荒漠草原沙漠化植物群落及土壤物理变化

沙漠化是草地退化最严重的形式之一。以空间代替时间的方法,通过对宁夏中北部荒漠草原沙漠化过程中植物群落特征和土壤物理特性的研究,探讨草地植物群落与土壤物理特性对沙漠化的响应机制。结果表明:(1)潜在沙漠化阶段草地以牛枝子、猪毛蒿、中亚白草为优势种,轻度沙漠化阶段草地以中亚白草、苦豆子为优势种,中度沙漠化阶段草地以狗尾草、虫实为优势种,重度沙漠化阶段草地以沙米、赖草、狗尾草为优势种,极度沙漠化阶段草地以沙米为优势种。(2)随着沙漠化程度的加剧草地植物群落生物量、Shannon-Wiener指数、丰富度指数、盖度均呈降低趋势,但轻度沙漠化阶段草地植被生物量比潜在沙漠化增加了23%。(3)草地沙漠化导致土壤容重和土壤粗砂粒含量增加,而土壤水分,土壤细砂粒和粘粉粒含量降低。荒漠草原沙漠化导致了土壤环境和植被明显退化,草地生产力明显降低。     

间作缓解蚕豆连作障碍的根际微生态效应

通过田间小区试验,研究了3个品种蚕豆(92-24、云豆324、凤豆6号)与小麦间作对蚕豆产量、枯萎病病情指数、根际镰刀菌数量、根际真菌代谢功能多样性和土壤酶活性的影响。结果表明:与单作蚕豆相比,云豆324与小麦间作(YD324/W)和凤豆6号与小麦间作(FD6/W)处理均显著提高了蚕豆地上部干重、籽粒产量和百粒重。YD324/W和FD6/W处理使蚕豆枯萎病发病初期病情指数分别降低57.14%和41.67%,镰刀菌数量分别降低32.06%和29.88%,而92-24与小麦间作(92-24/W)处理蚕豆产量、枯萎病病情指数和镰刀菌数量与单作蚕豆均无显著差异。YD324/W和FD6/W处理显著提高了蚕豆根际真菌的多样性指数和丰富度指数,并使蚕豆根际真菌的AWCD值分别比单作蚕豆提高了61.75%和46.49%;YD324/W和FD6/W处理明显改变了蚕豆根际真菌的群落结构。而92-24/W处理对蚕豆根际真菌的多样性指数、丰富度指数和AWCD值均无显著影响,也未明显改变真菌的群落结构。不同发病时期,YD324/W和FD6/W处理均显著提高了蚕豆根际土壤的蔗糖酶、脲酶和过氧化氢酶活性;而92-24/W处理蚕豆根际蔗糖酶、脲酶和过氧化氢酶活性与单作蚕豆均无显著差异。总之,小麦与不同品种蚕豆间作改变了蚕豆根际的真菌群落结构,提高了蚕豆根际真菌的活性、多样性和丰富度,提高土壤酶活性并改善蚕豆生长,增加了蚕豆产量。表明小麦与蚕豆间作改善了根际土壤的微生态环境,降低了镰刀菌的数量,缓解了蚕豆连作障碍,但蚕豆品种的差异影响间作控病效果。     

外源氮素添加对森林土壤氨基糖转化的影响

采用室内模拟培养法研究了不同数量氮素添加条件下森林土壤中3种微生物来源的氨基糖含量的动态变化,并且利用氨基葡萄糖和胞壁酸的比值分析了氮素添加条件下土壤真菌和细菌对土壤氮素转化和积累的相对贡献。结果表明:土壤中氨基糖含量的动态变化与土壤中的养分状况密切相关;当向土壤中添加氮源时,微生物会利用外加氮源合成自身的细胞壁物质,并且高氮处理胞壁酸含量高于低氮处理,而高氮处理氨基葡萄糖含量则低于低氮处理,说明随施氮量的增加更有利于以胞壁酸为代表的细菌残留物在土壤中的积累,不利于以氨基葡萄糖为代表的真菌残留物的积累,氨基半乳糖对氮素添加的响应较小;当土壤中养分缺乏时,氨基糖能够发生不同程度的分解;添加氮源条件下,真菌和细菌来源氨基糖的比值发生变化,细菌对土壤氮素转化的贡献大于真菌,并且高氮处理细菌的贡献更大。本研究表明,氮素添加改变了以氨基糖为代表的土壤氮素的微生物转化过程。     

尾巨桉液流特征分析

目前尾巨桉( Eucalyptus urophylla × E. grandis)在南部大面积种植,尤其是在广西,其水分利用效率对森林可持续发展和水资源管理的影响越来越受到关注,因此了解其水分利用特征具有一定的意义。该文通过Granier热扩散探针法(TDP)对广西黄冕国有林场4~5年生尾巨桉人工林液流密度(SFD)的年变化规律、不同个体变化及其与环境因子的关系进行了研究。结果表明：尾巨桉年平均日液流密度为830.1 L.m-2.d-1;从尾巨桉日液流密度的年变化来看,最大值不超过2000 L.m-2.d-1,与相似研究比较,该研究得到的结果偏低。不同直径尾巨桉SFD具有相似的变化趋势,胸径相近其液流密度也大致相同,但胸径相差很大时,其液流密度相差也大,相差最大可达1300 L.m-2.d-1,这主要与不同生长状况的植物根系从土壤吸收水分能力不同有关。相关研究表明光合有效辐射和水汽压亏缺是树木冠层蒸腾的主要动力,该研究也发现树干液流密度与水汽压亏缺( VPD)、光合有效辐射( PAR)在年变化上有很好的同步性,主要表现出夏秋季节较高、春冬季节较低的现象。 SFD与PAR的关系比较显著,与VPD、空气温度( AT)、土壤温度( ST)有一定的关系,但与空气相对湿度( RH)和土壤湿度( SM)没有呈现规律。环境因子和植物生物学特征是树干液流密度主要的影响因素,进一步探讨尾巨桉如何响应这些因子的变化显得尤为重要。     

Remodeling of apolipoprotein E-containing spherical reconstituted high density lipoproteins by phospholipid transfer protein

Phospholipid transfer protein (PLTP) transfers phospholipids between HDL and other lipoproteins in plasma. It also remodels spherical, apolipoprotein A-I (apoA-I)-containing HDL into large and small particles in a process involving the dissociation of lipid-free/lipid-poor apoA-I. ApoE is another apolipoprotein that is mostly associated with large, spherical HDL that do not contain apoA-I. Three isoforms of apoE have been identified in human plasma: apoE2, apoE3, and apoE4. This study investigates the remodeling of spherical apoE-containing HDL by PLTP and the ability of PLTP to transfer phospholipids between apoE-containing HDL and phospholipid vesicles. Spherical reconstituted high density lipoproteins (rHDL) containing apoA-I [(A-I)rHDL], apoE2 [(E2)rHDL], apoE3 [(E3)rHDL], or apoE4 [(E4)rHDL] as the sole apolipoprotein were prepared by incubating discoidal rHDL with low density lipoproteins and lecithin:cholesterol acyltransferase. PLTP remodeled the spherical, apoE-containing rHDL into large and small particles without the dissociation of apoE. The PLTP-mediated remodeling of apoE-containing rHDL was more extensive than that of (A-I)rHDL. PLTP transferred phospholipids from small unilamellar vesicles to apoE-containing rHDL in an isoform-dependent manner, but at a rate slower than that for spherical (A-I)rHDL. It is concluded that apoE enhances the capacity of PLTP to remodel HDL but reduces the ability of HDL to participate in PLTP-mediated phospholipid transfers.     

Characterization and properties of pre beta-HDL particles formed by ABCA1-mediated cellular lipid efflux to apoA-I

The contribution of ABCA1-mediated efflux of cellular phospholipid (PL) and cholesterol to human apolipoprotein A-I (apoA-I) to the formation of pre beta 1-HDL (or lipid-poor apoA-I) is not well defined. To explore this issue, we characterized the nascent HDL particles formed when lipid-free apoA-I was incubated with fibroblasts in which expression of the ABCA1 was upregulated. After a 2 h incubation, the extracellular medium contained small apoA-I/PL particles (pre beta 1-HDL; diameter = 7.5 +/- 0.4 nm). The pre beta 1-HDL (or lipid-poor apoA-I) particles contained a single apoA-I molecule and three to four PL molecules and one to two cholesterol molecules. An apoA-I variant lacking the C-terminal alpha-helix did not form such particles when incubated with the cell, indicating that this helix is critical for the formation of lipid-poor apoA-I particles. These pre beta 1-HDL particles were as effective as lipid-free apoA-I molecules in mediating both the efflux of cellular lipids via ABCA1 and the formation of larger, discoidal HDL particles. In conclusion, pre beta 1-HDL is both a product and a substrate in the ABCA1-mediated reaction to efflux cellular PL and cholesterol to apoA-I. A monomeric apoA-I molecule associated with three to four PL molecules (i.e., lipid-poor apoA-I) has similar properties to the lipid-free apoA-I molecule.     

绝经后女性CYP19基因Val80及OPG基因A163G多态性与骨密度的相关性研究

探讨细胞色素P450 19 (CYP19) 基因Val80多态性及护骨素(OPG) 基因A163G多态性与绝经后女性骨密度 (BMD) 的关系。随机选择居住在重庆的绝经后女性200例, 采用多聚酶链反应-限制性片段长度多态性法检测Val80及A163G多态性, 采用Norland公司XR-46系列双能X线骨密度仪测量股骨近端及腰椎BMD。 200名绝经后女性中Val80基因型GG、GA及AA的频率分别为19.5％、44.5％及36.0％; A163G基因型GG、GC 及CC的频率分别为: 13.0％, 42.0％及45.0％; 基因型频率分布均符合Hardy-Weinberg平衡 (P＞0.05)。协方差分析及多元逐步回归分析显示CYP19基因第3外显子Val80多态性与绝经后女性BMD无相关性 (P＞0.05)。除大转子外, A163G位点AG/GG/AG+GG基因型者股骨颈、Ward’s三角及腰椎BMD均较AA基因型者低, A163G基因型与股骨颈、Ward’s三角及腰椎BMD有相关性 (P＜0.05)。OPG基因启动子区A163G多态性分布存在明显的种族差异, 且与绝经后女性BMD有一定关联, AA型对BMD具有一定的保护作用, G等位基因是BMD降低的危险因素。     

土壤复合污染的联合修复技术研究进展

复合污染是土壤污染的主要存在形式,其中重金属、有机污染物等是主要的污染源。例如,共存于土壤中铅和镉会发生交互作用,从而增强了镉的迁移能力。此前单一的物理、化学、生物等修复手段对复合污染的修复效果并不明显。联合修复技术的使用可以在一定程度上克服使用单一的修复手段存在的缺点,提高修复效率、降低修复成本。最近有研究表明,综合利用化学氧化和超声波方法可以在很短的时间内将土壤中的甲苯和二甲苯完全氧化为CO和CO2。介绍了综合利用物理、化学、生物等方法对土壤复合污染修复的进展,并对研究中需要注意的问题及未来的发展趋势说明。     

The response of an Eastern Amazonian rain forest to drought stress: results and modelling analyses from a throughfall exclusion experiment

Warmer and drier climates over Eastern Amazonia have been predicted as a component of climate change during the next 50–100 years. It remains unclear what effect such changes will have on forest–atmosphere exchange of carbon dioxide (CO₂) and water, but the cumulative effect is anticipated to produce climatic feedback at both regional and global scales. To allow more detailed study of forest responses to soil drying, a simulated soil drought or 'throughfall exclusion' (TFE) experiment was established at a rain forest site in Eastern Amazonia, Brazil, for which time-series sap flow and soil moisture data were obtained. The experiment excluded 50% of the throughfall from the soil. Sap flow data from the forest plot experiencing normal rainfall showed no limitation of transpiration throughout the two monitored dry seasons. Conversely, data from the TFE showed large dry season declines in transpiration, with tree water use restricted to 20% of that in the control plot at the peak of both dry seasons. The results were examined to evaluate the paradigm that the restriction on transpiration in the dry season was caused by limitation of soil-to-root water transport, driven by low soil water potential and high soil-to-root hydraulic resistance. This paradigm, embedded in the soil–plant–atmosphere (SPA) model and driven using on-site measurements, provided a good explanation ( R ² > 0.69) of the magnitude and timing of changes in sap flow and soil moisture. This model-data correspondence represents a substantial improvement compared with other ecosystem models of drought stress tested in Amazonia. Inclusion of deeper rooting should lead to lower sensitivity to drought than the majority of existing models. Modelled annual GPP declined by 13–14% in response to the treatment, compared with estimated declines in transpiration of 30–40%.