环境条件和微生物对灭线磷降解的影响

环境条件和微生物影响灭线磷在土壤中的降解。随着土壤含水量和温度的增加,灭线磷的降解速度加快;微生物对灭线磷的降解有显著影响,30℃、含水量为40%条件下,未灭菌土中灭线磷的半衰期为16.6 d,灭菌土中灭线磷的半衰期为31.6 d;有机质对灭线磷的降解也有显著影响,有机质含量高,有利于灭线磷的降解;灭线磷在碱性土壤中的降解快于在酸性土壤中;30℃、含水量为40%条件下,灭线磷在3种土壤中的降解速度为:东北黑土＞广东红土＞山东砂壤土。     

啶虫脒和阿维菌素在4种不同类型土壤中的吸附及迁移

采用薄层层析和平衡振荡法,分别测定了啶虫脒和阿维菌素在紫色土、砖红土、黄壤土和黑土4种不同类型土壤中的迁移率(Rf )和吸附常数(Kd),比较了2种农药在单用及混用下迁移和吸附行为的差异。结果表明:2种农药在单用及混用下的迁移行为几乎不存在差异,在4种土壤中的Rf 值大小顺序均为:黄壤土>紫色土>黑土>砖红土;2种农药的吸附过程均符合经典的Freundlich模型,混用时阿维菌素对啶虫脒的吸附无影响,但啶虫脒的存在会减少土壤对阿维菌素的吸附,表现为竞争吸附作用。     

特丁硫磷在环境中的迁移性研究

采用室内模拟试验方法,研究了有机磷类农药特丁硫磷在不同环境介质中的挥发性以及在3种不同类型土壤中的吸附性、移动性及其影响因素。结果表明:特丁硫磷具有较强的挥发性,其在空气、土壤表面和水中的挥发率分别为87.1%、38.6%和2.51%;在江西红壤、太湖水稻土与东北黑土中的吸附性较好地符合Freundlich方程,3种土壤中的吸附系数Kd值分别为6.56、11.34和15.80;薄层层析试验显示,当溶剂展开至12.0 cm时,特丁硫磷在江西红壤、太湖水稻土与东北黑土中最远可分别移至6~8、4~6和6~8 cm处,土柱试验结果显示,江西红壤、太湖水稻土与东北黑土淋出液中特丁硫磷质量分数分别为5.77%、1.13%和1.22%,表明特丁硫磷具有一定的移动性。影响特丁硫磷在土壤中吸附性和移动性的主要因素为土壤有机质含量,其次为土壤质地。特丁硫磷具有高挥发性及一定的移动性,其对人畜的安全以及地下水的危害应引起高度重视。     

土壤中苯肽胺酸的测定及淋溶特性研究

建立了反相条件下超高效液相色谱-串联质谱(UPLC-MS/MS)检测土壤中苯肽胺酸残留量的分析方法,并结合土壤薄层层析试验研究了苯肽胺酸在3种典型土壤(黑土、水稻土和红土)中的淋溶特性。结果表明:添加水平为0.1、1和10 mg/kg时,苯肽胺酸在土壤中的添加回收率为77.3%~99.4%,相对标准偏差(RSD)为1.3%~11.4%;其在3种土壤中的检出限(LOD)均低于1.0μg/kg。苯肽胺酸在吉林黑土中的比移值(Rf)为0.83,其移动性为可移动;在江苏水稻土中的Rf值为0.61,在湖南红土中的Rf值为0.62,移动性均为中等。     

磺草酮在土壤中的淋溶特性研究

基于所建立的土壤中磺草酮残留的超高效液相色谱-串联质谱分析方法,通过土壤薄层层析试验研究了磺草酮在中国3种典型土壤中的淋溶特性。结果表明:添加水平为1和10 mg/kg时,磺草酮在土壤中的添加回收率为80%~104%,相对标准偏差为1.2%~8.1%,最低检测浓度为0.1 mg/kg。磺草酮在河北潮土、湖南红土和吉林黑土中的比移值(Rf)分别为0.563、0.101和0.422,其在潮土和黑土中的移动性为中等,在红土中为不易移动;磺草酮在土壤中的淋溶特性与土壤理化性质密切相关,主要影响因素是土壤p H值及黏粒组分含量。     

毒死蜱和氰戊菊酯在土壤中的吸附与迁移

为评估被用作白蚁预防药剂的毒死蜱和氰戊菊酯在土壤中的移动性,采用平衡吸附法和薄层层析法分别测定了两种农药在浙江宁波地区的东钱湖土(粉砂质壤土)、青岭土(粉砂质壤土)和象山土(粉砂质黏壤土)3种土壤中的吸附常数(Kd)和迁移率(Rf)。结果表明,两种供试药剂在东钱湖土中的吸附等温线线性化程度均较高,而在青岭土和象山土中的吸附等温线均近似于 "L"型。从Kd和有机质吸附常数Koc的数值看,氰戊菊酯在土壤中的吸附作用主要受土壤有机质因素影响,而毒死蜱的吸附并非只受土壤有机质因素的影响。毒死蜱在3种供试土壤中的Kd和Rf值均高于氰戊菊酯。这表明由Kd值推测不同农药在土壤中的相对移动性可能会存在一定偏差。毒死蜱和氰戊菊酯在3种土壤中的Rf值由大到小的顺序为:东钱湖土>青岭土>象山土;而Kd值由大到小顺序为象山土>青岭土>东钱湖土。对Kd和Rf值与土壤理化性质的多元线性回归分析表明:1)土壤有机质含量和阳离子代换量在决定Kd和Rf值中所起的作用相互重叠;2)土壤有机质含量(或土壤阳离子代换量)和土壤黏粒含量是影响Kd和Rf值的关键因素,而土壤pH值对于Kd和Rf值无决定性影响。     

化学农药环境安全评价试验准则(续)

3.1.6 土壤淋溶作用试验在农业上使用的农药,都要提供淋溶特性资料。淋溶作用与吸附作用密切相关,可利用吸附常数估计农药在土壤中的移动性。淋溶试验可用土壤柱淋溶法或土壤薄层层析法测定。用土壤柱淋溶法测定时,对易降解的农药,最好同时测定降解作用。试验时可模拟农药使用地区的气温与降雨条件,并提供土     

灭线磷对土壤微生物呼吸的影响

本文采用直接吸收法（密闭法）测定了灭线磷对3种土壤微生物呼吸的影响，并对其进行了安全性评价。结果表明：灭线磷对土壤微生物基本无影响，属低毒级农药。     

二氰蒽醌在几种典型土壤中的降解吸附和移动特性

采用室内模拟试验方法,研究了二氰蒽醌在国内3种典型土壤江西红壤、东北黑土和太湖水稻土中的降解、吸附和移动特性。结果表明,25℃下二氰蒽醌在江西红壤、东北黑土与太湖水稻土中的降解半衰期分别为5.614、1.939、4.767d,其在土壤中化学稳定性较弱,易于降解,且pH越高,降解越快。二氰蒽醌在江西红壤的吸附等温线可以Freundlich方程很好地拟合,在东北黑土和太湖水稻土中的则可用线性方程拟合,吸附系数Kd值分别为36.4、114.6和51.9,Koc值分别为3 661.9、6 741.1、4 119.0,二氰蒽醌在土壤中具有中等或较强的吸附性能,在环境中迁移扩散的能力较弱。采用土壤薄层试验得到二氰蒽醌在这三种土壤中的移动分配系数Rf均<0.1,属于难于淋溶的农药,对地下水影响较小。二氰蒽醌在我国的几种典型土壤中均表现出了易降解性,难迁移以及难淋溶的特性,在目前的使用情况下,二氰蒽醌的环境风险较低。     

新农药呋喃虫酰肼在土壤降解研究

本文研究了其在3种土壤中有氧环境下的降解情况。呋喃虫酰肼在3种土壤中的降解速率大小依次为河南黄土〉吉林黑土〉江西红土,其降解半衰期分别为315、365、213d,降解遵循一级动力学方程。根据国内农药在土壤中的残留划分标准,呋喃虫酰肼属于较难降解类农药。比较呋喃虫酰肼在非灭菌与灭菌的吉林黑土、江西红土和河南黄土中的降解情况表明,药剂在非灭菌土中降解明显加快,分析可能是土壤中微生物对呋喃虫酰肼的降解具有显著的影响。     

Movement and rate of decomposition of ethoprophos in soil columns under field conditions

The rates of degradation and downward movement of ethoprophos (O-ethyl SS-dipropyl phosphorodithioate) were measured under field conditions in four soils in aluminium columns (40 cm long). A 10% granular formulation was incorporated in the top 10 cm at a rate of 10.0–10.5 kg a.i./ha. Under outdoor conditions during spring and summer, loss of ethoprophos approximated to first order kinetics; the half-life was about 87 days in a humic sand and a peaty sand, with pH values of 4.5 and 4.6, respectively. In a sandy loam and a loam soil with pH values of 7.2 and 7.3, respectively, the half-life ranged between 14 and 28 days. Under experimental conditions with fallow soils and 35.3 cm rainfall, the downward movement of substantial concentrations of ethoprophos by leaching and diffusion was restricted to a few centimetres.     

Suppression of Rhizoctonia solani in potato fields. II. Effect of origin and degree of infection with Rhizoctonia solani of seed potatoes on subsequent infestation and on formation of sclerotia

The seed potatoes used in these experiments had been grown in a slightly acid pleistocene sandy soil or in a marine, holocene sandy loam. They were free of sclerotia ofR. solani or lightly or moderately speckled with them. Seed potatoes from the sandy soil produced plants that suffered less fromRhizoctonia than plants from seed potatoes that had been grown on the marine sandy loam. Similarly harvested tubers had, in a non-conducive soil and in conducive soils with a (very) low inoculum density ofR. solani, fewer sclerotia when they came from seed potatoes grown in an acid sand. In each soil, the degree of infestation of the crop not only depended on the severity of infection of the seed potatoes, but also on their origin. With regard to sclerotia production on tubers, three types of soil were distinguished: suppressive, conducive with a high, and conducive with a very low inoculum density ofR. solani. The differences in infestation and in the amounts of sclerotia on tubers between the crop grown from seed potatoes from the sandy soil and that from seed potatoes from the marine sandy loam soil, is attributed to a richer load of antagonists on the former and possibly to a larger proportion of saprophyticRhizoctonia strains among their sclerotia. The antagonists seem to be inhabitants of the subterranean parts of the plant and to function independently of the soil. This implies possibilities for their use in biological control.     

Activity,adsorption, mobility and field persistence of sulfosulfuron in soil

Petri dish bioassays, based on root response of corn grown in soil or in perlite, were used to study the activity, adsorption, mobility and field persistence of sulfosulfuron in a silty clay loam and a sandy loam soil. Both bioassays indicated that activity of sulfosulfuron increased with increasing herbicide concentration, and to a slightly greater degree in sandy loam soil than in silty clay loam soil. More sulfosulfuron was adsorbed on the sandy loam (not biologically available) than on the silty clay loam soil. Consequently, slightly greater amounts of sulfosulfuron were leached through the silty clay loam than through the sandy loam soil. Biologically available sulfosulfuron was not detected at depths below 40 cm after application in sandy loam, but this was not the case for the silty clay loam soil. In 2002, all sulfosulfuron rates showed field persistence of less than 5 months. On the other hand, in 2003, biologically available sulfosulfuron was detected in the 0–10-cm soil depth 150 days after application. http://www.phytoparasitica.org posting May 6, 2004.     

Gross nitrogen transformations and N_2O emission sources in sandy loam and silt loam soils

The soil type is a key factor influencing N(nitrogen) cycling in soil; however, gross N transformations and N_2O emission sources are still poorly understood. In this study, a laboratory ~(15)N tracing experiment was carried out at 60% WHC(water holding capacity) and 25℃ to evaluate the gross N transformation rates and N_2O emission pathways in sandy loam and silt loam soils in a semi-arid region of Heilongjiang Province, China. The results showed that the gross rates of N mineralization, immobilization, and nitrification were 3.60, 1.90, and 5.63 mg N/(kg·d) in silt loam soil, respectively, which were 3.62, 4.26, and 3.13 times those in sandy loam soil, respectively. The ratios of the gross nitrification rate to the ammonium immobilization rate(n/ia) in sandy loam soil and silt loam soil were all higher than 1.00, whereas the n/ia in sandy loam soil(4.36) was significantly higher than that in silt loam soil(3.08). This result indicated that the ability of sandy loam soil to release and conserve the available N was relatively poor in comparison with silt loam soil, and the relatively strong nitrification rate compared to the immobilization rate may lead to N loss through NO_3~– leaching. Under aerobic conditions, both nitrification and denitrification made contributions to N_2O emissions. Nitrification was the dominant pathway leading to N_2O production in soils and was responsible for 82.0% of the total emitted N_2O in sandy loam soil, which was significantly higher than that in silt loam soil(71.7%). However, the average contribution of denitrification to total N_2O production in sandy loam soil was 17.9%, which was significantly lower than that in silt loam soil(28.3%). These results are valuable for developing reasonable fertilization management and proposing effective greenhouse gas mitigation strategies in different soil types in semiarid regions.     

Evaluation of propargyl bromide for control of barnyardgrass and Fusarium oxysporum in three soils

With the scheduled phasing out of methyl bromide, there is an urgent need for alternatives. We evaluated the efficacy of propargyl bromide as a potential replacement for methyl bromide for the control of barnyardgrass (Echinochloa crus-galli) and Fusarium oxysporum in an Arlington sandy loam, a Carsitas loamy sand and a Florida muck soil. Soil was mixed with barnyardgrass seeds or F oxysporum colonized on millet seeds, and treated with propargyl bromide at a range of concentrations. The mortality of the fungi and weed seeds was determined after 24 h of exposure at 30 degrees C. The concentrations required to inhibit 50% barnyard seed germination (LC50) were 2.8, 2.4 and 48.5 micrograms g-1 in the sandy loam, loamy sand and muck soil, respectively. In contrast, the LC50 values for F oxysporum were 11.2, 10.8 and 182.1 micrograms g-1 in the sandy loam, loamy sand and muck soil, respectively. The low efficacy of propargyl bromide in the muck soil was a result of the rapid degradation and high adsorption of the compound in the soil. The degradation half-life (t1/2) was only 7 h in the muck soil at an initial concentration of 6.8 micrograms g-1, compared to 60 and 67 h in the sandy loam and loamy sand, respectively. The adsorption coefficients (Kd) were 0.96, 0.87 and 5.6 cm3 g-1 in the sandy loam, loamy sand and muck soil, respectively. These results suggest that registration agencies should consider site-specific properties in recommending application rates for propargyl bromide.     

[14C]Glyphosate transport in undisturbed topsoil columns

Although glyphosate (N‐(phosphonomethyl)glycine) is one of the most frequently used herbicides, few controlled transport experiments in undisturbed soils have been carried out to date. The aim of this work was to study the influence of the sorption coefficient, soil‐glyphosate contact time, pH, phosphorus concentration and colloid‐facilitated transport on the transport of [¹⁴C]glyphosate in undisturbed top‐soil columns (20 cm height × 20 cm diameter) of a sandy loam soil and a sandy soil. Batch sorption experiments showed strong Freundlich‐type sorption to both soil materials. The mobility of glyphosate in the soil columns was strongly governed by macropore flow. Consequently, amounts of glyphosate leached from the macroporous sandy loam soil were 50–150 times larger than from the sandy soil. Leaching rates from the sandy soil were not affected by soil‐glyphosate contact time, whereas a contact time of 96 h strongly reduced the leaching rates from the sandy loam soil. The role of pH and phosphorus concentration in solution was relatively unimportant with respect to total glyphosate leaching. The contribution of colloid‐facilitated transport was <1 to 27% for the sandy loam and <1 to 52% for the sandy soil, depending on soil treatment. The risk for glyphosate leaching from the top‐soils seems to be limited to conditions where pronounced macropore flow occurs shortly after application. © 2000 Society of Chemical Industry     

宁夏中部干旱带降水渗透深度预测模型研究

为掌握降水在宁夏中部干旱带天然草场土壤中的渗透情况,引入根据土壤含水量增量变化确定渗透深度的方法,并运用回归、逐步回归和相关分析等多种统计手段,建立了不同土壤质地下降水渗透深度预测统计模型。结果表明:(1)运用回归方法建立的渗透深度预测模型(R~2在0.60~0.67)比逐步回归预测模型(R~2在0.49~0.58)显著性好,两种预测模型中降水量或降水日数的回归系数在置信度为0.05水平下均通过显著性检验。(2)通过对两种预测模型预测结果与实测值的相关分析,回归预测结果、逐步回归预测结果和实测值之间的相关系数达0.70以上,特别是两种模型预测结果相关性显著(相关系数0.88~0.93),从模型简单可用的角度考虑,最终选用逐步回归预测模型。(3)兴仁沙壤土条件下预测效果较好(81%~100%的样本相对误差均在30%左右或以下),同心壤土预测效果中等(55%~60%的样本相对误差小于30%),盐池粗砂土条件下效果一般(约50%左右样本相对误差在30%及以下)。(4)同时,文中预测模型试验验证了不同土壤质地对降水渗透深度的影响,当相同的降水过程下,降水渗透深度大小顺序为粗砂土沙壤土壤土。     

Crawler phenology and generation development of the Florida wax scale,ceroplastes floridensis,on citrus planted in two soil types

Appearance of Florida wax scale (FWS) crawlers in citrus groves planted in sandy soil preceded that in groves planted in loam. The duration of crawler presence was longer on citrus in loam than in sandy soil. Mean age, as expressed by weighted developmental stage, yielded a linear regression with time. FWS develops two generations per year, which on sandy soil appear earlier and develop faster to the preovipositional stage than on loam. The size of ovipositing females was in direct correlation with the duration of development.