EDTA Extraction of Heavy Metals from Different Soil Fractions and Synthetic Soils

A laboratory-prepared contaminated soil was partitioned into four fractions, namely carbonate, Fe/Mn oxides, organic matter and clay mineral, according to the form in which the heavy metal bound with soil constituents. Individual contaminated soil fractions and synthetic soils were prepared for the study of soil extraction using ethylenediaminetetraacetic acid (EDTA). The effect of contact time and EDTA concentration were evaluated for both individual soil fractions and synthetic soils. The extraction reached equilibrium rapidly, after about 30 min. A 0.01 M EDTA solution was less effective than a 0.05 M or a 0.10 M EDTA. EDTA was proved to be effective for metal removal from the four individual soil fractions and synthetic soils. In general, approximately 90% of metals were removed from synthetic soils by 0.10 M EDTA. EDTA extraction of Pb from a contaminated carbonate fraction was thought to be affected by the formation of lead carbonates. A simple equation based on the sum of the released heavy metal from the individual components is used to check if there are interactions among the different soil components when mixed. The estimated values agreed well with the experimentally measured results only for the 0.10 M EDTA system.     

Adsorption of sulphate and fluoride by variable charge soils

The adsorption of sulphate and fluoride by three variable charge soils was studied. Adsorption increased with increase in the amount of sulphate added at constant _pH, and decreased with increase of _pH.
The ratios of the amount of released OH⁻to that of the adsorbed SO^2-₄ at pH 5–0 were 0.12, 0.14 and 0.20 for the three soils, respectively, much lower than the corresponding OH⁻/F⁻ ratios which ranged from 0.3 to 1.0. For a ferric acrisol the OH⁻ released accounted, on average, for only 15% of the SO^2-₄ adsorbed, leaving more than 60% to be explained by the decrease in positive charge and the increase in negative charge carried by the soil.     

桃树茎部施药的生理基础研究

探讨了茎部施药对桃树的生长及生理基础的影响,并运用灰色系统方法阐述了农药种类,深度及施药方法对叶相对生长率,新梢相对生长率,果实体积,叶绿素含量,净光合速率和防治效果等各考察因素的影响。研究表明,茎部施药效果普遍优于叶面喷药的处理,其中又１：３的久效磷进行茎部施药效果最好。     

利用计算机视觉定量描述茶叶色泽

选择ＨＩＳ颜色系统描述茶叶颜色,并对颜色描述系统模型进行了改进,使之能更好地模拟理想颜色模型。在此基础上对自然存储条件下不同年份生产的龙井茶的茶叶色泽和汤色进行定量测量,测量结果：利用计算机视觉能定量地茶叶色泽随储藏时间的变化。     

流域侵蚀产沙的尺度变异规律研究

 侵蚀产沙的尺度变异规律,是当今土壤侵蚀研究的前沿,它涉及的研究范围广泛,小到土壤颗粒,大到全球气候变化与碳循环过程。特别是不同尺度流域之间侵蚀产沙和输移,究竟有什么样的内在联系,小流域所获得的研究成果是否能推广应用到大中流域,已成为迫切需要解决的重要科学问题。有关流域侵蚀产沙与输移过程随流域尺度复杂变化的研究,国际上刚刚开始,国内有关流域尺度研究主要涉及于水文学领域的一些尺度研究,关于流域侵蚀产沙与输移过程随流域尺度复杂变化的研究不多。作者对国外当前土壤侵蚀模型的最新进展进行了综述,并对侵蚀产沙的尺度变异规律进行了分析。由于具有GIS强大的空间数据管理和分析能力,它将在流域侵蚀产沙尺度变异这一侵蚀产沙的问题研究中发挥重要作用。     

土壤氮矿化-固持周转(MIT)研究进展

土壤氮矿化-固持周转(MIT)过程与土壤供氮力及氮素损失间存在密切关系。本文概述了近年来MIT过程的研究方法及其相应的模型;对土壤温度、土壤水分、土壤理化性质、植物生长状况以及有机、无机肥的施用等影响MIT过程的主要因素进行了较详尽地阐述,并展望了今后主要的研究方向。     

槐花中黄酮类物质提取工艺的研究

该文研究了水提法、传统的醇回流法提取槐花总黄酮类化合物的提取工艺,并使用正交试验确定了最佳提取条件。试验结果表明:槐花中总黄酮类物质的最佳提取条件为B2C3A2,即用2倍量40%的乙醇连续回流提取3次(每次2h)     

Tillage and crop sequence effects on organic carbon and total nitrogen content in an irrigated Alberta soil

A better understanding of tillage effects on soil organic matter is vital for development of effective soil conservation practices. The objective of this research is to determine the effect of tillage and crop sequence on soil organic carbon (OC) and total nitrogen (TN) content in an irrigated southern Alberta soil. A field experiment was conducted using a split–split plot design from 1994 to 1998 in Alberta, Canada. There were two crop sequences (Sequence 1: spring wheat (Triticum aestivum L.)–sugar beet (Beta vulgaris L.)–spring wheat–annual legume; and Sequence 2: spring wheat–spring wheat–annual legume–sugar beet) and two tillage practices (CT: conventional tillage and MT: minimum tillage). Surface soil under MT had significantly higher OC (30.1 Mg ha⁻¹) content than under CT (28.3 Mg ha⁻¹) after 4 years of treatment. The MT treatment retains crop residue at the soil surface, reduces soil erosion and slows organic matter decomposition, which are key factors in enhancing the soil fertility status of southern Alberta irrigated soils.     

Aggregates and gel network structure of globin hydrolysates

A gel with excellent functional properties was prepared successfully using the hydrolysates of globin. In the present study, the structures of intermediate aggregates and gel network were observed directly with an electronic microscope. It was shown clearly that the intermediate aggregates were in a thin rod shape with a length of 130--140 nm, which was in good accordance with the results of the light scattering obtained in a previous study. The diameter of intermediate aggregates was 4--5 nm. Each unit of the intermediate aggregate was composed of beta-chain and peptide beta-1 in a ratio of 1:1. Its molecular weight was 26922 Da, and it had a diameter of 4.1 nm. The thin rod-shaped aggregates were formed with units through the hydrophobic interaction. The length of intermediate aggregate was >30--33 times the diameter. Furthermore, the cross-linked structure formed by peptide alpha-1 and the thin rod-shaped aggregates was also confirmed by the photography of the electronic microscope. These results supported the model proposed in previous papers as proper to depict exactly the formation and structure of the gel network of globin hydrolysates.     

Soil nutrient changes due to land use changes in Northern China: a case study in Zunhua County, Hebei Province

Abstract. Since the 1980s, land use in rural areas of China has changed greatly as the result of political initiatives. These changes have caused soil nutrient changes which are examined in this paper for Zunhua County, northern China from 1980 to 1999. The areas of farmland, grassland, and paddy decreased greatly and were replaced by increases in forest and residential land. The soils under forest in 1999 transformed from farmland in 1980 increased in organic matter by 21%, total nitrogen by 18%, available nitrogen by 65%, available phosphorus by 17% and available potassium by 17%. Similarly, in the area which was converted from farmland in 1980 to grassland in 1999, soil organic matter, total nitrogen, available nitrogen, available phosphorus, and available potassium increased by 38%, 37%, 71%, 2% and 28%, respectively. Changes from farmland to forest and grassland not only changed land cover but also improved soil fertility and probably reduced soil nutrient losses.