入侵植物加拿大一枝黄花综合管理技术的研究进展

加拿大一枝黄花的入侵已经成为不容忽视的问题,产生了无法估量的经济、社会、生态损失。由于加拿大一枝黄花繁殖能力强、传播迅速、生境多样,因此该种的控制难度也大。文章综述了有关加拿大一枝黄花物理防治、化除、生物防治、植物替代等方法及其应用效果,以期为更有效地实施拿大一枝黄花的综合管理提供理论基础和实践依据。     

硬叶空气凤梨对铅的富集特征研究

空气凤梨是一类生长在空气中、不需要土壤的特殊植物,是有效的监测环境变化的指示植物。文章以硬叶空凤为材料,以环境中最典型的污染物—铅对其进行胁迫处理后,发现硬叶空凤对铅具有很强的耐性,而且可对铅进行有效的富集,是一种合适的指示铅污染的植物。扫描电镜和能谱分析表明,不论何种铅浓度处理植物体,硬叶空凤叶表鳞片中都可检测到铅元素的存在,进一步表明叶表鳞片很可能是铅等重金属元素的主要富集结构。另外,硬叶空凤叶表鳞片的3类细胞在富集铅时所起的作用是不同的,最内部的碟状细胞中铅的含量要大于中间的环状细胞,更大于最外部的翼状细胞,暗示铅的迁移是一种代谢性主动吸收过程。     

三岔河沿岸植物铅、镉富集特性的研究

以紫茎泽兰（EupatoriumadenophorumSpreng）、青蒿（HerbaArtemisiaeAnnuae）、三叶鬼针草（Bidenspilosa）、野牡丹（MelastomaAfffine D．Don）、光叶蕨（Knuiwatsukiacuspidata）为例,分别在河边、路边、山上和污水灌溉的旱地4个采样点采取5种植物的根部和茎叶,测量重金属元素Pb、Cd的含量、富集系数和转移系数并分析数据。结果表明,各种植物不同器官在不同环境中对重金属元素Pb、Cd的富集和转移水平各不相同,就平均水平来说三叶鬼针草对重金属Pb、Cd的富集系数较大,转移系数也高,但其对Pb的转移量明显高于Cd的转移量;紫茎泽兰对重金属元素Cd的富集和转移速度相对高于其它4种植物,说明紫茎泽兰对Cd的吸收和转移比较快,可作为受镉污染土壤进行改良的备选植物种。     

海岸带含水层咸淡水界面随潮汐波动的数值模拟

在分析、研究了滨海地带含水层和不透水层的水文地质特性及含水层内的咸淡水渗流运动特征的基础上,运用数学推理的手法,建立了一种较为简单适用的模拟海岸带含水层咸淡水界面和天然地下水面变动规律的二维数学模型,通过该模型的计算值与实验值的比较,证明该模型的计算结果与实验结果有着非常好的拟合度,即该模型能较客观地揭示海水入侵引起的咸淡水界面的变化规律.其后,运用该模型系统的探讨了含水层以下为非平坦的不透水层的滨海地带天然地下水面、咸淡水界面伴随着潮汐的波动而变化的规律.即伴随着潮汐的波动,一方面天然地下水面和咸淡水界面与潮汐具有相似的振动波形,波动的幅度随离海岸距离的增加而减小.在海岸附近咸淡水界面的振幅大于天然地下水面的振幅,而在离开海岸一定距离后天然地下水面的振幅超过咸淡水界面的振幅.总体上天然地下水面的振幅呈负指数衰减,而咸淡水界面的振幅几乎呈直线衰减(其衰减直线的倾角在135～150 °之间变动),且潮汐波动对天然地下水面影响的范围远大于其对咸淡水界面的影响;另一方面天然地下水面和咸淡水界面波动的振幅及它们之间的相位差的大小还与天然地下水面的水力坡度、含水层的渗透系数、有效孔隙率、不透水层形状及其变动的幅度有关,但它们之间的相位差的大小与潮汐波动的幅度无关,其振幅与潮汐的振幅成比例增减.当不透水层的形状一定时,不论天然地下水面的水力坡度、含水层的渗透系数、有效孔隙率及潮汐波动的幅度怎么变动,天然地下水面、咸淡水界面振动的相位差的变化趋势及其峰值出现的位置几乎不变,即不透水层的形状决定着天然地下水面、咸淡水界面振动的相位差的变化趋势,而其大小与含水层的水文地质参数(水力坡度、渗透系数及有效孔隙率)密切相关.此外,当天然地下水面和咸淡水界面的振动存在相位和振幅的较大差异时,可以断定含水层以下存在非平坦的不透水层,且这种差异越大,不透水层凸凹不平的程度越高.     

强化供氧条件下潜流型人工湿地运行特性

针对潜流型人工湿地中溶解氧浓度和脱氮率偏低的问题,试验研究了强化供氧对植物和微生物的影响及人工湿地内溶解氧浓度、净化效率的变化规律.结果表明,强化供氧宜在湿地前端进行,最佳气水比为6左右,可采用连续供氧方式.供氧对湿地植物生理特性无明显不良影响,可显著增加湿地中硝化菌、反硝化菌数量,硝化菌可比供氧前高出1～2个数量级,反硝化菌高出1个数量级.强化供氧有效改善了湿地内氧环境,供氧前湿地内溶氧浓度普遍低于0.6 mg/L,供氧后氧浓度上升至1 mg/L以上.强化供氧有利于各类污染物质尤其是有机物和氮类物质的去除,有机物去除率比原湿地高出10％左右, TN去除率能够达到60％以上.因此,强化充氧措施具有较好的研究和应用价值.     

Residual dynamics of thiacloprid in medical herbs marjoram, thyme, and camomile and in soil

Thiacloprid is a new insecticide of the chloronicotinyl family. To assess its risk after application, residual characteristics of thiacloprid in marjoram, thyme, and camomile and in soil were studied under field conditions. The active ingredient was extracted from the plant material using a mixture of acetone-water. After filtration, the extract was concentrated to the aqueous phase, diluted with water, and portioned against ethyl acetate on a matrix solid phase dispersion column. Thiacloprid was extracted from soil using a mixture of methanol-water, filtered, and re.extracted （clean up） with dichloromethane. The residues were quantified using HPLC-MS-MS. The methods were validated by recovery experiments. Thiacloprid residues in marjoram, thyme, and camomile and in soil persisted beyond 10, 14, 14, and 21 d but no residues were detected after 14, 21, 21, and 28 d, respectively. The data obtained in this study indicated that the biexponential model is more suitable than the first-order function to describe the decline of thiacloprid in fresh marjoram, fresh thyme, and dried camomile flowers with half-life （t1/2） of 1.1, 0.7, and 1.2 d, respectively. However, both the first-order function and biexponential model were found to be applicable for dissipation of thiacloprid in soil with almost the same t1/2 values of 3.5 and 3.6 d. The results indicated that thiacloprid dissipates rapidly and does not accumulate in the tested herbs and in soil.     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.     

地下水环境安全不容忽视

地下水是水资源的重要组成部分,由于水量稳定、水质好,一直是人类的重要水源之一。进入工业社会,随着人口的增长、工农业的发展和科技的进步,对于水资源的需求不断增加,地下水的开采量和开采深度也进一步加大,洁净而丰富的地下水资源为农业灌溉、工矿生产和城市生活源源不断地注入着活力。数据显示,目前我国地下     

日本森林大气中过氧化物的浓度及其对森林植物的影响

为了研究森林衰退的原因,于2000,2001和2002年的8月,分别选择出现森林衰退的日本奥日光白根山落叶树森林和未出现森林衰退的长野县大芝高原红松森林设立监测点,对光化学氧化剂臭氧(O3)和过氧化物的浓度进行监测,同时利用人工气候室对森林植物山毛榉和白桦进行了50′10-9O3、100′10-9O3和50′10-9O3+2′10-9~3′10-9过氧化物(过氧化氢(H2O2)及甲基过氧化氢(MHP))的暴露实验.野外监测结果表明,监测期间奥日光和长野的O3平均浓度相同,奥日光的H2O2及MHP平均浓度均高于长野;大气中的H2O2和MHP总是与O3共存,并且其浓度随O3浓度的增加而增加.暴露实验结果表明,暴露于50′10-9O3+2′10-9~3′10-9过氧化物的山毛榉和白桦出现了不同于O3暴露的叶片伤害症状;与100′10-9O3相比,50′10-9O3+2′10-9~3′10-9过氧化物导致植物出现了严重的叶片伤害和显著的光合速率下降.研究结果表明,除O3外,大气中的过氧化物也是导致森林衰退的原因之一.     

Nitrogen cycle of a typical Suaeda salsa marsh ecosystem in the Yellow River estuary

The nitrogen (N) biological cycle of the Suaeda salsa marsh ecosystem in the Yellow River estuary was studied during 2008 to 2009. Results showed that soil N had significant seasonal fluctuations and vertical distribution. The N/P ratio (15.73±1.77) of S. salsa was less than 16, indicating that plant growth was limited by both N and P. The N absorption coefficient of S. salsa was very low (0.007), while the N utilization and cycle coefficients were high (0.824 and 0.331, respectively). The N turnover among compartments of S. salsa marsh showed that N uptake from aboveground parts and roots were 2.539 and 0.622 g/m2, respectively. The N translocation from aboveground parts to roots and from roots to soil were 2.042 and 0.076 g/m2, respectively. The N translocation from aboveground living bodies to litter was 0.497 g/m2, the annual N return from litter to soil was far less than 0.368 g/m2, and the net N mineralization in topsoil during the growing season was 0.033 g/m2. N was an important limiting factor in S. salsa marsh, and the ecosystem was classified as unstable and vulnerable. S. salsa was seemingly well adapted to the low-nutrient status and vulnerable habitat, and the nutrient enrichment due to N import from the Yellow River estuary would be a potential threat to the S. salsa marsh. Excessive nutrient loading might favor invasive species and induce severe long-term degradation of the ecosystem if human intervention measures were not taken. The N quantitative relationships determined in our study might provide a scientific basis for the establishment of effective measures.