南充农村土壤中有机氯农药残留现状分析

本研究以四川省南充市某农村土壤为研究对象,于2010年和2011年连续两年对土壤中有机氯农药(HCH,DDT)残留情况进行了定点监测。研究结果表明,试区土壤HCHs在2011年基本未检出。两年的DDTs的检出率均为100%。OCPs主要残留物为p,p’-DDE,占残留总量75%以上。不同利用类型土壤中有机氯残留总量排序为:菜地>重点污染场地>基本农田>居民聚集区。所有土壤样品中的HCHs含量均达到国家《土壤环境质量标准》(GB15618-1995)一级标准(<0.05mg/kg),DDTs含量均达到二级标准(<0.50mg/kg)。残留污染较轻。     

成都市人乳中有机氯农药蓄积水平调查研究

有机氯农药666,DDT以其高效、低毒、杀虫谱广,成本低,使用方便等特点,从本世纪40年代始即广泛使用于农业生产及日常生活方面,到60年代末已成为世界上产量最高,用量最大的农药。但这类农药性质十分稳定,不易分解,在环境     

山东聊城市表层土壤有机氯农药残留研究

2008年麦收期间以网格布点法采集了聊城市137个土壤表层样品，利用ASE萃取技术，采用GC-ECD方法测定了样品中六六六（BHCs）、滴滴涕（DDTs）、六氯苯、艾氏剂、狄氏剂、异狄氏剂和七氯的检出率和残留量，并对土壤质量状况做了评价。结果表明，土壤中DDTs的检出率高达94.1％，其他6种有机氯农药（OCPs）均有不同程度检出。OCPs总残留量平均值为145.35μg／kg，其中DDTs占88.58％，是残留OCPs的主要成分。全部样点中BHCs的单因子污染指数Pi最大值为0.1，土壤未受BHCs污染；95％的样点中DDTs的Pi值小于1，土壤中DDTs含量未超标，而3％的样点Pi值小于2，土壤属轻度污染，2％的样点Pi值大于2，土壤属重度污染。     

成都市人乳中有机氯农药蓄积水平调查研究

有机氯农药666,DDT 以其高效、低毒、杀虫谱广,成本低,使用方便等特点,从本世纪40年代始即广泛使用于农业生产及日常生活方面,到60年代末已成为世界上产量最高,用量最大的农药。但这类农药性质十分稳定,不易分解,在环境中逐渐积累,并通过生物富集和食物链作     

杭州城区蔬菜地农药残留现状与评价

采用加速溶剂萃取,气相色谱-质谱法测定了杭州市城区蔬菜地中农药残留量,并进行了评价。结果表明：杭州市城区蔬菜地中有机氯类、有机磷类、拟除虫菊酯类农药残留量为ND～0.19mg·kg^-1、ND～0.238mg·kg^-1、ND～0.013mg·kg^-1,检出率为52.4%、33.3%和28.6%。其中有机氯类农药达到国家土壤环境质量标准（GB15618—1995）二级以上,符合无公害蔬菜产地环境要求;根据加拿大残留限量标准评价有机磷类农药,超标率为14.3%;拟除虫菊酯类农药对土壤造成的污染不论是残留量还是检出率都小于前2类农药。     

关中西部某铅锌冶炼区周边土壤重金属污染纵向分布规律及生态风险评价

为了了解铅锌活动对深层土壤的污染情况,以关中西部某铅锌冶炼区周边土壤作为研究对象,通过室外采样调查和和室内样品分析,检测样品中主要重金属元素的含量以及纵向分布规律,并对该地区的重金属污染情况进行评价。结果表明:该铅锌冶炼区周边土壤中Pb、Zn、Cu、Cd、Cr、Ni的平均含量分别为28.92、86.72、26.02、0.31、70.01和32.40mg/kg,均高于陕西省土壤元素背景值。在纵向的60~80cm土层中Pb、Zn、Cd、Cr重金属元素含量都已经超过陕西土壤背景值。评价结果表明该冶炼区周边土壤中Cd元素已达到中度污染,土壤污染程度达到中等,生态风险强烈,因此该铅锌冶炼区周边土壤存在一定的生态风险。     

沈阳市道路绿化带土壤污染现状调查分析

选择沈阳市内不同道路绿化带土壤进行现状调查与分析,分别在5个区域,各布设3个采样点,分析测定土壤中的p H,阳离子交换量,汞、砷、铅、镉等元素以及DDT、六六六有机项目的含量。结果表明,总体上北部地区镉、汞、铅、DDT、六六六含量都较低,而南部地区含量则较高;各种元素中铅浓度相对较高。     

汕头地区农业生态系统中有机氯农药的研究

有机氯农药（Organochlorine Pesticides,OCPs）是一类由人工合成的杀虫广谱、毒性较低、残效期长的化学杀虫剂。本文以汕头市为研究区域,探讨了土壤OCPs的残留现状和特征,并对该区的土壤进行了环境质量评价和初步的生态风险评价。结果表明：（1）汕头地区土壤中OCPs的检出率高达99.13％,OCPs残留量的平均值是113.37 ng·g^-1,主要的OCPs污染物为DDTs和硫丹类;南澳县OCPs残留量平均值最高（174.68 ng·g^-1）,其次为龙湖区,濠江区含量平均值最低（69.24 ng·g^-1）;（2）与国内外一些地区土壤中OCPs的残留量对比,本研究区域土壤中的OCPs处于中等污染残留水平;与美国马里兰州标准、纽约州可容许的土壤浓度标准和我国的土壤环境质量标准相比较,OCPs基本没有超标;（3）本研究地区土壤存在较高的生态风险,OCPs可能对环境造成一定的危害,其中生态风险最高的是DDTs,BHCs的生态风险较低。     

土壤As动态影响下枸杞质量评价及环境风险预测

选择柴达木盆地诺木洪农场3种类型农田进行20 cm表层土壤砷（As）含量检测。第1种为新开垦原生地,第2种为20年耕种地,第3种为50年耕种地,检测As含量分别为16.29、14.90、14.04 mg·kg^-1。3种土壤As含量均达到无公害食品标准（25 mg· kg^-1）和绿色食品标准（20 mg·kg^-1）。多年耕种并没有造成农田表层土壤As积累。农田灌溉用河水中未检出As。生产中使用的22种农药、肥料均检测到As,其中15种杀虫剂、杀真菌剂、除草剂、植物激素等,每年输入土壤As 4513.59 mg·hm^-2;7种肥料每年输入土壤As 258015.24 mg·hm^-2。施肥是土壤中As输入的重要来源,最主要的输入源是磷酸二铵,占到50％;其次为复合肥、鸡粪和有机肥。每年随作物输出As总量为4380 mg·hm^-2。模拟田间灌溉,进行土壤柱淋漓试验,农田20 cm表层土壤每年随灌溉淋漓输出As为245230.65 mg·hm^-2,这与随着肥料、农药输入量几乎相等。表层土壤As处在一个输入、输出相对稳定的动态平衡状态。从土壤中输出的As,随灌溉水输入到水系统中,继而造成水系统As的积累,最终将影响到地区农业的可持续发展。     

环境专家对《绵阳地区土壤及主要粮油产品中有机氯农药残留量调查研究》成果进行鉴定

绵阳地区科委和绵阳地区城乡建设环境保护局于1984年5月22日至23日,在绵阳市主持召开了由绵阳地区环境科研监测站承担完成的《绵阳地区土壤及主要粮油产品中有机氯农药残留量调查研究》课题技术鉴定会。参加会议的有中国环境监测总站,回川省科学技术委员会成果办、回川省城乡建设环境保护厅、四川大学、成都科技大学、四川农学院、四川师范     

Soil mixing to decrease surface stratification of phosphorus in manured soils

Continual applications of fertilizer and manure to permanent grassland or no-till soils can lead to an accumulation of P at the surface, which in turn increases the potential for P loss in overland flow. To investigate the feasibility of redistributing surface stratified P within the soil profile by plowing, Mehlich-3 P rich surface soils (128-961 mg kg(-) in 0-5 cm) were incubated with lower-P subsoil (16-119 mg kg(-1) in 5-20 cm) for 18 manured soils from Oklahoma and Pennsylvania that had received long-term manure applications (60-150 kg P ha(-1) yr(-1) as dairy, poultry, or swine manure for up to 20 yr). After incubating a mixture of 5 g surface soil (0- to 5-cm depth) and 15 g subsoil (5- to 20-cm depth) for 28 d, Mehlich-3 P decreased 66 to 90% as a function of the weighted mean Mehlich-3 P of surface and subsoil (i.e.. 1:3 ratio) (r2 = 0.87). At Klingerstown, Northumberland County, south central Pennsylvania, a P-stratified Berks soil (Typic Dystrochrept) (495 mg kg(-1) Mehlich-3 P in 0- to 5-cm depth) was chisel plowed to about 25 cm and orchardgrass (Dactylis glomerata L.) planted. Once grass was established and erosion minimized (about 20 wk after plowing and planting), total P concentration in overland flow during a 30-min rainfall (6.5 cm h(-1)) was 1.79 mg L(-1) compared with 3.4 mg L(-1) before plowing, with dissolved P reduced from 2.9 to 0.3 mg L(-1). Plowing P-stratified soils has the potential to decrease P loss in overland flow, as long as plowing-induced erosion is minimized.     

原油在土壤中迁移及降解的研究

为了解原油在土壤中淋滤及降解的规律，剖析了大庆老油田开发区贮油池土壤含油状况，进行了自然植被不同类型土壤的浇油、室内原油淋滤模拟及栽培试验。结果表明：贮油池土壤原油淋滤深度绝大部分集中在0～30cm，以下原油明显减少（除沙化土壤外）；盐碱土集中在0～10cm；草甸黑钙土集中在0～50cm；柱内油水混合渗透试验，80％集中在0～20cm；原油覆盖土壤表面时清水淋渗较弱，在0～20cm内残留94％；加原油的土壤降解试验，平均降解59．92％，范围为53．94％～62．25％，盆栽试验平均降解61．99％，范围为55.12％～70．68％。     

Heavy metals distribution in an Iowa suburban landscape

This study investigated the degree to which human activities through urbanization influence heavy metal concentrations in a suburban landscape in Ankeny, IA. Residential areas from different years in nine time periods of development were identified from aerial photos. Soil cores were collected from the center of the front yard of 10 randomly selected homes. Cores were subdivided into 0- to 5-, 5- to 10-, and 10- to 20-cm increments from a composite of five cores. The soils were analyzed for organic C, pH, and total Cd, Co, Cr, Cu, Ni, Pb, and Zn. Results showed that organic C increased and pH decreased with time, and that there was a general decreasing trend in heavy metal concentrations from the pre-1939 period until 1983-1990, after which there was a sharp increase in the concentrations of most of the metals. The mean Cu concentration ranged from 21 mg kg(-1) for the pre-1939 time period of development to 14.9 mg kg(-1) for the recent period of development (2003-2005). Nickel concentrations increased significantly with depth with means of 21.3 mg kg(-1) at depth 0 to 5 cm, 22.5 mg kg(-1) at depth 5 to 10 cm, and 23.0 mg kg(-1) at depth 10 to 20 cm. The concentrations of heavy metals were significantly intercorrelated, except Zn, suggesting their coexistence as mineral constituents or common contamination source. The concentrations of Cu and Pb in some locations could be due to anthropogenic inputs or higher organic matter content in soils adjacent to older homes. There appears to have been a source that caused an increase in Cd, Cr, Co, Cu, Pb, and Ni concentrations in soil adjacent to homes built between 1983 and 1990.     

Denitrification potential in relation to lithology in five headwater riparian zones

The influence of riparian zone lithology on nitrate dynamics is poorly understood. We investigated vertical variations in potential denitrification activity in relation to the lithology and stratigraphy of five headwater riparian zones on glacial till and outwash landscapes in southern Ontario, Canada. Conductive coarse sand and gravel layers occurred in four of the five riparian areas. These layers were thin and did not extend to the field-riparian perimeter in some riparian zones, which limited their role as conduits for ground water flow. We found widespread organic-rich layers at depths ranging from 40 to 300 cm that resulted from natural floodplain processes and the burial of surface soils by rapid valley-bottom sedimentation after European settlement. The organic matter content of these layers varied considerably from 2 to 5% (relic channel deposit) to 5 to 21% (buried soils) and 30 to 62% (buried peat). Denitrification potential (DNP) was measured by the acetylene block method in sediment slurries amended with nitrate. The highest DNP rates were usually found in the top 0- to 15-cm surface soil layer in all riparian zones. However, a steep decline in DNP with depth was often absent and high DNP activity occurred in the deep organic-rich layers. Water table variations in 2000-2002 indicated that ground water only interacted frequently with riparian surface soils between late March and May, whereas subsurface organic layers that sustain considerable DNP were below the water table for most of the year. These results suggest that riparian zones with organic deposits at depth may effectively remove nitrate from ground water even when the water table does not interact with organic-rich surface soil horizons.     

宁夏灌区不同类型农田土壤氮素累积与迁移特征

在宁夏灌区选择设施菜田（n=4）和水旱轮作大田（n=4）,通过田间多点取样观测和室内分析的方法,研究了2种类型农田土壤氮素累积与分布特点,以及其迁移对浅层地下水的影响。结果表明,设施菜田0~150 cm土壤剖面溶解性总氮（TSN）、硝态氮（NO3--N）和溶解性有机氮（SON）含量都显著高于大田,前者分别是后者的1.5~5.6、1.5~3.4倍和1.6~9.8倍。设施菜田土壤氮素主要累积在0~5 cm和5~20 cm土层,而大田主要在40~100 cm土体。设施菜田和大田土壤溶解性总氮占全氮比例分别在5.4%~11.5%和2.2%~4.9%之间,前者的淋失风险较高。设施菜田各形态氮素累积量表现为SON＆gt;NO3--N＆gt;NH4＋-N,大田为NO3--N＆gt;SON＆gt;NH4＋-N。设施菜田浅层地下水中TSN、NO3--N和SON含量也都显著高于大田,前者平均含量分别是后者的9.5、13.8倍和7.0倍。因此,硝态氮和溶解性有机氮都是2种类型农田氮素累积的主要形态,也是浅层地下水污染的重要来源。     

Relationships between phosphorus levels in soil and in runoff from corn production systems

Phosphorus-enriched runoff from cropland can hasten eutrophication of surface waters. A soil P level exceeding crop needs due to long-term fertilizer and/or manure applications is one of several potential sources of increased P losses in runoff from agricultural systems. Field experiments were conducted at locations representative of three major soil regions in Wisconsin in corn (Zea mays L.) production systems to determine the effect of tillage, recent manure additions, soil P extraction method, and soil sampling depth (0-2, 0-5, and 0-15 cm) on the relationship between soil test P level and P concentrations in runoff. Runoff from simulated rainfall (75 mm h(-1)) was collected from 0.83-m2 areas for 1 h after rainfall initiation and analyzed for dissolved phosphorus (DP), total phosphorus (TP), and sediment. The DP fraction of the TP concentration in runoff ranged from 5 to 17% among sites with most of the variation in TP due to varying sediment concentration on the well-drained silt loam soils and to soil test P level on the poorly drained silty clay loam soil. In 213 observations across a range of soils and managements, good relationships occurred between soil test P level and DP concentration in runoff for most of the tests and sampling depths used. Recent manure additions and high levels of surface cover from corn residue sometimes masked this relationship. The slope of DP relative to soil test P level was markedly higher on the silty clay loam soil than on the silt loam soils possibly due to soil permeability-infiltration rate differences. Agronomic soil P tests were as effective as environmentally oriented soil P tests for predicting DP concentrations in runoff.     

Effects of Climate and Soil Properties on U.S. Home Lawn Soil Organic Carbon Concentration and Pool

Following turfgrass establishment, soils sequester carbon (C) over time. However, the magnitude of this sequestration may be influenced by a range of climatic and soil factors. Analysis of home lawn turfgrass soils throughout the United States indicated that both climatic and soil properties significantly affected the soil organic carbon (SOC) concentration and pool to 15-cm depth. Soil sampling showed that the mean annual temperature (MAT) was negatively correlated with SOC concentration. Additionally, a nonlinear interaction was observed between mean annual precipitation (MAP) and SOC concentration with optimal sequestration occurring in soils receiving 60–70?cm of precipitation per year. Furthermore, soil properties also influenced SOC concentration. Soil nitrogen (N) had a high positive correlation with SOC concentration, as a 0.1?% increase in N concentration led to a 0.99?% increase in SOC concentration. Additionally, soil bulk density (ρ_b) had a curvilinear interaction with SOC concentration, with an increase in ρ_b indicating a positive effect on SOC concentration until a ρ_b of ~1.4–1.5?Mg?m^?3 was attained, after which, inhibition of SOC sequestration occurred. Finally, no correlation between SOC concentration or pool was observed with texture. Based upon these results, highest SOC pools within this study are observed in regions of low MAT, moderate MAP (60–70?cm?year^?1), high soil N concentration, and moderate ρ_b (1.4–1.5?Mg?m^?3). In order to maximize the C storage capacity of home lawns, non C-intensive management practices should be used to maintain soils within these conditions.     

Approximating phosphorus release from soils to surface runoff and subsurface drainage

Phosphorus application in excess of crop needs has increased the concentration of P in surface soil and runoff and led many states to develop P-based nutrient management strategies. However, insufficient data are available relating P in surface soil, surface runoff, and subsurface drainage to develop sound guidelines. Thus, we investigated P release from the surface (0-5 cm depth) of a Denbigh silt loam from Devon, U.K. (30-160 mg kg-1 Olsen P) and Alvin, Berks, Calvin, and Watson soils from Pennsylvania (10-763 mg kg-1 Mehlich-3 P) in relation to the concentration of P in surface runoff and subsurface drainage. A change point, where the slopes of two linear relationships between water- or CaCl2-extractable soil P and soil test phosphorus (STP) (Olsen or Mehlich-3) meet, was evident for the Denbigh at 33 to 36 mg kg-1 Olsen P, and the Alvin and Berks soils at 185 to 190 mg Mehlich-3 P kg-1. Similar change points were also observed when STP was related to the P concentration of surface runoff (185 mg kg-1) and subsurface drainage (193 mg kg-1). The use of water and CaCl2 extraction of surface soil is suggested to estimate surface runoff P (r2 of 0.92 for UK and 0.86 for PA soils) and subsurface drainage P (r2 of 0.82 for UK and 0.88 for PA soils), and to determine a change point in STP, which may be used in support of agricultural and environmental P management.     

Phosphorus forms and chemistry in the soil profile under long-term conservation tillage: a phosphorus-31 nuclear magnetic resonance study

In many regions, conservation tillage has replaced conventional tilling practices to reduce soil erosion, improve water conservation, and increase soil organic matter. However, tillage can have marked effects on soil properties, specifically nutrient redistribution or stratification in the soil profile. The objective of this research was to examine soil phosphorus (P) forms and concentrations in a long-term study comparing conservation tillage (direct drilling, "No Till") and conventional tillage (moldboard plowing to 20 cm depth, "Till") established on a fine sandy loam (Orthic Humo-Ferric Podzol) in Prince Edward Island, Canada. No significant differences in total carbon (C), total nitrogen (N), total P, or total organic P concentrations were detected between the tillage systems at any depth in the 0- to 60-cm depth range analyzed. However, analysis with phosphorus-31 nuclear magnetic resonance spectroscopy showed differences in P forms in the plow layer. In particular, the concentration of orthophosphate was significantly higher under No Till than Till at 5 to 10 cm, but the reverse was true at 10 to 20 cm. Mehlich 3-extractable P was also significantly higher in No Till at 5 to 10 cm and significantly higher in Till at 20 to 30 cm. This P stratification appears to be caused by a lack of mixing of applied fertilizer in No Till because the same trends were observed for pH and Mehlich 3-extractable Ca (significantly higher in the Till treatment at 20 to 30 cm), reflecting mixing of applied lime. The P saturation ratio was significantly higher under No Till at 0 to 5 cm and exceeded the recommended limits, suggesting that P stratification under No Till had increased the potential for P loss in runoff from these sites.