以磺胺嘧啶(Sulfadiazine,SDZ)为研究对象,通过室内原状土柱(0~15 cm,土柱Ⅰ和15~30 cm,土柱Ⅱ)出流试验探讨了其在不同剖面深度处的迁移特征,运用Hydrus-1D软件对试验结果进行模拟,并对不同流速下磺胺嘧啶在0~200 cm土壤中的迁移行为...以磺胺嘧啶(Sulfadiazine,SDZ)为研究对象,通过室内原状土柱(0~15 cm,土柱Ⅰ和15~30 cm,土柱Ⅱ)出流试验探讨了其在不同剖面深度处的迁移特征,运用Hydrus-1D软件对试验结果进行模拟,并对不同流速下磺胺嘧啶在0~200 cm土壤中的迁移行为做了预测。结果表明:SDZ在原状土柱Ⅱ中的穿透曲线相较于原状土柱Ⅰ的发生左移,即较深层土壤中,SDZ的迁移速度更快,这主要是受土壤理化性质,如有机质、阳离子交换量和p H等的影响;两区模型(TRM)模拟的R^2>0.91,均方根误差RMSE<0.061,不动水区域f<0.154,其模拟效果优于单点模型(OSM)和两点模型(TSM),表明土壤的不可动区域是吸附SDZ的重要部分。预测结果显示:同一流速时,SDZ浓度峰值随着土壤剖面深度增加而减小,出流时间逐渐增大;同一深度处,当水流速度从0.017 cm min^(-1)增加到0.030 cm min^(-1)再到0.100 cm min^(-1)时,磺胺嘧啶在土壤中的迁移速度不断加快,出流浓度也越来越高,当流速为0.100 cm min^(-1)时,SDZ可快速穿过土层进入地下水,其穿透曲线不再对称,出现拖尾现象。展开更多
Both physical and chemical processes affect the fate and transport of herbicides. It is useful to simulate these processes with computer programs to predict solute movement. Simulations were run with HYDRUS- 1 D to id...Both physical and chemical processes affect the fate and transport of herbicides. It is useful to simulate these processes with computer programs to predict solute movement. Simulations were run with HYDRUS- 1 D to identify the sorption and degradation parameters of atrazine through calibration from the breakthrough curves （BTCs）. Data from undisturbed and disturbed soil column experiments were compared and analyzed using the dual-porosity model. The study results show that the values of dispersivity are slightly lower in disturbed columns, suggesting that the more heterogeneous the structure is, the higher the dispersivity. Sorption parameters also show slight variability, which is attributed to the differences in soil properties, experimental conditions and methods, or other ecological factors. For both of the columns, the degradation rates were similar. Potassium bromide was used as a conservative non-reactive tracer to characterize the water movement in columns. Atrazine BTCs exhibited significant tailing and asymmetry, indicating non-equilibrium sorption during solute transport. The dual-porosity model was verified to best fit the BTCs of the column experiments. Greater or lesser concentration of atrazine spreading to the bottom of the columns indicated risk of groundwater contamination. Overall, HYDRUS-1D successfully simulated the atrazine transport in soil columns.展开更多
以虾致敏蛋白Pen a 1（Tropomyosin）抗原表位为研究对象,建立了利用Pena 1表位抗体亲和纯化致敏蛋白的新方法.Fmoc法合成致敏Pen a 1蛋白的C端含有3个抗原表位的第247 ～284位氨基酸对应的多肽片段,应用马来酰亚胺法将多肽与KLH（匙孔...以虾致敏蛋白Pen a 1（Tropomyosin）抗原表位为研究对象,建立了利用Pena 1表位抗体亲和纯化致敏蛋白的新方法.Fmoc法合成致敏Pen a 1蛋白的C端含有3个抗原表位的第247 ～284位氨基酸对应的多肽片段,应用马来酰亚胺法将多肽与KLH（匙孔血蓝蛋白）、BSA（牛血清白蛋白）偶联制备人工免疫抗原（Pep-tide-KLH）和人工包被抗原（Peptide-BSA）,免疫人工抗原免疫纯种新西兰白兔,获得多克隆抗血清,抗血清经辛酸-硫酸铵及特异性血清纯化预装柱（HiTrap rProtein A FF）纯化后与溴化氰活化琼脂糖凝4B（CNBr-Activated Sepharose 4B）进行偶联.ELISA（酶联免疫吸附试验）测定该多克隆抗体效价为2.05×106,多肽对抗体的IC50（50％抑制浓度）为0.21 mg/L,交叉试验表明该抗体与虾中非Pena 1蛋白无交叉反应性;Bradford法测定CNBr-Activated Sepharose 4B与抗体的偶联率为90.76％.间接竞争ELISA测定1 mL偶联介质的吸附容量为2.84 mg Pen a 1,免疫亲和柱的加标回收率为89.6％～93.6％,亲和柱使用寿命为4次.展开更多
The riverbank soil is a natural purifying agent for the polluted river water(Riverbank filtration, RBF). This is of great importance to groundwater safety along the riverbank. This paper examines the migration and tra...The riverbank soil is a natural purifying agent for the polluted river water(Riverbank filtration, RBF). This is of great importance to groundwater safety along the riverbank. This paper examines the migration and transformation rules of ammonia-nitrogen in three typical types of sand soil using the indoor leaching experiment of soil column, and then makes comparison with the indoor experiment results in combination with the numerical simulation method. The experiment process shows that the change in ammonia-nitrogen concentration goes through three stages including "removal-water saturation-saturation". As the contents of clay particles in soil sample increase, the removal of ammonia-nitrogen from soil sample will take more time and gain higher ratio. During the removal period, the removal ratio of Column 1, Column 2 and Column 3 averages 68.8%(1-12 d), 74.6%(1-22 d) and 91.1%(1-26 d). The ammonia-nitrogen removal ratio shows no noticeable change as the depth of soil columns varies. But it is found that the ammonia-nitrogen removal ratio is the least of the whole experiment when the soil columns are at the depth of 15 cm. It can be preliminary inferred that the natural purifying performance of soil along the river for ammonia-nitrogen in river water mainly depends on the proportion of fine particles in soil. HYDRUS-1D model is used to simulate this experiment process, analyze the change of the bottom observation holes by time and depth in three columns(the tenth day), and make comparison with the experiment result. The coefficients of determination for fitting curves of Column 1, Column 2 and Column 3 are 0.953, 0.909, 0.882 and 0.955, 0.740, 0.980 separately. Besides, this paper examines the contribution of absorption, mineralization and nitrification in the simulation process. In the early removal stage, mineralization plays a dominant role and the maximum contribution rate of mineralization is 99%. As time goes by, absorption starts to function and gradually assumes a dominant position. In the middle and late展开更多
文摘以磺胺嘧啶(Sulfadiazine,SDZ)为研究对象,通过室内原状土柱(0~15 cm,土柱Ⅰ和15~30 cm,土柱Ⅱ)出流试验探讨了其在不同剖面深度处的迁移特征,运用Hydrus-1D软件对试验结果进行模拟,并对不同流速下磺胺嘧啶在0~200 cm土壤中的迁移行为做了预测。结果表明:SDZ在原状土柱Ⅱ中的穿透曲线相较于原状土柱Ⅰ的发生左移,即较深层土壤中,SDZ的迁移速度更快,这主要是受土壤理化性质,如有机质、阳离子交换量和p H等的影响;两区模型(TRM)模拟的R^2>0.91,均方根误差RMSE<0.061,不动水区域f<0.154,其模拟效果优于单点模型(OSM)和两点模型(TSM),表明土壤的不可动区域是吸附SDZ的重要部分。预测结果显示:同一流速时,SDZ浓度峰值随着土壤剖面深度增加而减小,出流时间逐渐增大;同一深度处,当水流速度从0.017 cm min^(-1)增加到0.030 cm min^(-1)再到0.100 cm min^(-1)时,磺胺嘧啶在土壤中的迁移速度不断加快,出流浓度也越来越高,当流速为0.100 cm min^(-1)时,SDZ可快速穿过土层进入地下水,其穿透曲线不再对称,出现拖尾现象。
基金the China Harbor Engineering Company (CHEC) for providing financial support
文摘Both physical and chemical processes affect the fate and transport of herbicides. It is useful to simulate these processes with computer programs to predict solute movement. Simulations were run with HYDRUS- 1 D to identify the sorption and degradation parameters of atrazine through calibration from the breakthrough curves （BTCs）. Data from undisturbed and disturbed soil column experiments were compared and analyzed using the dual-porosity model. The study results show that the values of dispersivity are slightly lower in disturbed columns, suggesting that the more heterogeneous the structure is, the higher the dispersivity. Sorption parameters also show slight variability, which is attributed to the differences in soil properties, experimental conditions and methods, or other ecological factors. For both of the columns, the degradation rates were similar. Potassium bromide was used as a conservative non-reactive tracer to characterize the water movement in columns. Atrazine BTCs exhibited significant tailing and asymmetry, indicating non-equilibrium sorption during solute transport. The dual-porosity model was verified to best fit the BTCs of the column experiments. Greater or lesser concentration of atrazine spreading to the bottom of the columns indicated risk of groundwater contamination. Overall, HYDRUS-1D successfully simulated the atrazine transport in soil columns.
基金supported by Special Scientific Research Expenditure for Public Charity Industry of Ministry of Water Resources(No.201501008)Institute of Resources and Environment of North China University of Water Resources and Electric Power
文摘The riverbank soil is a natural purifying agent for the polluted river water(Riverbank filtration, RBF). This is of great importance to groundwater safety along the riverbank. This paper examines the migration and transformation rules of ammonia-nitrogen in three typical types of sand soil using the indoor leaching experiment of soil column, and then makes comparison with the indoor experiment results in combination with the numerical simulation method. The experiment process shows that the change in ammonia-nitrogen concentration goes through three stages including "removal-water saturation-saturation". As the contents of clay particles in soil sample increase, the removal of ammonia-nitrogen from soil sample will take more time and gain higher ratio. During the removal period, the removal ratio of Column 1, Column 2 and Column 3 averages 68.8%(1-12 d), 74.6%(1-22 d) and 91.1%(1-26 d). The ammonia-nitrogen removal ratio shows no noticeable change as the depth of soil columns varies. But it is found that the ammonia-nitrogen removal ratio is the least of the whole experiment when the soil columns are at the depth of 15 cm. It can be preliminary inferred that the natural purifying performance of soil along the river for ammonia-nitrogen in river water mainly depends on the proportion of fine particles in soil. HYDRUS-1D model is used to simulate this experiment process, analyze the change of the bottom observation holes by time and depth in three columns(the tenth day), and make comparison with the experiment result. The coefficients of determination for fitting curves of Column 1, Column 2 and Column 3 are 0.953, 0.909, 0.882 and 0.955, 0.740, 0.980 separately. Besides, this paper examines the contribution of absorption, mineralization and nitrification in the simulation process. In the early removal stage, mineralization plays a dominant role and the maximum contribution rate of mineralization is 99%. As time goes by, absorption starts to function and gradually assumes a dominant position. In the middle and late
