不同土壤磷流失过程模拟研究

本研究通过室内培养、淋溶模拟和径流模拟试验，分别对酸性土壤（红壤）和不同质地碱性土壤（潮褐土和黑钙土）磷流失过程进行模拟研究。结果表明，不同土壤相同水分条件下，土壤磷流失潜能不同：潮褐土磷流失潜能最强，黑钙土次之，红壤最低。不同水分条件下，相同土壤磷流失潜能也不同：淹水条件土壤磷流失潜能最高，其次为先干后湿条件和先湿后干条件，好气条件和淋溶最低。各种条件下土壤磷流失潜能均随施磷量的增加而增大。施肥初期或土壤环境变化初期，土壤磷通过地表径流和优先流流失的风险较高；通过基质流流失的磷在土壤中逐渐向下迁移，故磷流失风险发生在施肥后期。 分段模型（Split Line）方法适合于预测土壤磷通过径流向地表水或通过优先流向地下水体的流失，但不适合预测土壤磷通过基质流的流失。应针对土壤不同水分条件分别使用分段模型方法。若不考虑土壤不同水分条件，则用淹水条件下的临界值较为安全。在预测通过基质流淋失的磷时，使用深层土壤CaCl2-P磷含量较使用表层土壤磷含量更为合理。对于红壤，由于在各种培养条件下土壤Bray-P的变化趋势与CaCl2-P较为一致，且土壤Bray-P的分辨度较高，用土壤Bray-P表征磷流失潜能优于Olsen-P。 综合各种水分条件，红壤土壤磷流失安全值为Bray-P含量低于130 mg kg-1，黑钙土为Olsen-P含量低于138.2mg kg-1，潮褐土为Olsen-P含量低于88.9mg kg-1。

有机质、CaCl_2和MgCl_2对细颗粒泥沙絮凝沉降的影响

在CaCl2和MgCl2浓度为0~1.0mmol/L,泥沙浓度为10g/L时,用吸管法研究了有机质、CaCl2和MgCl2对细颗粒泥沙静水絮凝沉降的影响,结果表明,去除有机质后,细颗粒泥沙絮凝沉降加快,其絮凝所需的最佳电解质浓度降低;CaCl2和MgCl2的絮凝能力无明显差异,有机质含量对其几乎没有影响;在相同盐度下,细颗粒泥沙的絮凝沉降速度随电解质摩尔浓度的增大而增大.

有机质对细颗粒泥沙静水絮凝沉降特性的影响

在CaCl2 和MgCl2 浓度为 0～ 1.0mmol L ,泥沙浓度为 10g L时 ,本文用吸管法研究了有机质对细颗粒泥沙絮凝沉降的影响 ,结果表明 :在液面下同一深度 ,有机质并不影响泥沙浓度随时间呈指数衰减的变化规律。但去除有机质后 ,细颗粒泥沙絮凝的最佳电解质浓度降低 ;对于相同的电解质浓度 ,其絮凝沉降加快 ,泥沙平均沉速明显增大

水稻重金属镉含量与土壤质量关系的研究

采用盆栽试验的方法,考察了土壤中不同浓度的镉对水稻生长、结实及重金属镉富集的影响以及镉在水稻植株的分布情况,并进一步研究了糙米(可食部位)对镉的富集量与土壤中镉总量和有效态镉含量的关系。研究表明:低浓度的镉对水稻生长稍有促进作用,高浓度的镉对其生长并没有明显的抑制作用;镉在水稻植株中总的分布趋势为根>茎>稻壳>糙米;用4种有效态提取剂(0.1 mol/L CaCl2、DTPA、0.05 mol/L EDTA和1 mol/L NH4OAc)浸提出的有效态镉的含量和土壤中镉总量与水稻糙米中镉含量均达到显著相关水平,并确定了它们的临界值分别为CaCl2-Cd=0.71 mg/kg,DTPA-Cd=1.34 mg/kg,EDTA-Cd=0.76 mg/kg,NH4OAc-Cd=0.77 mg/kg。

微量添食对柞蚕蚁蚕抗逆性的影响

通过卵面微量添食葡萄糖、有益微生物 (EM)及CaCl2 3种物质 ,以半数致死时间 (LT50 )为指标 ,研究添食不同物质对柞蚕初孵蚁蚕抗逆性的影响。结果表明 ,卵面添食这 3种物质均能增强蚁蚕的抗低温能力 ,延长其在低温条件下的半数致死时间 (LT50 )。添食葡萄糖能显著延长蚁蚕对饥饿的LT50 ;添食EM能极显著延长蚁蚕对饥饿的LT50 ;添食CaCl2 对蚁蚕耐饥饿能力的影响不显著。各种添食物质对蚁蚕抗逆性的影响均存在浓度效应

Cytotoxicity of liver targeted drug-loaded alginate nanoparticles

In this study, novel liver targeted doxorubicin (DOX) loaded alginate (ALG) nanoparticles were prepared by CaCl2 crosslinking method. Glycyrrhetinic acid (GA, a liver targeted molecule) modified alginate (GA-ALG) was synthesized in a heterogeneous system, and the structure of GA-ALG and the substitution degree of GA were analyzed by H-1 NMR, FT-IR and elemental analysis. The drug release profile under the simulated physiological condition and cytotoxicity experiments of drug-loaded GA-ALG nanoparticles were carried out in vitro. Transmission electron micrographs (TEM) and dynamic light scattering (DLS) analysis showed that drug-loaded GA-ALG nanoparticles have spherical shape structure with the mean hydrodynamic diameter around 214 +/- 11 nm.

INFRARED SPECTRA AND CRYSTAL STRUCTURE OF BIS-(DIMETHOXYLPHOSPHATO) COPPER

The title complex has beep synthesized by the reaction of CaCl2, with trimethyl phosphate. Its Infrared spectra from 4000 to 100 cm(-1) measured. The assignment of acme absorption bands was discussed. It is found that the stretching vibrations of bridge groups O-P-O are divided into two groups according to their bond length. The crystal structure of the complex boa been determined from single crystal K-ray diffraction data. The crystals belong to monoclinic system, space group P2(1)/c with cell parameteras, a = 1,0704(4), b = 0.5093(2), c = 1.9737(6)nm, beta = 96.23(3)degrees, V = 1.0696(6)nm(2), Z = 4, final R = 0.044. Copper ion is coordinated to five Rimester oxygen atoms to form a distorted square pyramid. The adjacent copper ions are connected by symmetric and non-symmetric bridge groups of O-P-O, forming an infinite one-dimensional chain coordination polymer.

Purification and partial characterization of Mn superoxide dismutase from muscle tissue of the shrimp Macrobrachium nipponense

Superoxide dismutase (SOD; EC 1.15.1.1) is an enzyme that protects against oxidative stress from superoxide radicals in living cells. This enzyme had been isolated, purified and partially characterized from muscle tissue of the shrimp Macrobrachium nipponense. The purification was achieved by heat treatment, ammonium sulfate fractionated precipitation and column chromatograph on DEAE-cellulose 32. Some physiological and biochemical characterization of it was tested. The molecular weight of it was about 21.7 kDa, as judged by SDS-polyacrylamide gel electrophoresis. The purified enzyme had an absorption peak of 278 nm in ultraviolet region, and the enzyme remained stable at 25-45 degreesC within 90 min. However, it was rapidly inactivated at higher temperature. Treatment of the enzyme with 1 mM ZnCl2, SDS and 1 mM or 10 mM mercaptoethanol showed some increasing activity. However, the enzyme activity was obviously inhibited by 10 mM CaCl2, CuSO4, ZnCl2 and 1 mM CaCl2 and 10 mM K2Cr2O7. SOD activity did not show significantly variation after incubated with 1 mM CaCl2, EDTA and 10 MM SDS. The enzyme was insensitive to cyanide and contained 1.03 +/- 0.14 atoms of manganese per subunit shown in atomic absorption spectroscopy, which revealed that purified SOD was Mn superoxide dismutase. (C) 2004 Elsevier B.V. All rights reserved.

Preparation of chloroplasts from brown algae

Thalli from a brown alga Undaria pinnatifida were soaked by CaCl2 solution with different concentration and time at 4 degreesC, the effect of CaCl2 solution on efficiency and influorescence emission spectra of chloroplasts were examined. The results show that the efficiency of collected chloroplasts is increased markedly after soaking in CaCl2 solution. According to the results of collected efficiency and characteristic of influorescence emission spectra at room temperature of chloroplasts, it was suggested that soaking in the 0.2 mol/L CaCl2 solution for 10 min is optimum. Under this condition, the efficiency of collected chloroplasts is as 5 fold as control group, and the characteristics of chloroplasts obtained by CaCl2 soaking are similar to that of traditional method.

Comparison of effectiveness of different ashing auxiliaries for determination of phosphorus in natural waters, aquatic organisms and sediments by ignition method

An improved method for the determination of phosphorus in natural waters, aquatic organisms and sediments by ignition method is proposed. The recoveries of phosphorus (P) from selected inorganic and organic P-containing compound standards after ignition with different auxiliaries, such as MgSO4, Mg(NO3)(2), MgO2, Mg(Ac-2) and CaCl2, were compared. We found that the phosphorus from most compound standards could not be completely recovered when these compounds were ignited (450-500degreesC) with the MgSO4 as auxiliary and the baked residue was extracted with 0.2 mol l(-1) HCl for 30min at 80degreesC or at room temperature. P recoveries, for example, were poor, less than 85%, if pyrophosphate and metaphosphate were ignited with the addition Of MgSO4 prior to the extraction of the baked residue with 0.2 mol l(-1) HCl at 80degreesC for 30 min. In contrast, MgO2, Mg(Ac)(2) and CaCl2, as well as Mg(NO3)(2), could all yield complete P recoveries at routine ashing temperatures (450-500degreesC). The results demonstrate that MgC12 is a more effective auxiliary agent for the determination of phosphorus in natural waters, aquatic organisms and sediments by ignition method than MgSO4 which is commonly used. (C) 2003 Elsevier Science Ltd. All rights reserved.

Extraction of phosphorus in natural waters and sediments by ignition method

Phosphorus recoveries from selected inorganic and organic P-containing compounds after ignition with auxiliaries, such as MgSO4, Mg (NO3)(2), MgCl2, Mg (Ac)(2) and CaCl2 were studied. It was found that the phosphorus could not be completely recovered when most P-containing compounds were ignited with MgSO4 at temperature not higher than 500degreesC if the baked residue was extracted with 0.2 mol/L HCl for 30 min at 80degreesC or at room temperature. In contrast, MgCl2, Mg(Ac)(2) and CaCl2, as well as Mg(NO3)(2), could all yield complete P recoveries. We suggest that MgCl2 rather than MgSO4, which is usually used, should be utilized as ashing auxiliary agent in the P extraction by ignition method. Although Mg (NO3)(2) is a highly effective auxiliary agent, yet interference from MgSO4, danger of explosion, toxicity of nitrogen dioxide and more manipulation steps may limit its widespread utilization. It is suggested that if sediment is ignited with MgCl2, the extraction of residue with 0.2 mol/L HCl for 30 min at 80degreesC could give good result.

藏药7号水提液对大鼠离体胸主动脉条收缩作用的影响

目的通过观察藏药7号水提液对大鼠离体胸动脉条收缩作用的影响,研究藏药7号的降压机制.方法以生理盐水作为对照组,观察藏药7号水提液(6 g/L)和维拉帕米(Ver 0.013 g/L)对高K+液引起的主动脉条收缩的时效影响,观察对KCl、NE及CaCl2引起的大鼠主动脉条收缩的量效曲线的影响,以及对NE引起的依赖于细胞内钙及细胞外钙收缩的影响.结果藏药7号水提液抑制高K+液引起的主动脉收缩(P<0.001);而且可以使KCl、NE及CaCl2引起的大鼠主动脉条收缩的量效曲线非平行右移,最大效应降低,呈非竞争性拮抗作用(P<0.05);与维拉帕米相似,并且对NE引起的依赖于细胞内钙及细胞外钙的收缩均有抑制作用(P<0.05).结论提示藏药7号的降压机制与钙离子通道拮抗剂一致,而且其作用效果比Ver平稳,其最大作用与Ver相近.

Suitability of extractants for predicting available sulfur in natural grassland in the Inner Mongolia steppe of China

It was the objective of this study to compare the suitability of different extractants for predicting the availability of sulfur (S) in natural grassland in a sulfur response trial on three different soil types in the Inner Mongolia steppe of China. For soil analysis, seven different extractants have been employed. The inorganic SO4-S concentration was determined by ion chromatography. Additionally, in the Ca(H-2-PO4)(2) extract the total soluble S was determined employing turbidimetry. Weak salt solutions (0.15% CaCl2, Ca(H2PO4)(2), and KH2PO4) extracted similar amounts Of SO4-S. Extraction with 0.025 M KCl provided the lowest SO4-S values. Deionized water dissolved significantly more SO4-S in the control plots than most weak salt extractants. The concentration of soluble organic S decreased in the control plots after 100 days of plant growth, indicating that the organic S pool contributed significantly to the S nutrition of the forage crops. Significant relationships among the SO4-S in the soil determined in different extracts and crop yield, sulfur content in the forage, and total sulfur uptake were only found for the Ca(H2PO4)(2) extract. In general, the correlation coefficients proved to be unsatisfactory for field experimentation.

水-盐-气天然流体的物理化学性质模拟与流体包裹体应用研究

Natural fluids with water-salt-gas are often found in every sphere of the Earth, whose physicochemical properties and geochemical behaviors are complicated. To study these properties and behaviors turns out to be one of the challenging issues in geosciences. Traditional approaches mainly depend on experiments and observations. However, it is impossible to obtain a large number of data covering a large T-P space of the Earth by experimental methods in the near future, which will hinder the advance of the theoretical study. Therefore, it is important to model natural fluids by advanced theoretical methods, by which limited experimental data can be extended to a large temperature-pressure-composition space. Physicochemical models developed in this dissertation are not only more accurate, but also extend the applied T-P-m region of the experimental data of the multi-fluid systems by about two times. These models provide the new and accurate theoretical tools for the geochemical research, especially for the water-rock interactions and the study of the fluid inclusions. The main achievements can be summarized as follows: (1) A solubility model on components of natural gases is presented. The solubility model on the systems of CH4-H2O-NaCl, C2H6-H2O-NaCl or N2-H2O-NaCl takes advantage of modern physicochemical theory and methods, and is an improvement over previous models whose prediction and precision are relatively poor. The model can predict not only the gas solubility in liquid phase but also water content in the gas phase. In addition, it can predict gases (methane or nitrogen) solubility in seawater and brine. Isochores can be determined, which are very important in the interpretation of fluid inclusions. (2) A density model on common aqueous salt solutions is developed. The density models with high precision for common aqueous salt solutions (H2O-NaCl, H2O-LiCl, H2O-KCl, H2O-MgCl2, H2O-CaCl2, H2O-SrCl2 or H2O-BaCl2) are absent in the past. Previous density models are limited to the relatively small range of experimental data, and cannot meet the requirement of the study of natural fluids. So a general density model of the above systems is presented by us based on the international standard density model of the water. The model exceeds the other models in both precision and prediction. (3) A viscosity model on common aqueous alkali-chloride solutions is proposed. Dynamic viscosity of water-salt systems, an important physics variable, is widely used in three-dimension simulation of the fluids. But in most cases, due to the lack of viscosity models with a wide T-P range, the viscosity of aqueous salt solutions is replaced by that of the water, giving rise to a relatively large uncertainty. A viscosity model with good prediction for the systems (H2O-NaCl, H2O-LiCl or H2O-KCl) is presented on the base of the international standard viscosity model of water and the density model developed before. (4) Equation of State applied in fluid inclusions. The best Equations of State in the world developed by others or us recently are applied in the study of the fluid inclusions. Phase equilibria and isochores of unitary system (e.g. H2O, CO2, CH4, O2, N2, C2H6 or H2S), binary H2O-NaCl system and ternary H2O-CH4-NaCl system are finished. From these programs and thermodynamic equations of coexisting ores, the physicochemical conditions before or after the deposits form can be determined. To some extent, it is a better tool.