Environmental fate of the triazole fungicide propiconazole in a rice-paddy-soil lysimeter

Environmental fate of the triazole fungicide propiconazole, 1-[[2(2,4-dichlorophenyl)-4-propyl-1,3-diox olane-2-yl]methyl]1H-1,2,4-triazole, in soil was investigated using lysimeters simulating a rice-paddy-soil conditions. Two lysimeters composed of different soil types, a sandy loam (lysimeter A) and silty clay (lysimeter B), were used. Propiconazole (Tilt 250^R EC) plus [U-¹⁴C]-propiconazole was applied over a two-year period to the soil surface of the lysimeters. Propiconazole fate in the lysimeters was assessed by measuring total radioactivity in the leachate, evolved ¹⁴CO₂, and ¹⁴C-residues in the soil and rice plants. The amounts of applied ¹⁴C in the leachate from lysimeter A were 4.4 and 5.2% in the first and second year, respectively. A background level of (0.00005% of applied) ¹⁴C in the leachate from lysimeter B was detected, suggesting negligible movement of the fungicide to groundwater in the silty clay soil. The amount of ¹⁴CO₂ evolved from lysimeter A accounted for 7.8 and 12.2% of applied ¹⁴C in the first and second year, respectively, whereas those from lysimeter B were 5.7 and 7.1%. Total ¹⁴C detected in the rice plants grown in lysimeter A were 7.3 and 9.8% of applied ¹⁴C in the first and second year, respectively, which compared to 3.0 and 7.6% in lysimeter B. Most of the applied ¹⁴C was detected in the top 10 cm soil layer, suggesting that propiconazole remains close to the soil surface after application in soil. Degradation products of propiconazole identified in the lysimeter soils were 1-[[2(2,4-dichlorophenyl)-2-(1,2,4-triazole -1-yl) ketone (DP-1), 1-(2,4-dichlorophenyl)-2-(1,2,4-triazole-1- yl) ethanol (DP-2) and 1-[[2(2,4-dichlorophenyl)-4-hydroxypropyl-1,3-dioxolane-2-yl]methyl]1H-1,2,4-triazole (DP-3 and DP-4).     

Mercury translocation in and evaporation from soil. III. quantification of evaporation of mercury from podzolized soil profiles treated with Hg Cl

Mercury evaporation from undisturbed iron‐humus podzol lysimeters was measured over 3 months after treatment with HgCl₂ spiked with radioactive ²⁰³Hg. The relative evaporation rate from HgCl₂ treated soils followed the sum of two exponential functions. Because evaporation asymptotically approaches zero with time, the integral of the fit curve represents the evaporative loss in percent of atmospheric deposition. For the soil investigated, about 5% of atmospheric Hg deposition was reemitted into the atmosphere. It is hypothesized that mercury evaporation can decrease the leaching of mercury in and from soil significantly; this effect is probably increasing with decreasing rain acidity or soil acidity. Mercury deposited as soluble salt remains susceptible to reemission to air for 300 d after incorporation into the soil matrix. Indications are found that Hg evaporation from soils in geological background areas predominantly derives from recent atmospheric Hg deposition and not from geological sources.     

A field lysimeter study of heavy metal movement down the profile of soils with multiple metal pollution during chelate-enhanced phytoremediation

The agricultural soils near a copper smelter in southeast China were found to be highly contaminated with Cu, Pb, Zn, and Cd. Metal migration from the soil to groundwater presents an environmental risk that depends on the physicochemical properties of the contaminated soils. Soil solution samples were obtained using lysimeters from a loam soil with multiple metal pollutions over a period of about 1 yr. A field lysimeter study was also conducted to examine the potential use of (S, S')-ethylenediamine-N, N'-disuccinic acid trisodium salt (EDDSNa3) in chelate-enhanced phytoremedation and to evaluate the leaching of heavy metals. The average heavy metal concentrations in the soil solution (without the addition of EDDS) were high (e.g., 0.15 mg Pb L(-1) at a 50-cm depth) compared to the upper limit for protection of groundwater in China, but varied during the sampling period. Cu concentrations were not correlated with pH or dissolved organic carbon (DOC), but Zn and Cd concentrations were related to soil solution pH. EDDS enhanced metal solubility in the soil, but plant metal uptake by Elsholtzia splendens Nakai did not increase accordingly. There may be an increasing risk of groundwater pollution by Cu and the EDDS enhanced phytoremediation technique needs to be carefully applied to minimize this side effect.     

Erythrocyte catalase activity in chronic renal failure patients and donors in the presence of metal lons

The effect of hemodialysis on erythrocyte catalase (CAT) activity was studied in chronic renal failure (CRF) patients. This enzyme was analyzed in vitro, and its activity throughout the incubation period was found to be 34% lower than in healthy donors. The influence of Al³⁺, Cu²⁺, and Ni²⁺ on CAT activity in donor's blood (in vitro) is also studied, for short incubation periods at trace levels of 2.5, 0.25, and 0.196 mM, respectively. With Al³⁺ and Cu²⁺, there is a decrease in the enzyme activity. With Ni²⁺, there is at first a similar decrease, followed by a recovery in activity up to control values.     

土壤蒸发和植被蒸腾对三江源退化高寒草甸蒸散的影响

蒸散(ET)主要由土壤蒸发(E)和植被蒸腾(T)组成,然而难以把E与T从陆地生态系统ET中区分开。为阐明位于青海省境内的三江源区(89°24′—102°23′E, 31°39′—36°16′N)高寒草甸E和T对生态系统ET的影响,利用小型蒸渗仪和微气象系统定量研究了三江源退化高寒草甸ET、E和T的变化,以及植被和环境因子对其的影响。结果表明:2017和2018年的ET分别为467.7 mm和479.2 mm,其中生长季(5—9月)约占72%,且E对生态系统ET的贡献(56%)大于T(44%),年降水量(P)的90%以上通过ET返回大气(ET/P> 90%)。根据生长季中不同植被覆盖度的蒸渗仪观测结果发现,ET随植被覆盖度的降低而增加。逐步回归分析表明,净辐射(R_n)是驱动生态系统ET、E、T最主要的因子;另外,E对饱和水汽压差(VPD)的响应更敏感,而T受空气温度(T_a)的影响更大;土壤含水量(SWC₅)对蒸散的影响相对较小,可能由于研究区降水相对较多的原因。结果说明,草甸退化将加剧土壤蒸发,进而导致生态系统散失更...     

Speciation analysis of nickel in soil solutions and availability to oat plants

Soil solutions were collected for speciation analysis of nickel from a pot experiment with oats. Oat plants (Avena sativa L.) were grown on 3 soils differing in total amount and origin of nickel (Ni) (Luvisol, LS with 28 mg kg^-1; sludge amended Luvisol, LS+SS with 32 mg kg^-1; Cambisol, CS with 95 mg kg^-1). Results were compared with those for soil solutions obtained from corresponding unplanted pots. Separation methods were used for characterization of size and charge distribution and stability of the Ni species. In addition, short-term experiments were performed on the uptake rates of Ni by oat plants from the different soil solutions as well as from nutrient solutions with increasing concentrations of a synthetic chelator.The Ni concentrations in the soil solutions of unplanted soils increased in the order: LS5000 g mol^-1) was the predominant form, whereas in the other soils the low-molecular-size cationic and chelated Ni species (500–1000 g mol^-1) dominated in the soil solution. In the short-term uptake studies, the uptake rates of Ni from the solutions decreased in the order: nutrient solution > soil solutions, and in the latter in the order: LS>LS+SS>CS, which was inversely related to the concentrations of dissolved organic carbon in the soil solutions.The results demonstrate that Ni availability to plants is not only affected by total concentration of Ni in the soil solution and the rate of replenishment from the solid phase, but also by Ni species, which can differ considerably between soil types.     

接种泡囊假单胞菌对土壤生物性质及A. corsicum吸收Ni的影响

采用室内模拟试验方法,研究了在水稻土、元江土和墨江土中添加泡囊假单胞菌（Pseulormanas vesicularis）后土壤中微生物种群数量、土壤酶活性和镍超积累植物Alyssum corsicum对土壤镍的富集效果.土壤接种泡囊假单胞菌70d后,水稻土中DTPA提取态镍较对照土中的明显减少、元江土和墨江土中的有所减少;土壤中细菌、真菌和放线菌数量增加,5种土壤酶活性提高.试验结果表明,水稻土、元江土、墨江土添加泡囊假单菌后植物地上部生物量较对照分别增加了29%、309%和43%,进而提高了A.corsicum自土壤中富集镍的效率：水稻土中增加54%,元江土中增加306%,墨江土中增加32%.泡囊假单胞菌这一新用途的发现,可为植物修复微生物制剂和基因工程菌的开发提供本土的微生物的菌种资源.     

Response of the root system of a winter wheat crop to waterlogging

This study was aimed at analysing and quantifying the response of the root system dynamics of a wheat crop to waterlogging. Two experiments were carried out in parallel: one under controlled conditions with semi-permanent water tables using lysimeters equipped with oxygen measurers, and the other under conditions of artificially drained plots by continually monitoring their hydraulic functioning. The root system was observed frequently using the root mapping method, and this made it possible to measure the growth of the root front, to estimate root densities, and infer growth indices from them. The results showed that the anoxic medium for wheat roots consisted of a water-saturated soil with an oxygen concentration of below a critical threshold estimated to be 0.12 mol m^–3 water. The results also showed that the area which was unfavourable to root growth corresponded to the water table topped with a capillary zone of approximately 6 cm. Once the critical threshold had been reached, it was the water-table duration that explained root behaviour and the first effects were perceptible after approximately 48 h. On the basis of these results, two stress variables were analysed: water-table duration in the root zone (WTD) and proportion of roots in the water table (RPWT). The RPWT variable gave the best results within the two experimental contexts. In the case of the permanent regime, this variable made it possible to consider the root proliferation observations made above the saturated zone. Equations linking the stress variable RPWT to the growth indices are proposed that offer new perspectives to modelling waterlogging effects.     

富营养化河水灌溉对稻田土壤氮磷养分贡献的影响——以太湖地区黄泥土为例

以太湖地区主要稻田土壤类型黄泥土为对象,利用当地富营养化河水对回填土柱和植稻原状土渗漏池进行模拟稻田灌溉试验,系统研究了灌溉水对稻田土壤氮磷营养的贡献.在回填土柱灌溉试验中,在试验初期,不同形态的氮素均有较高的淋失量,以后逐渐降低,表明初期淋失的氮素主要来自土壤,而不是灌溉河水.在整个水稻生长季,均观测到有可溶性有机氮淋失,表明富营养化河水灌溉条件下可溶性有机氮是稻田土壤主要的氮素淋失形态.在本试验中,磷素的淋失动态与氮素的淋失动态截然相反,淹水后很长一段时间内均没有土壤磷素淋失,但在淹水灌溉后期有大量的土壤磷素淋失损失,这可能是淹水后期土壤对磷的吸持已达到饱和状态,不能继续固持土壤中多余的磷所致.与回填土柱模拟灌溉淋洗试验相比,在当前供肥条件下,原状土渗漏池试验氮磷淋失量远低于回填土柱试验,而灌溉水对土壤氮磷养分的贡献远高于回填土柱.通过富营养化河水灌溉带入当季稻田的N量达到每公顷56.3 kg,其中有55.8 kg N可被土壤吸持和作物吸收,表明太湖地区稻田土壤对氮磷养分来说是一个环境友好的生态系统.在利用当地富营养化河水进行稻田土壤灌溉时可适量减少肥料施用量、优化氮磷肥料管理.     

Improving the Agronomy of Alyssum murale for Extensive Phytomining: A Five-Year Field Study

Large ultramafic areas exist in Albania, which could be suitable for phytomining with native Alyssum murale. We undertook a five-year field experiment on an ultramafic Vertisol, aimed at optimizing a low-cost Ni-phytoextraction crop of A. murale which is adapted to the Balkans. The following aspects were studied on 18-m² plots in natural conditions: the effect of (i) plant phenology and element distribution, (ii) plant nutrition and fertilization, (iii) plant cover and weed control and (iv), planting technique (natural cover vs. sown crop). The optimal harvest time was set at the mid-flowering stage when Ni concentration and biomass yield were highest. The application of N, P, and K fertilizers, and especially a split 100-kg ha^?1 N application, increased the density of A. murale against all other species. It significantly increased shoot yield, without reducing Ni concentration. In natural stands, the control of graminaceous weeds required the use of an anti-monocots herbicide. However, after the optimization of fertilization and harvest time, weed control procured little benefit. Finally, cropping sown A. murale was more efficient than enhancing native stands and gave higher biomass and phytoextraction yields; biomass yields progressively improved from 0.3 to 9.0 t ha^?1 and phytoextracted Ni increased from 1.7 to 105 kg ha^?1.     

A review on remediation technologies for nickel-contaminated soil

Abstract

With the rapid pace of industrialization and urbanization, the environmental safety of soil is a worldwide concern. In China alone, one-fifth of the arable land is reported to be contaminated with heavy metals including nickel. In this review, current research on nickel remediation, specifically the various remediation technologies including physical and chemical remediation methods, such as immobilization, soil washing, encapsulation, soil replacement, and electrokinetic methods; phytoremediation; and bioremediation, is summarized. Further, the mechanisms underlying the presented remediation technologies, along with their advantages and disadvantages, are discussed. The lacunae in available technologies for nickel remediation are also briefly discussed. The review concludes with a scheme for successful soil remediation.     

Nickel Exposure and its Effects

The aim of the study was to determine the nickel concentrations of soil and plant specimens taken from a rural area exposed to cement factory emissions and also to determine the blood concentrations and sensitivity conditions observed in humans residing in this rural area. The study was carried out in Çukurhisar, a town in Eski?ehir-Turkey, between May 2000 and March 2001. Beside the 108 soil (36 for control) and plant specimens, which were taken from 8 directions from the cement factory, blood samples of the individuals residing in this area were taken from 258 subjects (258 for control) following a physical examination, and patch tests were also applied. The nickel concentrations of the soil and plant specimens taken from different places in different directions of the factory were higher than in the control areas. The physical examination of subjects did not reveal results different from those of the control group except for the diagnosis of contact dermatitis. The analyses of venous blood samples showed that nickel concentrations were found to be within the reference values given for both groups, but higher in the subjects (p<0.001). According to the results of patch tests, sensitivity to nickel was found to be more frequent for the subject group than the control group (p<0.05). According to these results, clinical tools revealed no toxic effects for the subjects, except contact dermatitis. However, sensitivity to patch tests showed that this subject group has been affected compared to the control group and that this effect increased with age.     

镍污染对土壤微生物的生态效应

镍是高等植物和某些微生物必需的微量营养元素之一,在它们的生命活动中起着重要作用;但浓度较高时,也是一种极毒元素。大量的研究表明,镍污染土壤中微生物的生长、代谢、群落结构和种群多样性会受到不同程度的影响;微生物在长期受重金属威迫的环境中形成其适应性。利用微生物形成的这种适应机制,采用微生物技术治理重金属污染的土壤是可能的。本文还对镍污染土壤的微生物评价指标体系、土壤环境容量、微生物技术开发和综合治理技术开发等的进一步研究作了展望。     

冬小麦生长条件下土壤硝态氮淋洗的传递函数模拟和预报

观测了地中渗透计的土壤在 3种不同施肥量下冬小麦自播种至返青期硝态氮的淋洗动态 ,由试验资料获得了硝态氮在土壤中迁移时间的概率密度函数 ,进而运用传递函数模型对土壤排水出流液中的硝态氮浓度和淋洗量动态进行了数学模拟和预报。