溴氟菊酯的光解、水解与土壤降解

在实验室测定了溴氟菊酯的光解、不同ｐＨ条件下的水解以及在太湖水稻土、江西红壤与东北黑土等３种不同土壤中的降解。试验结果表明：在３００Ｗ低压汞灯下，溴氟菊酯的水相溶液与其石油醚相济液中的光解均呈二级反应动力学方程，光解半衰期分别为１３．７与９．４ｍｉｎ；在ｐＨ为５，７，９的缓冲溶液中其水解半衰期分别为１５．６，８．３与４．２ｄ；在３种不同土壤中的降解半衰期为４．８～８．８ｄ。     

毒草胺在环境中的降解特性研究

毒草胺是一种被广泛应用的农药,其在环境中的降解特性备受关注。文章采用室内模拟试验方法,研究了毒草胺的光解、水解及土壤降解特性。研究结果表明,毒草胺在光强为2 370l x、紫外强度为13.5μW.cm-2的人工光源氙灯条件下,光解半衰期为2.5 h,较易光解。25℃时在pH值为5.0、7.0和9.0的缓冲水溶液中,降解半衰期分别为147.5、173.3和239.0 d;50℃时半衰期分别为15.2、27.0和42.3 d,结果显示温度对其降解速率影响较大,温度增加,水解速率明显加快,水解半衰期降低约6~10倍。该药在江西红壤中降解半衰期为46.5 d,在太湖水稻土、东北黑土中降解半衰期分别为6.4和7.9 d,比较容易降解,主要为微生物降解。结果表明毒草胺在水体中具有一定的稳定性,尤其在避光条件下难以降解。但在土壤中,比较容易被微生物降解。     

Toxic elements leaching in different soils affected by the spill from the aznalcollar pyrite mine (Sevilla,Spain)

A study has been made of the leaching of Cd, Zn, Pb, Cu, Tl and As in three representative soils of the zone affected by the spill from a pyrite mine in Aznalcollar (Sevilla, Spain) employing packed soil columns. According to the breakthrough and cumulative leaching curves, the relative mobilities of the different toxic elements in the columns are as follows: Tl > Cd > Zn > As > Cu > Pb. The results also show that the soils themselves have a good capacity for immobilizing the soluble fraction of the elements from the spilled mud, this capacity varying as follows: clayey soil with a high carbonate content > clayey soil with a moderate carbonate content > sandy‐clay loam soil with a low carbonate content. The results obtained in the work are a valuable contribution to the necessary assessment of the impact of the toxic spill on underground waters.     

吡虫啉的光解水解和土壤降

在实验室测定了吡虫啉的光解、不同ｐＨ条件下的水解与在东北黑土等３种不同土壤中的降解。试验结果表明，在３００Ｗ低压汞灯下，吡虫啉水相溶液的光解呈一级反应动力学反应，光解半衰期为６．８１ｈ；在ｐＨ５、ｐＨ７、ｐＨ９的缓冲溶液中的水解半衰期分别为３０．６、１３．６与８．０ｄ；在东北黑土、太湖水稻土和江西红壤中的降解半衰期分别为１０．７、１１．１和４．１ｄ。     

Mobility and adsorption of the triketone herbicide mesotrione in the soil of corn crops

The triketone herbicide mesotrione has been applied pre‐emergence at the dose of 150 g a.i. ha^?1 on corn fields grown within the same period of time at different sites on clay, loam, sandy loam or sandy soils. During the crops and one month after the corn harvest, the mobility of mesotrione has been measured in the 0–20 cm surface soil layer, soil samples being taken in the 0–2,2–4,4–6,6–8, 8–10, 10–15 and 15–20 cm surface soil layers. During the first month after the treatment, mesotrione remained in the 0–2 cm surface soil layer. Thereafter, mesotrione was at a higher concentration in a 2 cm‐thick soil layer which progressively moved down in the clay, loam and sandy loam soils. In the sand soil, mesotrione moved down as a uniform diffusion, its concentration being similar in all the 2 cm‐thick layers of the 0–10 cm soil surface layer. Low mesotrione residues (6–10 ug kg^?1 dry soil) attained the 10–15 cm layer faster in the clay and sand soils than in the loam and sandy loam soils. Mesotrione was not detected in the 15–20 cm soil layer of the loam and sandy loam soils, but well in the sand and clay soils. In the soils of the corn crops mesotrione thus mainly remained in the 0–10 cm surface soil layer. This low mobility and depth of penetration conjugated to the rate of mesotrione soil degradation explain why there was no movement of mesotrione toward the deeper soil layers. The adsorption of mesotrione was greatest on the soils recently treated with organic fertilizers, and having a loam or sandy loam texture. The adsorption coefficients explained the lower mobility and the greatest persistence of mesotrione in these soils.     

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。     

两种土壤中对硝基氯苯被Fe~0还原的对比研究

利用零价铁(Fe~0)还原技术修复受对氯硝基苯(p-CNB)污染的土壤,研究常温常压下松砂土和中壤土两种不同土壤的理化性质对还原反应的影响.结果表明:Fe0能有效还原松砂土和中壤土中的p-CNB,生成对应的苯胺化合物,降低毒性;当土壤中p-CNB的含量约为2.5×10~(-6)mol·g~(-1),Fe~0用量为25 mg·g~(-1),反应体系中水分含量为0.75 mL·g~(-1)时,于25℃反应2 h后,松砂土和中壤土中p-CNB的还原率均超过93%;还原反应在中壤土中进行得较快.污染物在土壤中的老化时间对Fe~0还原降解效果影响很小,而土壤粒径、土壤是否灭菌以及土壤有机质含量等因素则对还原有较明显影响;还原降解反应在没有灭菌、有机质含量较高且粒径偏小的壤土中进行得最彻底.     

Dissipation of the triketone mesotrione herbicide in the soil of corn crops grown on different soil types

The new triketone herbicide mesotrione corresponds to the older sulcotrione in which the 2‐chloro benzoyl substituent is replaced by a nitro group, generating an herbicide of greater efficiency and a broader spectrum of activity. Mesotrione has been applied within the same 15 days period pre‐emergence at the rate of 150gha^‐1 to four corn crops made at different sites located 40 km apart in Belgium and of soils of different textures, but similar pH and organic matter (old humus) contents. The mesotrione soil half‐life in the 0–10 cm surface soil layer (which contained more than 90% of the residue) was 50 days in loam soil (at Zarlardinge), 41 days in sandy loam soil (at Melle) and in clay soil (at Koksijde), and 34 days in sandy soil (at Zingem). The cumulative effects of the recent organic fertilizer treatments and of the soil texture could explain the differences between the soil half‐lives. The time for the 90% dissipation of mesotrione was between 3.6 (in the sandy soil) to 4.7 months (in the sandy loam, loam and clay soils). The low mesotrione soil residues remaining after the corn harvest should disappear with the usual heavy rains in autumn, and the tilling which precedes the following crop and dilutes the mesotrione soil residue. These low mesotrione soil residues thus should have no phytotoxicity toward the following crop, especially at the lower application dose of 100 g mesotrione ha^‐1 used in practice.     

Relationships between distributions of longevous population and trace elements in the agricultural ecosystem of Rugao County,Jiangsu, China

Soil, plant, and water, as well as trace elements they contain, can influence human health through the food chain. A survey was conducted on distributions of trace elements in soils, plants, and drinking water in Rugao County, Jiangsu Province, China, an agricultural area with a high level of centenarians and nonagenarians. The ratio of people over 90 years old per 100,000 inhabitants (90-rate) based on village (about 4,000 residents in 4 km²) was correlated with trace elements in soil, drinking water, and rice by means of correlation analysis and/or principal component analysis. Although the average 90-rate in the whole area was as high as 277, the rates were not uniform across the entire region. The 90-rate in the area of loamy and strongly-developed Anthrosols and Cambosols was about 330, significantly higher than the 255 in the areas of sandy and strongly-developed Cambosols and of clayey and weakly-developed Cambosols. The concentrations of available Se, B, Ni, and Mo in soils of the area with the high 90-rate were markedly greater than those in the area with the low 90-rate. This was demonstrated by highly positive correlations between the 90-rate and available Se (r = 0.33), B (r = 0.21), Ni (r = 0.17) and Mo (r = 0.17) at the p < 0.01 level and high loadings of available Se (0.851), B (0.535), Ni (0.594) and Mo (0.394) in the longevous factor. Similar relationships between the available elements in soils and elements in water and rice were found. These results suggest that: (1) the available forms of elements in soil were more crucial to elemental bio-availability in the ecosystem and human health than total elements in soil; and (2) the element association above might have affected the 90-rate positively and could be an important environmental geochemical factor influencing the longevity of humans.     

Sediment texture and nutrients of Arasalar estuary, Karaikkal, south-east coast of India

Sediment samples were collected for texture, composition and nutrient such as organic carbon, total nitrogen and total phosphorus for a period of two years from three stations in Arasalar estuary. The sediment temperature, pH and nutrients were higher during summer season and lower during monsoon season. At station 1, sediment texture was loamy sand during summer and premonsoon season. At station 2, clay type soil was recorded. Whereas, at station 3, clay was observed in summer and premonsoon and then it shifted to sandy loam type soil during monsoon. Sediment nutrients were lower than that of values of various ecosystem of India.     

农药在环境中的水解机理及其影响因子研究进展

农药的水降解与其在环境中的持久性是密切相关的,它是影响农药在环境中的归宿机制的重要依据之一,也是评价农药在水体中残留特性的重要指标。近些年来,国内外不少学者对农药尤其是有机磷、氨基甲酸酯、拟除虫菊酯和磺酰脲类等的水解进行了大量研究,其内容涉及到农药水化学降解机理及其各种因子如pH值、温度和黏土矿物等对农药水解的影响等,并取得了很多新的进展。但是所有这些研究主要集中于实验室内,而对其自然环境中各因子的贡献及其水解机制的了解则相对较少。今后应加强农药在自然条件下的水解动力学与机理以及黏土矿物和腐殖酸对农药在水体中的催化水解研究,以更好地评价农药在环境中的行为与归宿,为农药的合理使用提高科学依据。     

Sorption of tetracycline to sediments and soils: assessing the roles of pH,the presence of cadmium and properties of sediments and soils

Batch sorption experiments were conducted to evaluate the sorption behavior of tetracycline (TC, H₃L) on sediments and soils in the presence and absence of cadmium (Cd), as affected by pH and properties of sediments and soils. The results indicated stronger nonlinearity and higher capacity of TC sorption on sediments than on soils. Sorption of TC also strongly depended on environmental factors and sediment/soil properties. Lower pH facilitated TC sorption through a cation exchange mechanism, which also took place at pH values above 5.5, where TC existed as a zwitterion (H₂L⁰) or anions (HL^- and L^2-). When pH was above 7, however, ligand-promoted dissolution of TC might occur due to TC weakening the Al-O bond of aluminum oxide and the Fe-O bond of iron oxide. Natural organic matter (NOM) plays a more important role in TC sorption than cation exchange capacity (CEC) and clay contents. The presence of Cd (II) increased TC sorption on both sediments and soils, which resulted from the decrease of equilibrium solution pH caused by Cd²⁺ exchange with H⁺ ions of sediment/soil surfaces. The increase of TC sorption was also related to the formation of TC-Cd complexes, where Cd²⁺ acted as a bridge between the sediment/soil and TC.     

Sorption and desorption of pymetrozine on six Chinese soils

Pymetrozine is a selective insecticide with a unique chemical structure and mode to control hemipteran and homopteran. While pymetrozine has brought great benefits to crop production by killing insects, its residues in soil may have a detrimental effect on environment. Therefore, it is of great importance to investigate its behaviors in soil. In this study, the sorption and desorption of pymetrozine on six Chinese soils were investigated using a batch equilibrium approach to understand its mobile behavior in the soils. Both sorption and desorption isotherms of pymetrozine were in good agreement with the Freundlich model. The sorption coefficient K_F varied between 3.37 and 58.32 mL∙g⁻¹ and the sorption isotherms were nonlinear, with 1/n ranging from 0.57 to 0.91. A regression equation was proposed to predict the sorption of pymetrozine on six different soil samples: log K_F = 4.3708 − 4.5709 × log (pH in 0.01mol·L⁻¹ CaCl₂) + 0.4700 × log OC% + 0.0057 × sand (%) + 0.0022 × CEC(clay), with R² = 0.9982. The organic carbon content of soil positively affected the sorption of pymetrozine, but soil pH had a negative effect on the sorption. Additionally, effects of CaCl₂ concentration, soil to solution ratio and pesticide form were investigated. The sorption was promoted with an increase in soil to solution ratio and a decrease in CaCl₂ concentration. The possible variation of the five formulated products of pymetrozine was also investigated.     

Sorption and bioavailability of arsenic in selected Bangladesh soils

The bioavailability of arsenic (As) in the soil environment is largely governed by its adsorption–desorption reactions with soil constituents. We have investigated the sorption–desorption behaviour of As in four typical Bangladeshi soils subjected to irrigation with As-contaminated groundwater. The total As content of soils (160 samples) from the Laksham district ranged from <0.03 to approximately 43 mg kg⁻¹. Despite the low total soil As content, the concentration of As in the pore water of soils freshly irrigated with As-contaminated groundwater ranged from 0.01 to 0.1 mg l⁻¹. However, when these soils were allowed to dry, the concentration of As released in the pore water decreased to undetectable levels. Remoistening of soils to field moisture over a 10-day period resulted in a significant (up to 0.06 mg l⁻¹) release of As in the pore water of soils containing >10 mg As kg⁻¹ soil, indicating the potential availability of As. In soils containing <5 mg As kg⁻¹, As was not detected in the pore water. A comparison of Bangladeshi soils with strongly weathered long-term As-contaminated soils from Queensland, Australia showed a much greater release of As in water extracts from the Australian soils. However, this was attributed to the much higher loading of As in these Australian soils. The correlation of pore water As with other inorganic ions (P, S) showed a strongly significant (P < 0.001) relationship with P, although there was no significant relationship between As and other inorganic cations, such as Fe and Mn. Batch sorption studies showed an appreciable capacity for both As^V and As^III sorption, with As^V being retained in much greater concentrations than As^III.     

北平热带桐柏山地土壤特性及其合理利用

本文阐明了豫南桐柏山北坡土壤形成的自然条件,并以三个代表性剖面为对象,研究了土壤的发生特性。结果表明,土壤具有淡色或暗色表层,质地多为砂质壤土和砂质粘壤土,土体有一定的发育,pH呈酸性至微酸性,盐基饱和度多在80％左右,土壤粘粒的硅铝率均>3.4,粘土矿物组成主要为水云母、高岭石、蛭石。土壤类型随海拔高度增加而有规律地变化,基带土壤为黄棕壤,中部为暗黄棕壤,棕壤则分布在1000m以上。文章还提出了土壤资源合理利用的基本途径,即以林为主,在搞好水土保持工作的同时,实行多种经营措施相结合的综合开发体系。     

Temporal changes of Collembola population and alterations of life history parameters and acetylcholinesterase and superoxide dismutase activities in Cyphoderus javanus (Collembola) as biomarkers of fly ash pollution in lateritic soil

Fly ash is applied in agricultural fields to improve soil quality and crop yield; however, there are concerns regarding environmental hazards and toxicity to ecologically important soil organisms. The soil microarthropod fauna is a vital component of detritus food web, and major groups like Collembola are sensitive indicators of soil quality; however, information is scanty on their biomarker potentials against xenobiotics in tropical soils. The present study was aimed to evaluate temporal changes of Collembola population in fly ash amended field plots, and assess the biomarker potentials of life history parameters and biochemical responses such as acetylcholinesterase (AChE) and superoxide dismutase (SOD) activities in Cyphoderus javanus Borner (Collembola, Insecta), exposed to fly ash treated soil in microcosms. The field study using 5% (50 t ha^?1) and 20% (200 t ha^?1) doses of fly ash revealed dose-dependent and persistent decline in the density and relative abundance of Collembola population in sandy loam lateritic soil. The microcosm experiments showed negligible lethal effect of fly ash on C. javanus, but major life history parameters namely survival success, fecundity, and molting were significantly inhibited by fly ash treatments. The activity of AChE was downregulated, whereas activity of SOD was upregulated within 7 days of exposure of C. javanus to fly ash treated soil. These biological and biochemical parameters in Collembola are potential biomarkers, and therefore, the effects of fly ash are significant in C. javanus, an ecologically relevant species in the tropical soils of India.     

Biogeochemical transfer and dynamics of iodine in a soil–plant system

Radioactive iodide (¹²⁵I) is used as a tracer to investigate the fate and transport of iodine in soil under various leaching conditions as well as the dynamic transfer in a soil–plant (Chinese cabbage) system. Results show that both soils (the paddy soil and the sandy soil) exhibit strong retention capability, with the paddy soil being slightly stronger. Most iodine is retained by soils, especially in the top 10 cm, and the highest concentration occurs at the top most section of the soil columns. Leaching with 1–2 pore volume water does not change this pattern of vertical distributions. Early breakthrough and long tailing are two features observed in the leaching experiments. Because of the relatively low peak concentration, the early breakthrough is really not an environmental concern of contamination to groundwater. The long tailing implies that the retained iodine is undergoing slow but steady release and the soils can provide a low but stable level of mobile iodine after a short period. The enrichment factors of ¹²⁵I in different plant tissues are ranked as: root > stem > petiole > leaf, and the ¹²⁵I distribution in the young leaves is obviously higher than that in the old ones. The concentrations of ¹²⁵I in soil and Chinese cabbage can be simulated with a dual-chamber model very well. The biogeochemical behaviors of iodine in the soil-cabbage system show that cultivating iodized cabbage is an environmentally friendly and effective technique to eliminate iodine deficiency disorders (IDD). Planting vegetables such as cabbage on the ¹²⁹I-contaminated soil could be a good remediation technique worthy of consideration.     

The effects of soil properties on the turbidity of catchment soils from the Yongdam dam basin in Korea

Environmental concerns have been raised that suspended solids in turbid water adversely affect human health, and that their removal increases in the cost of water treatment. The Yongdam dam reservoir, located in the southwestern region of Korea, is severely affected by inflowing turbid water after storms. In this study, soil samples were collected from 37 sites in the Yongdam upstream basin to investigate mineralogical and environmental factors associated with the turbidity potential of soils in water environments. Turbidity potential was estimated by measuring the turbidity of soil-suspension solutions after settling for 24 h. The mineralogy of the soils was dominated by four minerals—quartz, microcline, albite, and muscovite—with lesser amounts of hornblende, chlorite, kaolinite, illite, and mixed layer illite. The quartz content was the most variable of the soil mineralogy among the collected samples. Principal-components analysis (PCA) was used to examine relationships between turbidity potential and other soil properties. The variables considered in the PCA included turbidity potential, quartz content, albite content, mean size of soil particles, clay content, clay mineral content, zeta potential, conductivity, and pH of the soil-suspension solution. The first two components of the PCA explained 52% of the overall variation of the selected variables. The first component was possibly explained by physical properties such as the size of the soil particles; the second was correlated with chemical properties of the soils, for example dissolution and extent of weathering. Closer examination of the PCA results revealed that the quartz content of the soils was negatively correlated with their turbidity potential. A linear correlation (r = 0.63) was obtained between measured turbidity potential and that predicted using multiple regression analysis based on the content of clay-sized particles, clay minerals, and quartz, and the conductivity of the soil-suspension solution.     

改性土壤对模拟含硝基苯废水的吸附

研究了季铵盐阳离子表面活性剂四甲基铵离子（TMA）和十六烷基三甲基铵离子（HDTMA）改性的土壤（黑土、黄棕壤、红壤）对水中硝基苯的吸附作用。结果表明：改性土壤和改性土壤均能吸附水中的硝基苯。但改性土壤对水中硝基苯的吸附能力明显高于未改性土壤。改必土壤吸附硝基苯能力的顺序为1CEC－HDTMA黑土＞1CEC－HDTMA黄棕壤＞0．7 CEC－HDTMA黄棕壤＞1 CEC－HDTMA红壤＞0．7 CEC－HDTMA红壤＞1 CEC－TMA黄棕壤＞1 CEC－TMA红壤。未改性土壤和HDTMA改性土壤对硝基苯的吸附通过分配来进行，吸附等温线可用Henry方程表示，其lgKSOM为2．27，lgKHDTMA为2．87。     

Effects of β-cyclodextrin on adsorption and desorption of carbofuran in soils of divergent texture

Laboratory studies were conducted to determine the adsorption/desorption equilibrium of carbofuran between four divergently textured soils and distilled water and an aqueous solution of 0.01?mol?L^?1 β-cyclodextrin using a batch equilibrium technique. The determined adsorption isotherms for silt loam soils were of L-shaped, for sandy loam soil S-shaped, in agreement with a Freundlich isotherm. In the presence of β-cyclodextrin, the adsorption of carbofuran to the four soils was lower than with distilled water. Positive hysteresis was observed in all soils with distilled water, negative hysteresis when using a solution of β-cyclodextrin as desorbent. The results indicate the potential use of β-cyclodextrin for remediation of pesticide-contaminated soils.