (CO2‐e) principally through the application of low intensity early dry season fire management to reduce the amount of biomass combusted in higher intensity late dry season (LDS) fires. Savanna burning projects can only be conducted on areas with eligible fire‐prone vegetation fuel types where implementing the improved fire management regime is considered ecologically appropriate. This study assesses the suitability of including tall Acacia shrublands (‘Pindan’) as a new eligible fuel type. These shrublands make up 12% (~2 million ha) of the Kimberley region, Western Australia, where, on average, 32% is fire affected annually, mostly in the LDS. A standard assessment protocol was applied to describe vegetation fuel type structural and pyrolysis characteristics. We show that Pindan (i) can be identified and mapped as a unique tall Acacia shrubland vegetation fuel type, (ii) characterised by a significantly greater shrubby fuel load biomass, and (iii) the conservation status of which would benefit from imposition of strategic prescribed burning programme. Savanna burning projects in the Pindan fuel type could potentially abate up to 24.43 t.CO₂‐e/km² per year, generating significant income and employment opportunities for predominantly Indigenous land managers in the region.     

基于1H-NMR及GC-MS的中国块菌及其共生云南松的代谢物分析

采用代谢组学技术研究中国块菌(云南黑松露)及其共生云南松的小分子活性代谢产物.运用核磁共振(1H-NMR)和气相质谱(GC-MS)两种技术,分析新鲜中国块菌成熟子实体及松根的代谢成分;将1H-NMR及GC-MS数据导入SMICA-P软件进行多元统计分析,比较二者的差异代谢物.在块菌子实体及松根中分别共检测到了苏氨酸、甘...