连云港市农业非点源污染对水环境的影响

通过2002年对连云港市农药化肥使用量以及水体中N、P等污染研究的结果显示：化肥的使用强度在381kg/hm^2，农药使用强度在8.12kg/hm^2；市区河流水体中N、P的含量严重超标，郊县河流的污染主要是N；水库污染相对较轻，近海海域的污染较为严重，地下水中，亚硝酸酸盐的含量超标较为严重。     

应用~(32)P-后标记技术对苯醌和氢醌处理人血淋巴细胞形成DNA加合物的研究

应用核酸酶Ｐ１促进的３２Ｐ－后标记技术对苯醌和氢醌处理人血淋巴细胞后形成的ＤＮＡ加合物进行了研究。结果表明，人血淋巴细胞被苯醌和氢醌处理２４ｈ之后，均形成了同一种ＤＮＡ加合物。两种化合物在不同浓度下处理人血淋巴细胞每１０７核苷酸中有０．０１～１０个核苷酸形成加合物。为了达到同等ＤＮＡ加合物水平，氢醌比苯醌需要更高的浓度。小牛胸腺ＤＮＡ与苯醌、氢醌反应可生成５种ＤＮＡ加合物。用苯醌或氢醌处理淋巴细胞所形成的加合物种类与上述纯ＤＮＡ与苯醌，氢醌形成的５种加合物在双向薄层层折图谱上完全不相符合。这些结果意味着苯醌、氢醌与ＤＮＡ的加合作用在细胞内存在着修饰机制。     

砷超富集植物的热解特征及其与砷含量的关系

不同热解气氛和升温速率的比较研究表明,在空气气氛条件和25℃·min-1的升温速率下,砷超富集植物的热解曲线特征明显且实验速度适中,因此,是适用于砷超富集植物的热解实验条件.在该实验条件下,不同含砷浓度的蜈蚣草(Pteris vittata L.)和大叶井口边草(P.cretica L.)的热解温度主要集中在200～500℃之间.与低砷蜈蚣草相比,高砷蜈蚣草在300℃附近热解减弱,而在450℃附近热解加剧,蜈蚣草体内的砷有促使其热解过程向高温方向偏移的趋势;而大叶井口边草体内的砷则促使其在300℃附近热分解程度加剧,而对450℃附近的热解程度影响不明显.     

Degradation of crude oil by indigenous microorganisms supplemented with nutrients

Different kinds of mineral nutrients(NO3-N, NH4-N and PO4-P) were applied in the simulated oil-polluted seawater for enhancing oil biodegradation in the N/P ratio 10:1 and 20: 1. Although indigenous microorganisms have the ability to degrade oil, adding nutrients accelerated biodegradation rates significantly. For the group amended with NO3-N and PO4-P in the ratio 10:1, the reaction rate coefficient was 4 times higher than the natural biodegradation. Chemical and microbiological analysis showed that the optimal N/P ratio in the system is 10: 1, and microorganisms tend to utilize nitrate rather than ammonium as N source.     

人工富集微生物技术对太湖梅梁湾水源地氮磷的去除研究

采用2种载体(PM和ACP)进行人工富集微生物的方法,来去除太湖梅梁湾水源地水中的氮磷污染物。通过研究不同的载体密度和水力停留时间对去除效率的影响,中试结果表明:当载体密度为13.1%,停留时间为7d,源水中ρ(TN)为2.95～6.41mg·L-1,ρ(NH4 -N)为0.49～3.31mg·L-1,ρ(NO2--N)为0.07～0.51mg·L-1,ρ(TP)为0.084￣0.25mg·L-1,ρ(PO4--P)为0.005～0.059mg·L-1的条件下,人工富集微生物技术对TN,NH4 -N,NO2--N,TP,PO4--P的平均去除率最高分别达到22.68%,57.08%,88.83%,45.36%,29.58%,可见利用人工富集微生物技术能有效去除水源地中的氮磷营养盐,对富营养化水源地水体的水质有明显的改善作用。     

Nutrient dynamics in shallow lakes of northern greece

GOAL, SCOPE, BACKGROUND: Shallow lakes display a number of features that set them apart from the more frequently studied deeper systems. The majority of lakes in Northern Greece are small to moderate in size with a relatively low depth and are considered as sites of high value of the wetland habitat. However, the water quality of these lakes has only been evaluated segmentally and occasionally. OBJECTIVE: The objectives of this study were to thoroughly investigate nitrogen and phosphorus speciation in lakes of a high ecological significance located in N. Greece, in order to evaluate their eutrophication status and possible nutrient limitation factors, and to investigate the main factors/sources that affect the water quality of these systems. METHODS: An extensive survey was carried out during the period from 1998-1999. Water samples were collected on a monthly basis from lakes Koronia, Volvi, Doirani, Mikri Prespa and Megali Prespa located in N. Greece. Water quality parameters (temperature, dissolved oxygen, pH and conductivity), organic indices (COD, BOD5), and N- and P-species (NO3(-), NO2(-), NH4(+), and PO4(3-), Kieldahl nitrogen and acid-hydrolysable phosphorus) were determined according to standard methods for surface water. Statistical treatment of the data was employed. RESULTS AND CONCLUSIONS: The physicochemical parameters determined in the lakes studied revealed a high temporal variation. The trophic state of the lakes ranged from meso- to hypertrophic. The nutrient limiting factor varied among lakes suggesting either P-limitation conditions or mixed conditions changing from P- to N-limitation throughout the year. Urban/industrial activities and agricultural runoff are the major factors affecting all lakes, although with a varying contribution. RECOMMENDATION AND OUTLOOK: This lake-specific research offers valuable information about water quality and nutrient dynamics in lakes of significant ecological value located in N. Greece that can be useful for an effective pollution control/management of these systems. Due to the large intra-annual variability of certain physicochemical parameters, a properly designed monitoring program of lake water is recommended.     

Bioassay zur Bestimmung von TCDD-Toxizit?ts?quivalenten (TEQ) von Umweltproben und Reststoffen

Zusammenfassung  Polychlorierte aromatische Kohlenwasserstoffe (PHAK), z.B. 2,3,7,8-Tetrachlordibenzo-p-dioxin (TCDD), weisen eine Vielzahl von toxischen Wirkungen und biologischen Effekten auf. Die Substanzklasse der PHAK besitzt die Eigenschaft der Bindung an ein cytosolisches Rezeptor-Protein, gefolgt von der Synthese bestimmter Genprodukte, u.a. von Cytochrom P450 1A1 (CYP 1A1). In dieser Arbeit wird ein Bioassay beschrieben, der erlaubt, die Induktion von CYP 1A1 als Summenparameter für die biologische Wirksamkeit der kritischen, halogenierten Verbindungen in komplexen Umweltmatrizes zu bestimmen. Zur Abtrennung von Substanzen aus den Extrakten von Umweltproben (z. B. Naturstoffe und polyzyklische aromatische Kohlenwasserstoffe), die den Bioassay st?ren k?nnen, wurde ein Ein-S?ulen-Clean-up entwickelt. Die biologisch ermittelten TEQ-Werte stimmen gut mit den Resultaten der chemischen Analytik überein. Der Bioassay in Kombination mit dem Clean-up bietet eine zeitsparende und kostengünstige M?glichkeit zur Untersuchung von Umweltproben.      

Phosphorus Losses to Water from Lowland Rice Fields under Rice–Wheat Double Cropping System in the Tai Lake Region

To assess P losses to surface water by runoff during the rice season and by drainage flow during the winter wheat season, serial field trials were conducted in different types of paddy soils in the Tai Lake Region (TLR) during 2000 and 2001. Four P application rates were set as 0 (CK), 30, 150, and 300 kg P/hm² for flooded rice trials and 0 (CK), 20, 80, 160 kg P/hm² for winter wheat trials respectively. Field experiments were done in two locations with a plot size of 30 m² and four replications in a randomized complete block design. A simplified lysimeter was installed for each plot to collect all the runoff or drainage flow from each event. Total P (TP) losses to surface water during rice season by runoff flow from four treatments were 150 (CK), 220 (T30), 395 (T150), 670 (T300) g P/hm² in year 2000, and 298, 440, 1828, 3744 g P/hm² in year 2001 respectively in Wuxi station, here the soil is permeable paddy soil derived from loam clay deposit. While the losses were 102, 140, 210, 270 in year 2000, and 128, 165, 359, 589 g P/hm² in year 2001 respectively in Changshu station, here the soil is waterlogged paddy soil derived from silt loam deposit. During the winter wheat season, total P lost from the fields by drainage flow in the four treatments were 253 (CK), 382 (T20), 580 (T89), 818 (T160) g P/hm² in year 2000–2001, and 573.3, 709.4, 1123.2, 1552.4 g P/hm² in year 2001–2002 at the Wuxi station. While these were 395.6, 539.1, 1356.8, 1972.1 g P/hm² in year 2000–2001, and 811.5, 1184.6, 3001.2, 5333.1 g P/hm² in year 2001–2002 at the Changshu station. Results revealed that P fertilizer application rates significantly affected the TP concentrations and TP loads in runoff during the rice season, and by drainage flow during the winter wheat season. Both TP loads were significantly increased as the P application rate increases. The data indicate that TP losses to surface water were much higher during the winter wheat season than during the rice season in two tested sites. The data also reveal that the annual precipitation and evaporation rate affected the soil P losses to surface water significantly. Year 2000 was relatively dried with higher evaporation thus P losses to water by both runoff and drainage flow were less than in year 2001 which was a relatively wet year with lower evaporation. Results indicate that texture, structure of the soil profile, and field construction (with or without ridge and deep drains) affected soil P losses to surface water dramatically. Annual possible TP lost to water at the application rate of 50 kg P/hm² year tested in TLR were estimated from 97 to 185 tones P from permeable paddy soils and 109–218 tones P from waterlogged paddy soils. There was no significant difference of TP lost between the CK and the T50 treatments in both stations, which indicate that there is no more TP lost in field of normal P fertilizer application rate than in control field of no P fertilized. Much higher TP lost in runoff or drainage flow from those other P application rates treatments than from the T50 treatment, which suggest that P losses to surface water would be greatly increasing in the time when higher available P accumulation in plough layer soil in this region.     

Effect of N and P addition on soil organic C potential mineralization in forest soils in South China

Atmospheric nitrogen deposition is at a high level in some forests of South China. The effects of addition of exogenous N and P on soil organic carbon mineralization were studied to address: (1) if the atmospheric N deposition promotes soil C storage through decreasing mineralization; (2) if the soil available P is a limitation to organic carbon mineralization. Soils (0-10 cm) was sampled from monsoon evergreen broad-leaved forest (MEBF), coniferous and broad-leaved mixed forest (CBMF), and Pinus massoniana...