Do trace metal(loid)s in road soils pose health risks to tourists? A case of a highly-visited national park in China

Nowadays, more people tend to spend their recreational time in large national parks, and trace metal(loid)s in soils have attracted long-term attention due to their possible harm to human health. To investigate the pollution levels, potential sources and health risks of trace metal(loid)s in road soils, a total of eight trace metal(loid)s (including As, Cd, Cr, Cu, Ni, Pb, Zn and Hg) from 47 soil samples along roads were studied in the Huangshan National Park in Southeast China. The results showed that the concentrations of As, Cd, Pb, Zn and Hg appeared different degrees of pollution compared with their corresponding background values. According to the pollution indices, Hg and Cd were recognized as significant pollutants presenting moderate to high ecological risk. Combining principal component analysis and positive matrix factorization model, the results showed that traffic, industrial, agricultural and natural sources were the potential origins of trace metal(loid)s in this area, with contribution rates of 39.93%, 25.92%, 10.53% and 23.62%, respectively. Non-carcinogenic risks were all negligible, while the carcinogenic risk of As was higher than the limit (1 $\times$ 10⁻⁶). Moreover, children were more susceptible to trace metal(loid)s by ingestion which appeared to be a more important exposure pathway than dermal contact and inhalation. The contribution rates of different sources to non-carcinogenic risks and carcinogenic risks were similar among children and adults, while traffic and industrial sources have a significant impact on health risks. This study will give more insights to control the environmental risks of trace metal(loid)s in national parks.     

粉末活性污泥处理含铀废水的特性

以生活污水处理厂剩余活性污泥为原料,制备粉末活性污泥(PAS)作为生物吸附剂,考察p H值,PAS投加量,U(Ⅵ)初始浓度和吸附时间对PAS吸附U(Ⅵ)的影响,探讨了PAS吸附U(Ⅵ)的作用机理。实验结果表明,在U(Ⅵ)初始浓度为10 mg/L时,其最佳吸附p H值为3,去除率97.77%,吸附平衡时间120 min;吸附过程较好地拟合了准二级动力学模型(R2≈1)和Freundlich等温模型(R2≈1);X射线能谱和离子交换实验分析表明,离子交换为其主要吸附方式,参与交换的主要离子为Ca2+;红外光谱分析表明,PAS吸附U(Ⅵ)后自身结构未发生改变。以0.1 mol/L的HCl溶液作为解吸液,初次解吸率达92.83%,循环利用3次仍具有较好的吸附效果。     

催化荧光法测定痕量亚硝酸根

本文研究了在稀磷酸介质中，亚硝酸根对溴酸钾氧化中笥红的反应，建立了催化荧光法测定痕量亚硝酸根的方法，实验表明，亚硝酸根在０．０５－０．４０μｇ．２５ｍｌ＾－１范围内与ΔＦ成线性关系，大多数常见的共存离子不影响其测定。本法用于水样中亚硝酸根的测定，结果比较满意。     

山西省五台山区土壤氟元素的环境背景值及分布规律

对山西省五台山区垂直土壤主要土类的氟元素背景值进行了调查与分析，揭示了五台山区土壤氟元素区域背景的分布特征和变化趋势。结果表明：五台山区土壤氟背景值略高于我国平均水平，多数土壤Ｂ层含氟量最高。     

福建丰产荔枝园土壤微量元素含量的研究

与我国红壤平均水平相比，福建丰产荔枝园土壤有效态锌、钼及水溶态硼含量较高，而活性锰及有效铜含量较低；土壤全锌、锰、钢量亦较低。在土壤ｐＨ４．５４—８．７６时，ｐＨ值与有效态钼含量呈较显著正相关，而与代换态锰、水溶态硼、有效态铁含量呈显著或极显著负相关。本文初步提出福建荔枝园土壤微量元素含量的适宜指标，可供土壤营养诊断及平衡施肥之参考。     

分光光度法测定水稻土中有机酸的研究

本文以三种有机酸为代表,研究并建立了测定水稻土中有机酸的分光光度法。结果表明,三种有机酸的有色络合物具有相同的吸收光谱,且具有相同的最大吸收波长(λ_(mss)=500um)和相近的表观摩尔吸光系数。水分对酯化反应影响很大,含水量达4ml时,吸光值下降85％。酯化温度在10℃以上时,酯化率达最大值且保持稳定。在25℃时,显色反应20min趋干稳定,且在1h内吸光值下降不超过1.2％。土样中的有机酸采用NaCl溶液为提取剂,以3:1的液土比振荡提取30min,NaCl溶液浓度为1％就能达到良好的提取、过滤效果。提取液在烘干前需进行碱化,否则有机酸将损失30％以上。本法平均回收率为92.2％(n=5),标准差为0-0.0478cmol k8~(-1)(n=2-6),平均0.0142cmol kg~(-1)(n=26);变异系数为0—10％(n=2-6),平均4.87％(n=26);线性范围为0—0.0018mol L~(-1)。     

知识经济时代的企业经营与管理

21世纪经济正向着知识经济时代迈进.知识经济不仅对人类的生产方式和生活方式产生着深远影响,而且对企业的经营方式和管理模式也将产生深远的影响.我国企业在知识经济时代下,如何转变和调整经营与管理方式己成为新世纪的重大课题.     

沈阳市烟囱分布对大气污染的影响

本文介绍采用航空遥感技术和实地调查研究相结合的方法,分析了沈阳市烟囱数量、高度、密度以及高、中、低架烟囱的分布状况和特点,同时与大气污染监测结果对照分析了沈阳市煤烟型大气污染的规律及特点,研究了沈阳市烟囱分布对大气污染的影响。最后,提出了沈阳市燃煤污染的防治途径。     

Atmospheric sulfur deposition onto different ecosystems over China

The regional acid deposition model system (RegADMS) was applied to simulate the air sulfur deposition onto different landuse types over China, in which the dry deposition velocities of SO2 and sulfate aerosol (SO4(2-) were estimated by use of a big leaf resistance analogy model and the wet scavenging coefficients were parameterized in terms of precipitation rate. Investigations show that the annual total sulfur deposition over mainland China is 7.24mt (1 mt = 10(6) ton) , in which dry deposition and wet deposition accounts for 56 and 44%, respectively. The sulfur deposition onto agriculture land, grass land, and forest land is 1.09, 3.6 and 1.41 mt, respectively, which sums 6.1 mt and accounts for 84% of the total sulfur deposition. The modeled sulfur deposition was in agreement with the measurement conducted at farmland in Yingtan, a typical read soil region in Jiangxi province of China, during the period of November 1998--October 1999. The total sulfur deposition at the Yingtan site is about 10.3 gm(-2) year(-1) of which 83% is dry deposition. The modeling sulfur deposition at the same site is 8.4 g m(-2) year(-1) Furthermore, the comparison between RegADMS and RAINS-ASIA on modeling regional sulfur deposition shows the consistence of the two models. The correlation coefficient between the simulated sulfur deposition at the medium-large cities reaches 0.72.     

Field Studies on 32P Movement and P Leaching from Flooded Paddy Soils in the Region of Taihu Lake, China

Field experiments were done in two sites, Yixing and Changshu, Jiangsu province, China, to study P movement and leaching in flooded paddy soils. P movement in soil was investigated by using the KH₂ ³²PO₄ tracker method, and the amount of P leached from the soil layer in different depths was estimated by measuring P concentrations in the soil solution and saturated hydraulic conductivities in field. Determination was done about one month after P application. There was 46% and 42% of total ³²P retained in the 0–5cm layer of soil in the Yixing site and in the Changshu site respectively. The ³²P retained in the 25–30 cm layer was only about 1–2% of the total ³²P added. Furthermore, 8.01% of ³²P in the soil of Yixing site and 16.8% of ³²P in the soil of Changshu site was lost from the layer 0–30cm soil. The seasonal amounts of P leached from the top soil layer and from bottom layer are about 4.5–5.8% and 1.6–2.1% of the total P application, respectively. Changes of total P concentrations in soil solutions during rice growth showed that the fertilizer P applied before flooding of the paddy fields suffered a flash leaching loss and a slow leaching loss. We concluded that the fertilizer P could quickly move in the flooded paddy rice field and parts of it can enter into surface water and ground water. Unless the P application is well managed the risk of P loss and consequently environmental pollution exist.