Bioaccumulation of hexachlorobenzene in Eisenia foetida at di erent aging stages

The impacts of contact time on the extractability, the availability of hexachlorobenzene (HCB) in di erent soils (paddy soil, red soil, and fluvo-aquic soil) and bioaccumulation in earthworm Eisenia foetida were investigated under controlled conditions in laboratory. Results indicated that the aging rate of HCB displaying a biphasic character in di erent soils: a rapid aging in the first 60 d followed by a slow aging in the next 120 d incubation time. Moreover, most of extractable HCB (about 90%) decline occurred in the first 60 d after HCB was spiked into the soils. The aging rate of HCB in the paddy soil was higher than that in the fluvo-aquic soil or the red soil. The amount of HCB accumulated in the earthworms and its accumulative ability, expressed as a bioaccumulation factor (BAF), declined as the aging time increased from 1 to 180 d. Although the extractable HCB decreased with increasing residence time in soil, much of HCB could still be accumulated by earthworms (457.6–984.3 ng/g) through bioaccumulation, which poses a potential risk to soil ecological safety.     

Bioaccumulation of hexachlorobenzene in Eisenia foetida at dierent aging stages

The impacts of contact time on the extractability, the availability of hexachlorobenzene (HCB) in dierent soils (paddy soil, red soil, and uvo-aquic soil) and bioaccumulation in earthworm Eisenia foetida were investigated under controlled conditions in laboratory. Results indicated that the aging rate of HCB displaying a biphasic character in dierent soils: a rapid aging in the first 60 d followed by a slow aging in the next 120 d incubation time. Moreover, most of extractable HCB (about 90%) decline occurr...     

老化对六六六在土壤中可提取态含量及其生物有效性的影响

用室内模拟试验的方法研究了老化作用对六六六在土壤中可提取态含量变化及其在蚯蚓(Eisenia foetida)体内的生物富集规律.结果表明,六六六在土壤中的可提取态含量随着时间延长逐渐降低,下降速率呈现初始较快、而后减慢的趋势.在开始60 d老化时间内,α-六六六、β-六六六、γ-六六六和δ-六六六在土壤中的老化减少量是其初始添加量的57.2%、50%、52.2%和43.2%,分别是其在180 d内老化减少量的90.5%、87.4%、72.4%和84.4%.六六六在蚯蚓体内的生物富集量和生物富集系数也表现出和老化相似的规律.不同老化时间内,六六六在蚯蚓体内的生物富集量表现为α-六六六>β-六六六>δ-六六六>γ-六六六.生物富集系数在开始的15 d为γ-六六六>α-六六六>β-六六六>δ-六六六;而后呈α-六六六>β-六六六>acillus cereus efficiently debγ-rominated and degrade-六六六>δ-六六六的规律.老化使六六六在土壤中的可提取态含量和生物有效性降低,但仍可以在蚯蚓体内有一定的生物富集,对土壤生态安全的威胁依然存在.     

蚯蚓辅助微生物修复芘污染土壤

通过微宇宙实验,研究了蚯蚓对不同土壤中芘的微生物降解率的影响及蚯蚓对芘的富集率.结果表明,有机质较高土壤中芘的微生物降解率和蚯蚓富集率都低于有机质低的土壤,而老化作用降低了芘的生物有效性.无论在新鲜染毒还是老化的土壤中.蚯蚓均可提高土壤中芘的去除率和微生物降解率.在新鲜染毒的红壤和潮土中,蚯蚓可使芘的去除率由41.78%和27.02%分别提高到89.24%和57.53%,其中分别有51.48%和41.63%是蚯蚓促进的微生物降解作用引起的,37.76%和15.90%归因于蚯蚓富集作用.而在老化的红壤和潮土中,蚯蚓可使芘的去除率由36.53%和20.50%分别提高到91.93%和45.46%,其中分别有54.43%和32.83%是蚯蚓促进的微生物降解作用引起的,37.50%和12.63%归因于蚯蚓富集作用.     

水稻土中外源Cd老化的动力学特征与老化因子

选择5种不同性质的水稻土,通过外源添加制备了6个不同浓度梯度的Cd污染土壤,研究了外源Cd在几种水稻土中的老化动力学特征与影响因子;同时利用盆栽实验,结合Log-logistic分布模型,研究了5个不同老化时间(14、30、60、90和180d)与土壤中Cd对二种不同Cd敏感性水稻生长毒性的影响.结果表明,不同浓度外源Cd进入土壤后,0.05mol/L EDTA-2Na浸提的有效态Cd含量随着老化时间的增加而逐渐下降;与14d处理相比,老化30d后土壤中有效态Cd降幅达21.5%(红壤)~38.0%(黑土);老化90d后,土壤中Cd进入慢反应阶段. 基于二级动力学方程的拟合参数显示,土壤中Cd的老化特征表现为有效态Cd含量在30~60d内快速降低,随后变化减缓,经过90d的老化后,土壤中有效态Cd含量逐渐趋于平衡.基于老化动力学方程参数(C∞及K2)与土壤性质间的相关性分析表明,土壤pH值是影响Cd有效态含量变化的主控因子,其次是土壤CEC和OC含量.在不同性质土壤中,随着老化时间的增加,土壤中外源Cd对水稻生长毒性的半抑制浓度(EC50)值显著升高;与14d老化处理相比,经过180d老化后土壤中Cd对水稻生长毒性的EC50增加72.1%~195.0%;在大于90d的长期老化过程中,土壤pH值对Cd老化过程的影响逐渐降低,而CEC的影响逐渐上升,尽管如此,土壤中Cd老化过程的主要影响因子仍然是土壤pH,而与测试的2种水稻品种无关.     

外加芘在2种水稻土及其团聚体培养中的老化及其可浸提性和生物有效性的变化

老化是指有机污染物进入土壤后,随着时间的增加,其生物有效性、毒性和可浸提性会逐渐下降的现象.采用室内培养法研究了外加多环芳烃芘在2种水稻土乌栅土(潜育型水稻土)和黄泥土(潴育型水稻土)及其不同粒组团聚体中的老化现象,并采用二氯甲烷提取和蚯蚓吸收试验比较了培养老化后外加多环芳烃芘的可浸提性和生物有效性的变化.结果表明,培养90d后芘的浸提率下降了15%~23%,蚯蚓的摄食量也下降了37%~67%,说明外加有机污染物进入水稻土后发生了显著的老化现象,从而降低了其环境移动性和生物有效性.但不同粒径团聚体中老化程度没有差异,不过对蚯蚓的生物有效性存在差异.因此,并不能根据土壤中有机污染物的含量来预测其环境风险和生物有效性.     

处理温度和时间对六氯苯污染土壤热解吸修复的影响

以山东潮土作为供试土壤,模拟HCB(六氯苯)污染土壤的热解吸试验研究. 考察处理温度和时间2个主要影响因素对热解吸后土壤中HCB的去除率及其热解产物变化的影响. 结果表明:随处理温度的升高和处理时间的延长,HCB的去除率逐渐增大,在处理温度400 ℃、处理时间10 min时,HCB的去除率达到94.2%;在处理温度450 ℃、处理时间60 min时,HCB 的去除率达到99.4 %,去除效果明显,w(HCB)达到HJ 350—2007《展览会用地土壤环境质量评价标准》的A级标准限值(≤0.66 mg/kg);继续升高处理温度和延长处理时间对HCB的去除率改变不大. HCB的热解吸过程不仅是HCB的物理分离过程,也存在HCB的还原脱氯过程,HCB的热解产物主要为1,3,5-TCB(1,3,5-三氯苯)和1,2,4-TCB(1,2,4-三氯苯);处理温度450 ℃、处理时间60 min为该污染土壤较为合适的热解吸运行参数.      

Tracing the behaviour of hexachlorobenzene in a paddy soil-rice system over a growth season

Hexachlorobenzene (HCB), a persistent organic pollutant (POP), has been found in paddy soils. To improve the understanding of HCB contamination in paddy soils, a laboratory simulative study was carried out to investigate the behavior of HCB in a paddy soil and rice plants. This study was divided into three experiments. First, an experiment aimed to examine the evaporation of HCB in paddy soil. In the second experiment, rice was planted in 10 mg/kg HCB contaminated soil and after pot culture at 3, 6, 9, and 27 weeks (at maturity), both soil and plant samplings were scheduled to be sampled. The soil samples comprised rhizosphere soil, nonrhizosphere soil, and unplanted contaminated soil, whereas plant samples included shoots, roots, and rice grains (dehusked). Lastly, in this part, HCB in xylem saps was designed to be examined. The results showed that (1) the HCB translocation from paddy soil to rice by vaporization; (2) the HCB concentration in rice grains was surprisingly high; (3) the observed HCB decrease in rice rhizosphere offers a potential means for in situ HCB degradation; (4) HCB might not be transported along transpiration in rice.     

生物质炭施用对土壤中氯虫苯甲酰胺吸附及消解行为的影响

分别在黑土、黄壤、红壤、紫色土和潮土中添加0.5%(质量分数)生物质炭,采用批处理等温吸附实验及室内消解实验测定了CAP的吸附等温线及消解动态,目的是揭示不同类型土壤中施用生物质炭对残留CAP的环境行为影响规律,为评估生物质炭田间施用综合生态效应,评价土壤残留CAP的环境污染风险提供理论依据.结果表明,生物质炭施用可提高土壤对CAP的吸附活性,但提高程度因土壤性质不同而异.有机质含量较高的黑土中添加生物质炭,吸附农药Kd值提高了2.17%,而有机质含量较低的潮土添加等量生物质炭后则提高了139.13%.生物质炭施入土壤后其对农药吸附活性受到不同程度抑制.与施入土壤前比较,生物质炭施入黑土、黄壤、红壤、紫色土和潮土中后吸附常数KF,biochar分别降低了96.94%、90.6%、91.31%、68.26%和34.59%.CAP在黑土、黄壤、红壤、紫色土和潮土中的消解半衰期为115.52、133.30、154.03、144.41和169.06 d,而在添加生物质炭的土壤中消解半衰期分别延长了20.39、35.76、38.51、79.19和119.75 d.与吸附实验结果一致,生物质炭施入黑土对延缓农药土壤消解作用最小,而潮土中施入生物质炭效果最明显.本研究表明生物质炭施入土壤后可增强对农药的吸附作用,延缓农药的土壤消解,但影响程度与土壤性质有关.     

五种土壤吸附喹乙醇特性的研究

用振荡平衡法研究了喹乙醇在东北黑土、常熟水稻土、陕西潮土、南京黄棕壤和江西红壤中吸附行为及其影响因素.结果表明,喹乙醇在5种土壤中的吸附行为均可用Langmuir方程和Freundlich方程进行良好的线性拟合.其吸附系数KF很小,分别为2.813,1.740,0.446,0.309和0.201,显示很难被土壤吸附.其KF与土壤有机质含量及阳离子交换量呈良好的相关性.而与土壤pH值及黏粒含量相关性较差.温度和离子强度均对喹乙醇在土壤中的吸附有一定影响,较低的温度和离子强度均有利于土壤对喹乙醇的吸附.     

生物质炭对华北平原4种典型土壤N2O排放的影响

生物质炭作为一种新型的土壤改良剂,在降低土壤温室气体排放方面发挥着重要作用.为明确生物质炭对冬小麦苗期土壤N_2O排放的影响,以华北平原的4种典型土壤(水稻土、砂姜黑土、褐土和潮土)为研究对象,进行田间试验,设置了4个处理:对照(CK)、单施化肥(NPK)、单施生物质炭(BC)和化肥与生物质炭配施(NPK+BC).结果表明,单施化肥显著增加了4种土壤N_2O排放,与对照相比,水稻土、砂姜黑土、褐土和潮土N_2O排放分别增加了314%、116%、240%和282%.添加生物质炭对华北平原4种土壤N_2O排放影响存在差异,与CK相比,单施生物质炭水稻土、褐土N_2O排放显著增加了72. 4%和50. 9%,而砂姜黑土和潮土BC与CK处理无显著差异.与NPK相比,生物质炭与化肥配施显著降低了4种土壤N_2O排放.添加生物质炭提高了4种土壤pH,其中,初始pH最低的水稻土,受生物质炭影响较显著,施肥则降低了4种土壤pH.砂姜黑土、褐土和潮土施肥处理N_2O排放通量均与铵态氮含量呈显著正相关,水稻土和砂姜黑土单施生物质炭处理N_2O排放通量与硝态氮含量呈显著正相关.     

Aging effect on the mobility and bioavailability of copper in soil

Aging effect on the mobility and bioavailability of copper (Cu) was investigated using a spiked soil with different incubation periods from 3 to 56 d. Wheat was planted and earthworm was cultured separately in the incubated soils. The mobility of Cu in soil was evaluated by a chemical fractionation scheme and the toxicity and bioavailability were assessed by measuring the biomass and Cu concentration in tissues. Results showed that aging had a significant effect on Cu fraction distribution, of which Cu tended to incorporate from the exchangeable into more stable fractions such as the reducible and oxidisable fractions. However, aging had little effect on Cu bioavailability to wheat and earthworms. Comparing the soil being incubated for 3 d and 56 d, Cu concentration in wheat roots decreased from 14.5 to 12.8 mg/kg, and no significant changes in Cu concentration were observed in both wheat shoots and earthworms. The Cu concentration was around 2.0 and 50 mg/kg for wheat shoots and earthworms, respectively, irrespective of soil incubation time. The CaCl2-extractable Cu had a linear relationship with Cu concentration in wheat roots (R2 = 0.65, P < 0.05), but no linear relationship can be found for wheat shoots and earthworms. Biological control may be more crucial for Cu accumulation in organism than the changes in soil Cu fraction caused by aging.     

高效氯氰菊酯在土壤中的降解动态

在实验室条件下研究了高效氯氰菊酯两个异构体在3种土壤中的降解动态,随着时间的延长,氯氰菊酯在土壤中的含量逐渐减少.在未考虑土壤中微生物的作用时,3种农药在土壤中的稳定性与土壤中的有机质含量及pH值存在一定的相关性;高效氯氰菊酯在有机质含量高、pH值高的土壤中降解较快;在土壤中的降解以微生物降解为主,化学降解为辅.高效氯氰菊酯顺式体、反式体在黑土中的降解半衰期分别为7.95,5.35d;在河南二合土中的降解半衰期分别为13.2,6.87d;在江西红壤中的降解半衰期分别为30.3,15.9d,3种土壤微生物均选择性降解高效氯氰菊酯反式体,并且在酸性土壤中表现得更为稳定.     

微生物群落对土壤微生物呼吸速率及其温度敏感性的影响

通过灭菌和重新接种不同土壤微生物群落的方法,探索了改变土壤微生物群落对土壤微生物呼吸速率及其温度敏感性的影响.结果表明,灭菌海伦黑土接种未灭菌的哈尔滨黑土、封丘潮土和祁阳红壤后,15℃时土壤CO2的累积释放量分别为684.25、753.97和644.91μg,25℃时土壤CO2的累积释放量分别为963.06、1 015.44和852.31μg,35℃时土壤CO2的累积释放量分别为1 252.55、380.36和1 177.88μg;土壤CO2的累积释放量随接种剂土壤pH增加而增加,而与接种剂土壤有机质含量高低、接种剂土壤与被接种土壤的地理距离无关.15、25和35℃时,接种不同微生物群落的土壤呼吸速率表现差异的持续时间分别为104、277和1 177 h,差异持续时间随培养温度增高而延长.接种未灭菌的哈尔滨黑土、封丘潮土和祁阳红壤后,土壤呼吸温度敏感性指数Q10在0～104 h分别为1.63、1.49和1.80,在0～277 h分别为1.43、1.39和1.46,在0～1 609 h分别为1.35、1.35和1.35;呼吸温度敏感性随接种剂土壤pH降低而增加,随培养时间延长而减小.本研究表明改变土壤微生物群落将影响土壤微生物呼吸速率及其温度敏感性.     

添加有机物料对淹水土壤Cd活性的影响机制

采用红壤(pH 4.46)和潮黄土(pH 7.10),在N2覆盖下淹水(25±0.5)℃培养60d,研究了淹水土壤加入有机物料(苜蓿、稻草粉)后Cd活性变化及其制约机理.结果表明,土壤淹水后,氧化铁的还原溶解作用带来Fe组分再分配和pe+pH下降,导致Cd组分向低活性组分转化.淹水土壤添加有机物料后,通过pe+pH下降效应和pH升降效应增强了对Cd活性转化的影响,其中,红壤有机物料处理较对照pe+pH降低和pH值升高,致使固相Exc-Cd含量和液相Cd浓度低于对照,土壤Cd活性降低;潮黄土有机物料处理pe+pH和pH值均低于对照,致使固相Exc-Cd含量和液相Cd浓度高于对照,土壤Cd活性增加.添加有机物料对固相Org-Cd再分配的影响小,但在液相中DOM与Cd的络合效应显著.     

我国典型土壤对病毒等温静态吸附的数值模拟

通过室内等温静态批量平衡吸附实验,采用3种常见的等温线（Freundlich方程、Langmuir方程和Temkin方程）对2种病毒（MS2和X174）在2种处理（非灭菌和灭菌）条件下的6种土壤（红壤土、红粘土、乌栅土、黄泥土、沙质潮土和壤质潮土）中的吸附行为进行了回归拟合.实验结果和模拟结果均表明,土壤性质、病毒性质、土壤中的土著微生物对病毒在土壤中吸附行为均具有重要的影响.红粘土对MS2和X174的平均吸附比例几乎能达到100％,而2种潮土（沙质潮土和壤质潮土）相对较弱;总体来看土壤对X174的吸附能力高于MS2,但灭菌后的土壤对MS2的吸附能力却高于X174.在数值模拟中,Freundlich方程和Langmuir方程均具有理想的相关性.Freundlich方程能够表现出病毒浓度对其在土壤中吸附行为的影响;尽管Langmuir方程能够应用于土壤对病毒吸附能力的比较,但本研究中不能应用Langmuir方程来计算土壤对病毒的最大吸附量.     

不同类型土壤中As(Ⅴ)解吸行为的研究

为了解As(Ⅴ)在土壤中的解吸行为及不同类型试剂(NaOH、NaCl、NaHCO3、柠檬酸、草酸及磷酸盐缓冲液)对所吸附砷的解吸效果,对As(Ⅴ)在不同类型土壤中的解吸热力学和动力学效果进行了研究.结果表明,NaOH和磷酸盐缓冲液对几种土壤吸附砷的解吸效果较好,解吸率分别在47.3%～73.0%和35.4%～66.6%...     

Clomazone dissipation, adsorption and translocation in four paddy topsoils

IntroductionClomazone,(2 [(2 chlorophenyl)methyl ] 4 ,4 dimethyl 3 isoxazolidinone) ,isasoil appliedisoxazolidinoneherbicideproducedbyFMCCorp .Itisintroducedforannualgrassandbroad spectrumweedsinsoybeans(Rani,1998;Vyas,2 0 0 0 ) .Itisalsocurrentlyregis…     

Copper pollution decreases the resistance of soil microbial community to subsequent dry–rewetting disturbance

Dry–rewetting(DW) disturbance frequently occurs in soils due to rainfall and irrigation, and the frequency of DW cycles might exert significant influences on soil microbial communities and their mediated functions. However, how microorganisms respond to DW alternations in soils with a history of heavy metal pollution remains largely unknown.Here, soil laboratory microcosms were constructed to explore the impacts of ten DW cycles on the soil microbial communities in two contrasting soils(fluvo-aquic soil and red soil)under three copper concentrations(zero, medium and high). Results showed that the fluctuations of substrate induced respiration(SIR) decreased with repeated cycles of DW alternation. Furthermore, the resistance values of substrate induced respiration(RS-SIR)were highest in non-copper-stressed(zero) soils. Structural equation model(SEM) analysis ascertained that the shifts of bacterial communities determined the changes of RS-SIR in both soils. The rate of bacterial community variance was significantly lower in noncopper-stressed soil compared to the other two copper-stressed(medium and high) soils,which might lead to the higher RS-SIR in the fluvo-aquic soil. As for the red soil, the substantial increase of the dominant group WPS-2 after DW disturbance might result in the low RS-SIR in the high copper-stressed soil. Moreover, in both soils, the bacterial diversity was highest in non-copper-stressed soils. Our results revealed that initial copper stress could decrease the resistance of soil microbial community structure and function to subsequent DW disturbance.     

典型土壤组分及其与丁草胺除草剂作用的红外光谱研究

运用红外光谱法对3种典型土壤(红壤、潮土和黑土)的矿物质、胡敏酸及其与丁草胺的吸附附着物进行了研究.结果表明,江西红壤为高岭石型矿物质,在3 703,3 628,1 089,1 035,914,696及471 cm-1处有特征吸收峰.北京潮土和黑龙江黑土为蒙脱土型矿物质,在1 432和872 cm-1处有特征吸收峰,而在3 703和3 628 cm-1处吸收较弱或微弱.不同土壤中胡敏酸的组成基本相同,均在3 420,2 935,2 847,1 724,1 660及1 035 cm-1处有明显吸收,表明其含有缔合羟基、芳烃、羰基、醇、酚及酸等.丁草胺与土壤胡敏酸的吸附机理主要是在胡敏酸的羰基及酚醇羟基上形成氢键.