黑麦草对菲污染土壤修复的初步研究

本文研究了黑麦草(Lolium multiflorum Lam)对多环芳烃菲污染土壤的修复作用。通过60天的温室盆栽试验,观察到土壤中菲的可提取浓度随着时间逐渐减少,黑麦草加快了土壤中可提取态菲浓度的下降。在5、50、500mg/kg菲处理浓度下黑麦草生长的土壤中菲的降解率分别达93.1%、95.6%和94.7%。黑麦草增强土壤中多酚氧化酶活性而提高植物对菲的降解率。土壤自身具有修复多环芳烃菲的自然本能,种植黑麦草具有强化土壤修复菲污染的作用。增加黑麦草产量,增强土壤多酚氧化酶活性,可能提高黑麦草植物修复菲污染土壤的能力。     

红树植物秋茄对菲污染沉积物的根际修复研究

利用盆栽试验方法,研究了红树植物秋茄（Kandelia cande（lL.） Druce）对多环芳烃菲污染沉积物的修复作用。结果表明,在5、10、20、40mg·kg^-1菲处理浓度下,菲对秋茄的生长具有抑制作用,沉积物中菲初始浓度越高抑制作用越明显。4个月的修复试验结果表明,与无植物对照相比,种植秋茄能够明显促进沉积物中菲的降解。根际沉积物中菲的去除率为69%-82%,而非根际沉积物中菲的去除率为59%-66.9%。相同污染水平处理下根际沉积物中菲残留浓度低于非根际沉积物,而菲降解菌数量、多酚氧化酶和脱氢酶活性高于非根际沉积物,从而提高了沉积物中菲的降解率。     

深圳市土壤多环芳烃背景值及其源解析

【目的】精细化描述深圳市土壤多环芳烃(PAHs)的背景值和空间分布情况。【方法】采用环境单元法和网格法,在深圳市不受或很少受人类活动影响的基本生态控制区内布设了450个土壤表层点位和50个典型剖面点位。通过多点增量采样法,最终采集500个表层土壤样品和100个剖面土壤样品。利用SPSS统计分析了表层土壤样品和剖面土壤样品的PAHs含量,探究了表层土壤PAHs的背景值与土壤理化性质的相关性,分析了表层土壤PAHs的来源。【结果】(1)深圳市自然背景下表层土壤PAHs浓度变化范围为1.1～1004.19μg kg^-1(95%分位值为30.82μg kg^-1,土壤干重)。表层土壤PAHs中5环的占比为29.58%,占比最高。其次为3环和6环,占比分别为22.70%和20.23%。(2)50个剖面点位上土壤表、中和底层的PAHs总量的95%分位值分别为21.38μg kg^-1、12.34μg kg^-1和15.15μg kg^-1,平均值分别为9.35μg kg^-1、...     

苏丹草对土壤中菲芘的修复作用

采用盆栽试验法,研究了苏丹草对土壤中菲、芘的去除效果,及植物和微生物在去除土壤菲、芘中的交互效应。结果显示,在试验浓度范围（0-322．06mg·kg^-1内,土壤～苏丹草系统（TR,）对菲、芘的去除效果明显。种植苏丹草60d后,土壤菲、芘去除率分别为73．07％-83．92％、63％～77．62％;平均去除率分别比对照1（无植物,不加0．1％NaN3）高55．58％、50．71％,比对照2（无植物,加0．1％NaN3）高72．71％、66．57％,说明种植苏丹草可以促进微生物对土壤中芘、菲降解。土壤酶活性测定结果也显示,酶活性越高,污染物降解率越高,反之亦然。因此,植物一微生物间的交互效应是土壤中多环芳烃降解的主要途径。     

低分子量有机酸作用下土壤中菲和芘的残留及形态

采用微宇宙试验方法,以菲和芘为多环芳烃(PAHs)代表物,研究了几种低分子量有机酸作用下黄棕壤中菲和芘的残留和形态。结果表明,老化60 d后土壤中菲和芘的残留含量明显减少;不施加有机酸的对照土壤中,菲和芘的残留含量为10.13和29.18 mg kg-1,去除率为87.33%和63.50%。与对照相比,供试浓度(0～64 mg kg-1)范围内,柠檬酸、草酸、酒石酸等3种低分子量有机酸作用下土壤中PAHs残留含量提高,去除率减小,表明供试条件下有机酸抑制土壤中菲和芘的降解;进一步分析发现,少量(≤4 mg kg-1)的有机酸即可对PAHs降解产生高的抑制效果。微生物降解在PAHs的去除中起重要作用,且芘比菲更抗微生物降解。供试条件下,可脱附态和有机溶剂提取态是土壤中菲和芘存在的主要形态,而结合态残留占总残留的比例很小(<8.5%)。3种有机酸均提高了土壤中可脱附态和有机溶剂提取态菲和芘的残留含量,施加有机酸使土壤中菲和芘的可脱附态含量较对照分别提高了46.67%～749.1%和1.83%～80.20%,有机溶剂提取态则提高了8.73%～375.2%和22.63%～114.3%;低分子量有机酸作用下结合态的菲和芘含量仍很小。     

蚯蚓在植物修复菲污染土壤中的作用

采用盆栽试验法,研究了蚯蚓（Pheretima sp.）在植物修复菲污染土壤中的作用。结果显示,试验浓度（20.05-322.06 mg.kg-1）范围内,蚯蚓活动促进了菲污染土壤中修复植物黑麦草（Lolium multiforum）的生长,其根冠比明显增大。添加蚯蚓72 d后,种植黑麦草的土壤中菲的去除率高达64.35%-93.40%,其平均去除率（80.92%）比无蚯蚓活动的土壤-植物系统（71.57%）提高9.35%,比无植物对照组（22.58%）提高57.34%。各种生物、非生物修复因子中,植物-微生物交互作用对菲去除的平均贡献率（53.56%）最为突出,比无蚯蚓活动时（47.48%）提高6.08%。说明蚯蚓活动可强化土壤-植物系统对土壤菲污染的修复作用。     

菲降解菌的分离鉴定及其在污染土壤生物修复中的应用

采用室内培养方法,从吴江市郊长期被多环芳烃污染的土壤中富集到以菲为唯一碳源和能源的菲降解复合微生物菌群,复合菌群在7d内对无机盐液体中菲（含量100mg·L^-1）的降解率达到99%。从复合菌群中分离纯化获得两株菲高效降解菌B1和L2,经过菌体形态特征、生理生化特征和16SrDNA序列分析,鉴定菌株B1为百日咳博行特氏菌（Bordetella petrii）,菌株L2为墨西哥假黄单胞菌（Pseudoxanthomonas mexicana）。这两株菌在菲含量为100mg·L^-1的无机盐培养液中,7d内对菲（含量100mg·L^-1）的降解率大约为80%,9d内的降解率可达到99%。将复合菌群和菲污染土壤混合,在光照培养箱中进行培养修复。结果表明,修复88d后,接种复合菌群的低污染浓度（8.22mg·kg^-1）处理和高污染浓度（39.65mg·kg^-1）处理的菲去除率分别达到95.74%和98.06%。     

硅在Cd胁迫下对黄瓜产量和品质的影响

研究石灰性土壤Si对Cd胁迫下黄瓜产量和品质的影响,对实际土壤Cd毒害植物防治具有重要意义。采用盆栽完全随机设计方案,以黄瓜(密刺60)为试验材料,研究Si在Cd胁迫下对黄瓜产量和品质的影响。研究证明,随着Cd浓度的增加,黄瓜株高和鲜重显著降低,还原糖和维生素C含量降低,硝酸盐和果实中Cd含量明显增加。施入Si后,能显著改善黄瓜的产量和品质。当Cd含量为3 mg kg^-1,Si施加量为300 mg kg^-1时,黄瓜株高增加了31.9%。当Cd含量为5 mg kg^-1,Si施加量≥200 mg kg^-1情况下,黄瓜中硝酸盐含量下降21%～37%。Cd含量≤3 mg kg^-1,施Si量200 mg kg^-1时黄瓜中的维生素C含量达到最大值。当Cd含量≤3 mg kg^-1时,100mg kg^-1的Si施加量能使黄瓜果实中的Cd含量降至国家食品安全标准。试验结果可知,在石灰性土壤上,Cd会明显抑制黄瓜的生长,施加硅后可以显著改善Cd毒害,进而提高黄瓜的产量和品质。     

西藏日喀则地区青稞籽粒与栽培土壤中锌和硒含量特征

【目的】明确日喀则地区青稞及其栽培土壤中的锌、硒含量现状，探讨土壤锌、硒含量与青稞籽粒锌、硒之间的相关关系，为当地青稞的锌、硒营养强化栽培及育种提供参考。【方法】采用野外调查和室内分析相结合的方法自日喀则地区12个县(区)采集7个品种、86份青稞样品及其农田土壤样品进行测定分析。【结果】日喀则地区青稞籽粒锌含量范围为15.61～19.96 mg kg^-1，硒含量范围为60.88～186.19μg kg^-1。其中，主栽品种“喜玛拉19”籽粒硒富集能力较强，硒含量可达186.19μg kg^-1，显著高于其他品种；不同品种青稞籽粒锌含量无显著差异。日喀则地区青稞栽培土壤全锌、全硒含量分别为55.77～82.21 mg kg^-1、113.43～354.29μg kg^-1，土壤有效锌、有效硒含量分别为0.50～1.02 mg kg^-1、14.66～32.25μg kg^-1；大部分供试土壤锌、硒含量处于中低水平，其中，40.70%的土壤锌处于低水...     

蚯蚓对土壤-植物系统中菲、芘降解的强化效应研究

采用盆栽试验方法,研究了蚯蚓（Pheretima sp.）对土壤-植物系统中菲、芘的去除效果的强化作用及对土壤酶活性的影响。结果表明,在试验浓度范围（0~322 mg.kg-1）内,蚯蚓对供试植物苏丹草（Sorghum vulgare L.）生长促进作用显著。接种蚯蚓的土壤中,苏丹草在菲、芘各浓度下总生物量较未接种蚯蚓土壤分别提高14.41%~25.91%、14.39%~23.9%;蚯蚓活动可促进土壤-植物系统中菲、芘的降解,接种蚯蚓处理中菲、芘各浓度下降解率较未接种蚯蚓处理分别高4.20%~9.76%、3.69%~9.38%。土壤酶活性测定结果也显示蚯蚓活动可增加土壤酶的活性。     

蚯蚓与黑麦草相互作用对土壤中荧蒽去除的影响

Earthworms can promote the bioremediation of contaminated soils through enhancing plant growth and microorganism development. The individual and combined effects of earthworms and ryegrass (Lolium multiflorum Lam.) on the removal of fluoranthene from a sandy-loam alluvial soil were investigated in a 70-d microcosm experiment. The experiment was set up in a complete factorial design with treatments in four replicates: without earthworms or ryegrass (control, CK), with earthworms only (E), with ryegrass only (P), and with both earthworms and ryegrass (EP). The residual fluoranthene, microbial biomass C, and polyphenol oxidase activity in the soil changed significantly (P<0.01) with time. In general, the residual concentration of fluoranthene in the soil decreased sharply from 71.8-88.7 to 31.7-37.4 mg kg 1 in 14 d, and then decreased gradually to 19.7-30.5 mg kg 1 on the 70th d. The fluoranthene concentration left in the soil was the least with both earthworms and ryegrass, compared to the other treatments at the end of the experiment. Half-life times of fluoranthene in the E, P, and EP treatments were 17.8%-36.3% smaller than that of CK. More fluoranthene was absorbed by earthworms than ryegrass. However, the total amounts of fluoranthene accumulated in both the ryegrass and earthworms were small, only accounting for 0.01%-1.20% of the lost fluoranthene. Therefore, we assumed that microbial degradation would play a dominant functional role in fluoranthene removal from soil. We found that earthworms significantly increased microbial biomass C and polyphenol oxidase activity (P<0.01) in the presence of ryegrass at the end of the experiment. Furthermore, microbial biomass C and polyphenol oxidase activity were significantly (P<0.05) and negatively related to the residual fluoranthene concentration. This implied that earthworms might promote the removal of fluoranthene from soil via stimulating microbial biomass C and polyphenol oxidase activity.     

四环素对芘污染农田土壤微生物修复的影响及响应过程

针对城郊农田土壤中多环芳烃和抗生素复合污染的新特征,通过室内模拟土培实验,研究四环素(Tetracycline,TC)胁迫下,降解菌Sphingobium sp.PHE3对长三角典型农田土壤中芘的降解效果和影响机制。研究表明,接种降解菌处理(B)能明显促进土壤中芘的降解,TC的引入可显著抑制土壤中芘的深度降解过程(P0.05)。经过90天培养后,B处理与接菌+添加TC处理(BTC)的降解率分别为40.1%、25.7%,较对照分别提高了23.0倍、14.1倍。通过土壤微生物群落结构多样性分析发现,降解菌数量在经历90天的土壤环境适应期后逐渐快速增加,其数量变化与污染物芘在土壤中含量消减趋势呈负相关;引入芘和四环素对土壤细菌群落结构多样性和功能稳定性具有显著影响(P0.05),然而对土壤真菌群落影响不显著(P0.05)。此外,B和BTC处理条件下,土壤过氧化氢酶活性、荧光素二乙酸酯酶活性和土壤微生物生物量碳氮值显著高于单独添加芘处理(P)和单独添加TC处理(TC),但P处理与TC处理之间无显著差异(P0.05),说明外源污染物(芘或四环素)对于土壤酶活性和微生物生物量碳氮具有显著抑制作用(P0.05),致使降解菌功能作用受到抑制。综上研究结果表明TC可明显抑制土壤中典型四环多环芳烃的微生物降解过程,针对多环芳烃与抗生素复合有机污染农田土壤的微生物强化修复技术有待深入研究。     

生物耕作对土壤理化特性、酶活性及青花菜生长和品质的影响

通过田间试验,研究生物耕作(接种蚯蚓)对土壤理化性质、酶活性及青花菜生长和产量品质的影响。试验设置了传统机械旋耕(CK)、免耕(T1)以及生物耕作(T2)3个处理。研究结果表明:(1)生物耕作能有效提高耕层不同部位的土壤养分含量和含水量,其中尤以5～20 cm土层较为明显,生物耕作处理土壤有机质、全氮、有效磷含量以及含水量依次比传统机械旋耕(CK)增长58.33%、68.93%、67.06%和16.19%;与传统机械旋耕(CK)相比,生物耕作处理大大提升了土壤过氧化氢酶、脲酶以及蔗糖酶的活性,其中脲酶、蔗糖酶与CK之间差异显著(P<0.05)。(2)生物耕作处理下青花菜的株高、开展度、叶长、叶宽等指标与CK和T1之间差异显著(P<0.05);各处理间青花菜的叶绿素相对含量差异不大,生物耕作处理增强了青花菜在各生长期的净光合速率。(3)生物耕作处理大幅提高了青花菜品质,生物耕作处理下的青花菜Vc含量是CK的1.2倍,硫代葡萄糖苷含量分别比T1处理和CK高1.05 mol·g-1和3.29 mol·g-1,差异均达到显著水平;各处理间可溶性糖含量差异不显著。因此,在传统的农业生态系统中,培育土壤有益动物的生物数量(生物耕作)可提高土壤养分和酶活性,对改善农田土壤肥力有着重要意义。     

蚓粪对黑麦草吸收污染土壤重金属铜的影响

在长江冲积物形成的高沙土中加入CuSO4.5H2O模拟土壤污染,使Cu污染浓度分别为200、400、600 mg kg-1,并设置加蚓粪(15%)和加原土(15%)处理,二处理各设种植黑麦草(Lolium multiflorum)和不种黑麦草培养试验,研究蚓粪对黑麦草生长及对Cu吸收的影响,以揭示蚓粪在Cu污染土壤植物修复中的作用。结果表明:蚓粪显著增加了黑麦草的地上部和地下部的生物量(p<0.001**)以及根系的长度、表面积、体积和根尖数(p<0.05*),在Cu浓度为200 mg kg-1时促进作用最大;蚓粪还显著提高了黑麦草地上部Cu的浓度及累积量,但显著降低了地下部的Cu浓度(p<0.05*),而对地下部的铜累积量没有影响,显示蚓粪能促进Cu从根系向地上部的运移及在地上部的富集。通过对土壤的pH和Cu的形态特征分析,发现种植黑麦草处理降低了土壤的pH并增加了可交换态铜的含量,而且这种作用在加入蚓粪后更加明显。推测蚓粪主要通过促进黑麦草根系的生长和活性而影响根系周围环境,提高重金属铜的生物有效性进而增加植物对铜的吸收。     

Phosphorus in agricultural constructed wetland sediment is sparingly plant‐available

Agricultural constructed wetlands (CWs) are intended to retain sediment and phosphorus (P) carried off with runoff and drainage water. The accumulated sediment, with adsorbed P, is often advised to be recycled to agricultural land, but little is known about the fertilizer value of sediment‐associated P. This study examined the effects on P adsorption characteristics and P plant availability of mixing CW sediment into soil. Although the total P content in the sediment was approximately equal to that in catchment soil and the NaOH‐extractable P content was higher to that in catchment soil, in adsorption‐desorption tests sediment P solubility decreased and affinity for P increased with increasing addition rate of CW sediment to soil. Already the lowest sediment addition rate (12.5% of dry weight) decreased the equilibrium P concentration (EPC₀') by 60% on average compared to unamended catchment soil. In a greenhouse pot experiment, Italian ryegrass (Lolium multiflorum L.) yield was largely unaffected by CW sediment application, but P uptake systematically decreased when the rate of sediment application to soil increased. When 12.5% dry weight of sediment was added, plant P uptake decreased by 6–50% in P‐unfertilized pots and by 6–17% in P‐fertilized pots (150 mg P kg⁻¹) compared with P uptake of ryegrass grown in unamended field soil. Our other results suggest that the plant availability of P in CW sediments is very low due to high clay content and high concentrations of aluminium (Al) and iron (Fe) (hydr)oxides in the sediment. Thus, if applied to agricultural fields in large quantities, dredged CW sediment may impair crop P supply.     

Atrazine and phenanthrene degradation in grass rhizosphere soil

Organic contaminants often disappear more quickly from planted than from non-planted soils. Five grass species (Sudan grass, ryegrass, tall fescue, crested wheatgrass and switch grass) were grown in soils without (Phase I) or with (Phase II) prior atrazine (ATR) and phenanthrene (PHE) amendment to study the degradation of these compounds by rhizosphere microorganisms. In suspensions of soil without prior chemical exposure, no significant loss of ATR was observed after 16 days incubation. The most probable number (MPN) of ATR-degrading bacteria in the soils was below detection. Phenanthrene degradation was observed in suspensions inoculated with all soils, but the rates of degradation were not significantly different among them. The number of PHE-degrading bacteria was similar in planted and non-planted soils (10⁵ cells g⁻¹ soil) except the number in tall fescue soil was significantly higher than in non-planted soil. In the Phase II study, both compounds were mineralized whether or not soils had been conditioned with ATR or PHE. Prior amendment with either ATR or PHE significantly reduced the acclimation period preceding the onset of mineralization. However, enumeration procedures detected ATR-degrading bacteria only in ATR-amended soils. Prior exposure to PHE did not alter the number of PHE-degrading bacteria significantly.     

源于松针的可溶性有机物对土壤多环芳烃吸附和解吸行为的影响研究

Study of the relationship between plant litter-derived dissolved organic matter（DOM） and organic pollutant transport in soil is important for understanding the role of forest litter carbon cycling in influencing pollutant behaviour and fate in forest soil.With the aim of providing insight into the capacity of plant litter-derived DOM to influence sorption and desorption of selected polycyclic aromatic hydrocarbons（PAHs） on soil, batch experiments were carried out with application of a sorption-desorption model incorporating DOM effects. Freshly fallen pine（Pinus elliottii） needles were used as the source of organic matter. Input of the pine needle litter-derived DOM was found to significantly decrease desorption hysteresis as well as soil adsorption capacity of phenanthrene（PHE） and fluoranthene（FLA）. Addition of 1 728 mg L-1dissolved organic carbon（DOC） lowered the organic carbon-normalized sorption distribution coefficient of PHE from 7 776 to 2 541 L kg-1C and of FLA from 11 503 to 4 368 L kg-1C. Decreases of the apparent sorption-desorption distribution coefficients of PHE and FLA with increased DOC concentration indicated that DOM favored desorption of PAHs from soil. Increases in the fraction of apparently dissolved PAHs were attributable to the dissolved PAH-DOM complexes, accounting for the dissolved proportions of 39% to 69% for PHE and 26% to 72% for FLA in the sorption and desorption processes as the concentration of the added DOM solution rose from 0 to 1 728 mg L-1. Our results suggest that pine needle litterderived DOM can have a substantial effect of inhibiting PAHs sorption and promoting PAHs desorption, thus leading to enhanced leaching in soil, which should be taken into account in risk assessment of PAHs accumulated in forest soil.     

甘蔗酒精废液对土壤理化性状及氧化还原酶的影响

在蔗地上设计不施肥(CK1)、施化肥(CK2)和4个直接喷施甘蔗酒精废液处理,研究不同用量废液施用对土壤理化性状及两种氧化还原酶活性的影响.结果表明:蔗地施用废液提高了土壤全氮、Cl-、有机质、腐殖质含量,使甘蔗苗期土壤过氧化氢酶和多酚氧化酶活性异常升高,随后迅速下降,成熟期下降到接近或小于CK2的土壤酶活性水平.甘蔗苗期土壤过氧化氢酶活性与全氮、有机质、腐殖质呈极显著正相关,与富里酸、胡敏酸、Cl-呈显著正相关(r0.05=0.811,r0.01=0.917,n=6);土壤多酚氧化酶活性与有机质、腐殖质、Cl-呈显著正相关.与不种植甘蔗的75 tCK废液处理相比,种植甘蔗的75 t废液处理甘蔗生长后期土壤全氮、有机质、Cl-含量和多酚氧化酶活性较低.说明与施用化肥或不施肥处理相比,蔗地施用废液有提高土壤肥力和有机质、腐殖质含量的作用,但也使施用初期过氧化氢酶和多酚氧化酶活性异常升高,施废液的土壤种植甘蔗对废液养分吸收和环境净化有一定作用.     

Characterization of rhizosphere microbial community structure in five similar grass species using FAME and BIOLOG analyses

Accelerated biodegradation of organic contaminants in planted soil is frequently reported yet our current understanding of plant–microbe interactions does not allow us to predict which plant species can encourage the development of rhizosphere communities with enhanced degradation capacity. In a companion study, five grass species (Sudan grass, ryegrass, tall fescue, crested wheatgrass, and switch grass) were grown in a Matapeake silt loam soil to study the degradation of atrazine and phenanthrene by rhizosphere microorganisms (see Fang et al., 2000, this vol., Fang, C., Radosevich, M., Fuhrmann, J. J., 2000. Atrizine and phenanthrene degradation in grass rhizosphere soil. Soil Biology & Biochemistry, in press). In the present paper substrate utilization patterns (BIOLOG^®), and fatty acid methyl ester (FAME) profiles of the same rhizosphere microbial communities were determined. Both FAME and BIOLOG^® analyses detected changes in soil microbial community structure among treatments. However, community structure did not directly correlate to either ATR or PHE degradation rates.     

保水剂施用量对杨树苗土壤物理性状与微生物活性的影响

[目的]探讨保水剂不同施用量对杨树土壤物理性状与微生物活性的作用效果,为中国杨树人工林节水高产实践模式提供理论依据与技术参考。[方法]研究CK(常规灌量)、CL(60%常规灌量配施10g保水剂)、CM(60%常规灌量配施30g保水剂)和CH(60%常规灌量配施50g保水剂)4个处理对杨树苗土壤物理性状、水稳性团粒结构、微生物数量、微生物呼吸和代谢熵的影响。[结果]同CK相比,CM处理显著降低了土壤容重,并明显提高了非毛管孔隙度,其中土壤容重分别较CK,CL和CH处理显著下降13.71%,5.31%和7.76%;还明显促进了土壤大团聚体(0.25mm团粒)的形成。同时,CM处理明显增加了土壤微生物总量和微生物量碳、氮含量,并显著增强了土壤微生物呼吸作用,其微生物呼吸速率分别比CK,CL和CH处理提高30.77%,11.84%和7.59%。此外,CM处理还降低了代谢熵,分别较CK,CL和CH处理下降4.81%,8.29%和9.74%。[结论]适宜的节水灌溉措施(60%常规灌量与30g保水剂组合)有助于改善杨树苗土壤的物理环境,并增强微生物活性。