阿循拉津在土壤中的降解途径及其对持留性的影响

通过田间和实验室试验，研究了作草剂阿特拉津在土壤中的降解代谢规律及其与土壤特性的关系。试验表明，阿特拉津施用后，在作物生长期内可降解９０％以上，土壤酸碱度对阿特拉津在土壤中的代谢有显著影响。在碱性土 阿特拉津主要经过微生物代谢而被降解；在酸性土壤中化学水解占地位。     

阿特拉津在土壤中的生物降解研究

运用恒温培养法研究了阿特拉津在河北省白洋淀地区农田土壤中的生物降解动力学，并从中分离鉴定了土壤中降解阿特拉津的优势菌种，研究结果表明，该土壤对阿特拉津具有一定的降解能力，非生物＋生物的降解、非生物降解和生物降解的速率分别为０．０２６２ｄ＾－１，０．００５５４８ｄ＾－１和０．００８１９４ｄ＾－１，半衰期分别为２６ｄ，１２５ｄ和８５ｄ，发现土壤中降解阿特拉津的优势菌种为蜡状芽孢杆菌（Ｂａｃｉｌｌｕｓ     

皇竹草对土壤阿特拉津的降解特性

为了探明种植皇竹草(Pennisetum hydridum)对土壤阿特拉津降解的促进作用,通过盆栽试验研究了皇竹草对土壤阿特拉津的降解动态、转移特征以及土壤阿特拉津残留浓度与土壤相关酶活性的关系。结果表明:与未种植皇竹草相比,种植皇竹草土壤阿特拉津降解率明显提高,皇竹草对未灭菌和灭菌土壤阿特拉津的降解率分别提高52.84和42.38百分点;与未种植皇竹草处理相比,灭菌和未灭菌条件下种植皇竹草处理阿特拉津在土壤中的半衰期可分别缩短64.35和53.21 d;土壤中阿特拉津被皇竹草吸收后逐步由地下部分向地上部分转移,随着培养时间的延长,转移系数变大;土壤中阿特拉津残留浓度与土壤过氧化氢酶、过氧化物酶、转化酶和多酚氧化酶活性呈显著负相关(P0.05或P0.01)。认为种植皇竹草有助于阿特拉津的降解。     

皇竹草对土壤阿特拉津的修复作用

通过盆栽试验探讨了种植皇竹草（Pennisetum hydridum）对阿特拉津污染土壤的修复效果,阿特拉津对皇竹草生长的影响,以及皇竹草对土壤微生物数量的影响,以期为阿特拉津污染土壤的植物修复提供参考。结果表明：在≤200 mg.kg-1质量分数范围以内,种植皇竹草对土壤阿特拉津的初期降解效率比对照明显提高,最大提高了29.64%,达到显著或极显著差异;阿特拉津质量分数在≤200 mg.kg-1范围内对皇竹草株高没有影响,≤50 mg.kg-1质量分数范围内对生物量没有影响,根冠比变化不明显;随阿特拉津质量分数的增加皇竹草根际和非根际土壤中的细菌、真菌、放线菌数量均呈先增加后减少的趋势,在质量分数为100 mg.kg-1时达到最大,根际土壤中细菌和放线菌数量明显高于非根际土壤,真菌数量在根际与非根际土壤中变化不明显。说明种植皇竹草有助于阿特拉津降解效率的提高,且与种植皇竹草后改变了土壤微生物数量及皇竹草的生长状况有关。     

除草剂阿特拉津的环境毒理研究进展

叙述了阿特拉津的应用概况及其在生产实践中所存在问题;阿特拉津在生物体内和环境中的降解代谢过程。综述了近年来国内外在阿特拉津的残留分析方法、环境毒理学和微生物降解等方面的研究进展。     

接种降解菌对土壤中邻苯二甲酸二异辛酯降解的影响

邻苯二甲酸二异辛酯〔Di-(2-Ethylhexyl)phthalate,DEHP〕是农田土壤中常被检出的有毒有机污染物,在土壤中有较长的持留性,微生物降解是其从土壤中消失的主要途径.本文采用温室盆栽试验研究了接种两株从污水处理厂活性污泥中分离得到的高效DEHP降解菌及其混合菌悬液降解土壤中DEHP污染的效果,以及土壤中添加葡萄糖和种植作物对其降解效率的影响.结果表明,在土壤初始DEHP浓度为100mg kg-1的条件下,接种两种降解菌及其混合菌悬液都可显著提高土壤中DEHP消失的速率,其残留半衰期比不接种对照缩短了32~48d,但在相同条件下接种不同降解菌的处理之间没有显著差异.土壤中添加0.6%的葡萄糖虽然可以强烈地促进土壤微生物的整体活性,但并没有提高修复效率,反而在短期内延缓了降解菌对DEHP的降解,延长了DEHP在土壤中持留的半衰期;植物生长可显著提高降解菌的降解效率,降低土壤中DEHP的残留浓度.研究结果同时也表明,只添加葡萄糖或只种植植物对土壤中DEHP的降解并没有显著的影响.图3表4参14     

毒死蜱农药环境行为研究

研究了毒死蜱农药在环境中的水解、土壤吸附和土壤消解行为。实验结果表明，毒死蜱在水体中降解较慢，半衰期为 ２５．６ ｄ；土壤具有较强的吸持毒死蜱农药的能力；该农药在土壤中的消解也较慢。     

常州市郊大通河部分河段底泥中氯苯类化合的含量高的原因探讨及治理对策

氯苯类化合物在环境中不易非生物降解，其在环境中的持留性主要决定于微生物降解与否及速率如何，本文用江苏常州大通河灌区土壤实验了这类化合物在厌氧条件的渍水土壤以及好氧条件的湿润土壤中的微生物降解，在此基础上探讨了大通河部分河段底泥中氯苯类化合物含量高的原因，并提出了相应的治理对策。     

碳纳米管吸附阿特拉津对其生物可利用性的影响

采用批量实验研究阿特拉津在3种多壁碳纳米管(MWNT、MWNT-COOH、MWNT-OH)上的吸附解吸行为,并对吸附态阿特拉津生物可利用性进行研究.研究结果表明,3种碳管对阿特拉津的吸附能力依次为:MWNT-COOH>MWNT-OH>MWNT,比表面积是决定吸附的主要因素,含氧官能团也是影响吸附的重要因素之一.阿特拉津可从3种碳管上完全解吸,无解吸滞后现象.体系中99.5%以上的阿特拉津能够被微生物(高效降解菌AD2)利用,但也存在微量残余且阿特拉津在MWNT上的微量残留最大,这与其孔隙吸附机制有关.碳管的存在影响微生物对阿特拉津的脱氯降解,脱氯产物仅达到54.26%—82.49%;具有高含量含氧官能团的MWNT-OH影响尤为显著,可能机制是碳管对微生物降解性能及中间产物的影响使得降解彻底性降低.     

Arthrobacter sp.AD30和Pseudomonas sp.AD39在阿特拉津工业废水生物处理及污染土壤生物修复中的应用

将分类地位和降解特性不同的两个高效降解除草剂阿特拉津的菌株Arthrobacter sp.AD30和Pseudo-monas sp.AD39,用于阿特拉津工业废水的生物处理和污染土壤的生物修复试验.填充聚氨酯泡沫的小型生物反应器阿特拉津降解实验表明,在进水的CODCr为1702 mg·1-1、阿特拉津浓度为133 mg·1-1和水力停留时间(HRT)为24 h的条件下,出水的CODCr稳定在100 mg·1-1以下,阿特拉津浓度在0.2 mg·1-1以下,均达到国家工业水污染物排放标准(GB 21523-2008).土壤的生物修复实验表明,含有200 mg·kg-1阿特拉津的土壤接种上述两个菌株,在30℃处理20 d以后,土壤中99.1%的阿特拉津被去除.这些结果表明,由AD30和AD39组成的混合菌株在工业废水的生物处理和污染土壤的生物修复中具有很好的应用潜力.     

Environmental fate of pesticides used in Australian viticulture V. Behaviour of atrazine in the soils of the south Australian Riverland

The transport of the s‐triazine herbicide, atrazine, through the red, calcareous earth soils of the South Australian Riverland was investigated. Small, undisturbed soil cores were extracted from the inter‐row topsoil of a vineyard adjacent to the River Murray, approximately 10 km south‐west of Overland Corner, South Australia. The vines were grown in a deep (1–4 m) reddish brown, strongly alkaline, sandy loam with a low organic carbon content (<2%). Atrazine concentrations in the leachate were dependent on application rate and soil type. High application rates on subsoil gave high rates of leaching for a longer time compared to the same application rate on topsoil and/or lower application rates on either topsoil or subsoil. Overall, 37–65% of the applied atrazine was detected in the leachate from subsoil cores, 14–25% in topsoil core leachates. Small amounts of atrazine (< 10% of applied dose) were found only in the top 2 cm of the core profiles. The results suggest that this herbicide is somewhat mobile in such strongly alkaline, sandy loam soils and that the irrigated soils of this region are likely to be prone to leaching of atrazine, and therefore that groundwater supplies in this area may be at risk of contamination through use of triazine herbicides.     

Study of atrazine degradation in soil from Kenyan sugarcane-cultivated fields in controlled laboratory conditions

A study to compare the extent of atrazine mineralization in soils from Kenyan sugarcane-cultivated fields with and without history of atrazine use was carried out in the laboratory under controlled conditions. The study was testing the hypothesis that repeated atrazine application to soil will not result in enhanced atrazine mineralization. The study was carried out with ¹⁴C-uniformly ring-labeled atrazine in a laboratory under controlled conditions. Atrazine mineralization to ¹⁴CO₂ in soil with no history of atrazine use was negligible (0.16%) after 163 days of soil incubation. The three metabolites hydroxyatrazine, desisopropylatrazine, and desethylatrazine in the proportion of 17.7%, 1.3%, and 2.6%, respectively, were in the soil after 75 days. In the soil from the sugarcane-cultivated field with history of atrazine use, atrazine mineralization was 89.9% after 98 days. The same soil, amended with mature compost, showed a lag phase of eight days before rapid atrazine mineralization was observed.     

Extractable atrazine and its metabolites in agricultural soils from the temperate humid zone

Extractable atrazine and its metabolites (hydroxyatrazine, deethylatrazine and deisopropylatrazine) were evaluated in agricultural soils from the temperate humid zone (Galicia, NW Spain) under laboratory conditions. The experiment was performed with five soils with different properties (organic C, soil texture and atrazine application history), both unamended and treated with atrazine at field application rate. Measurements of the atrazine compounds were made at different time intervals (1, 3, 6, 9 and 12 weeks) during a 3-month incubation period. Results showed that only hydroxyatrazine was detected in the extractable fraction of the unamended soils, with values remaining relatively constant throughout the incubation period. Atrazine addition notably increased the concentration of the parent compound and its degradation products; deisopropylatrazine and hydroxyatrazine were the main metabolites detected in the extractable fraction of the treated soils, whereas deethylatrazine was not detected. After 7 days incubation, values of total extractable residues, expressed as percentage of initially added atrazine, ranged from 75 to 86% (25–68% of atrazine, 7–11% of hydroxyatrazine and 9–57% of deisopropylatrazine). The values decreased rapidly during the first 3 weeks of incubation, showing values of 2–8% in soils with higher atrazine application and from 28 to 30% in soils with lower application history. At the end of the incubation, 2–8% of total extractable residues were still detected (0–4% of atrazine, 2–3% of hydroxyatrazine and 0–2% of deisopropylatrazine), indicating a residual effect of atrazine addition. These variations in the extractable fraction indicated that most added atrazine was rapidly degraded, especially in soils with higher application history.     

哒嗪硫磷水解与土壤降解研究

采用室内模拟方法,研究了哒嗪硫磷在东北黑土、江西红壤和南京黄棕壤3种不同类型土壤中的降解特性及pH、温度和表面活性剂（SDS）浓度对水解的影响。结果表明,哒嗪硫磷水解速率随pH值与温度的升高而显著加快,在15℃、pH 5缓冲溶液中水解半衰期为216.56 d,在35℃、pH 9缓冲溶液中半衰期为3.47 d,平均温度效应系数为2.98。SDS能显著抑制哒嗪硫磷水解,且随着浓度的增大抑制作用增强。哒嗪硫磷在3种土壤中的降解速率依次为南京黄棕壤〉东北黑土〉江西红壤,半衰期分别为10.27、78.75、105.00 d,降解速率随土壤pH值的增大而增大。灭菌处理下,哒嗪硫磷在3种土壤中半衰期显著延长,其中在南京黄棕壤中半衰期延长近10倍,哒嗪硫磷在土壤中降解主要为微生物降解。     

阿特拉津对不同肥力土壤磷酸酶的影响

通过室内恒温培养法，研究除草剂阿特拉津对4种长期定位施肥处理下的土壤的磷酸酶活性的影响。试验结果表明，在阿特拉津质量分数不同和处理时间长短不同的情况下，阿特拉津对土壤磷酸酶的活性既有激活作用又有抑制作用。在试验过程中，4种不同肥力的土壤其磷酸酶活性随着处理时间的延续而呈现出“降低→升高→降低→升高”的消长趋势。不同阿特拉津质量分数对磷酸酶的影响没有规律，同一质量分数处理既有激活作用，也有抑制作用。在4种不同肥力的土壤中，磷酸酶活性最高的是以氮、磷、钾无机肥配合有机肥施用的土壤。     

Environmental degradation of atrazine,linuron and fenitrothion in soil samples

The persistence of atrazine, linuron and fenitrothion in soil samples from an estuarine area (Ebro delta, Tarragona, Spain) has been studied. Soil samples from the top surface (10 cm) were collected during 1989–91, freeze‐dried, sieved through 200 μm, Soxhlet extracted with methanol, cleaned‐up with Florisil and analysed either by gas chromatography‐nitrogen phosphorus detection (GC‐NPD), in the case of atrazine and fenitrothion, or by liquid chromatography with diode array detection (LC‐DAD), for linuron. Confirmation of the samples analysed by GC‐NPD was carried out using GC‐mass spectrometric detection (MS) in the electron impact mode. The soil half lives obtained under the real environmental conditions have been calculated and the values obtained have been correlated with the physicochemical properties of each pesticide and the soil type. Degradation was affected by volatilization since temperatures in the area of study are relatively high, ca. 30°C, in the summer period. In the case of atrazine it has been shown that deethylatrazine is formed in all the samples studied..     

Chloride and atrazine transport through saturated soil columns

A possible contamination of water resources by the application of pesticides is a problem confronting many irrigated areas in arid and semi-arid areas. The best management practices have to be adopted to minimize pesticide transport and leaching under irrigated conditions. Atrazine dissipation in loam and sandy loam soils has been tested in the laboratory using disturbed soil columns under saturated flooding conditions. All the experiments were performed in replicates. The chloride transport was also studied to test its behavior as an inert tracer in both the soils. Atrazine and chloride breakthrough curves were analyzed with the parameter optimization program CXTFIT to determine transport parameters including pore-water velocity (v), retardation coefficient (R), hydrodynamic dispersion coefficient (D), and pulse duration (t _o ). The pore-water velocity and pulse duration of the solute were estimated from the experimental conditions and kept constant during the optimization procedure. The results indicated that the R of chloride was not significantly different from 1, indicating that chloride is an inert tracer for the types of soil tested in this study. The average R of atrazine was 4.56 and 3.15 for sandy loam and loam soils, respectively. Results also showed that the hydrodynamic dispersion coefficient was much higher in the case of sandy loam soil compared to the loam soil for the two solutes, thus indicating non-equilibrium transport conditions. In the case of chloride, D increased from 0.4 for the loam soil to 16.2?cm²/min for the sandy loam soil. Similar results were observed in the case of atrazine in which D for the sandy loam soil was 60% higher than that for the loam soil. More atrazine leaching is expected under field conditions due to the presence of soil cracks and macropores.     

In vitro degradation of the herbicide atrazine by soil and wood decay fungi controlled through Elisa technique

The interaction between atrazine, a triazine herbicide, and a series of decay fungi was characterized in terms of biodegradation of the herbicide and its influence on fungal growth. The following fungi were studied: thermophilic cellulolytic (Penicillium sp. 13) and noncellulolytic (Humicola lanuginosa sp. 5 and 12) strains isolated from self‐heated plant composts, mesophilic diphenol oxidase producing strain Mycelia sterilia INBI 2–26, white‐rot fungi Cerrena maxima, Coriolopsis fulvocinerea and Coriolus hirsutus. Competitive enzyme immunoassay was elaborated for detection of atrazine in cultural liquid. During agar plate cultivation the growth of Humicola sp. 5 was promoted by atrazine whereas the growth of Humicola sp. 12 and Penicillium sp. 13 was suppressed whereas M. sterilia INBI 2–26 was not affected by the herbicide. Neither atrazine‐accelerated nor atrazine‐depressed thermophilic strains decomposed atrazine during 21‐day cultivation according to ELISA data. In contrast, white‐rot fungi Coriolus hirsutus, Coriolopsis fuhocinerea and Cerrena maxima degraded nearly 50% of the herbicide in 5‐day submerged cultivation and 80–92% of the herbicide up to the 40th day. The soil strain M. sterilia INBI 2–26 decomposed 70% of atrazine in 17‐day cultivation. The degradation level depended of the time of atrazine introduction to the growing media. The relationships between the degree of atrazine decomposition and laccase and Mn‐peroxidase production were shown.     

生物炭对土壤中阿特拉津吸附特征的影响

为探究生物炭对土壤中阿特拉津的吸附特征及影响因素,采用批处理实验研究了灭菌(T1)、5%秸秆生物炭+灭菌(T2)、未灭菌(T3)和5%秸秆生物炭+未灭菌(T4)条件下对土壤中阿特拉津吸附特征及土壤理化性质的影响.结果表明,在最初0—12 h内,不同处理下阿特拉津吸附量均随时间的延长而快速增加,而在12—96 h内增加较为缓慢并逐渐趋于平衡.在96 h时,T2和T4处理下阿特拉津最大吸附量分别达到46.22 mg·kg^-1和46.43 mg·kg^-1,而未添加生物炭的T1和T3处理则有所降低,分别为44.20 mg·kg^-1和43.09 mg·kg^-1.准二级动力学模型更好地拟合不同处理下土壤对阿特拉津吸附特征,T2和T4处理下吸附速率常数K分别为0.257 kg·mg^-1·h^-1和0.339 kg·mg^-1·h^-1,显著高于未添加生物炭处理的T1和T3处理(K分别为-0.083 kg·mg^-1·h^-1和-0.261 kg·mg^-1·h^-1).内扩散模型显示添加生物炭后,土壤对阿特拉津的吸附是一个由边界扩散、内部孔隙扩散等多因素控制的复杂化学过程.添加生物炭可显著提高土壤pH、有机碳、碱解氮、速效磷和速效钾含量,其中土壤有机碳含量与阿特拉津最大吸附量之间存在显著的正相关关系(P<0.05).由此可见,添加生物炭可以提高土壤对阿特拉津的固持能力,减少其淋溶迁移风险,从而达到修复阿特拉津污染土壤的目的.     

杀虫双对土壤磷酸酶的毒性效应

采用模拟方法，对碱性、中性和酸性3类磷酸酶的杀虫双毒性效应进行了研究。结果显示：杀虫双强烈抑制碱性和酸性酶活性，达到了极显著负相关，表明酸性磷酸酶活可表征土壤杀虫双污染的程度；而中性磷酸酶对杀虫双的反应较为迟钝，生态毒性也较弱；不同生态区土壤的酶特征截然不，土和红壤中的主导酶类分别是碱性和酸性磷酸酶，揭示出生态环境对土壤酶特征具有决定性的影响。图2表4参6