广东某含铊硫酸冶炼堆渣场土壤中重金属的污染特征

选取广东某硫酸厂工业堆渣周围土壤样品,重点研究了土壤剖面T1、cd、Pb、Zn四种重金属元素总量及形态分布特征.研究结果表明,该废渣在自然淋滤条件下已经对周围土壤产生了T1、Cd、Pb、Zn污染,并且T1、Pb、Cd较Zn污染严重.形态分析表明,堆渣场周围土壤中这些重金属主要是以残渣态和铁锰氧化物(氢氧化物)结合态存在.外围土壤受到的这些重金属污染及对环境的潜在危害大于废渣下伏土壤,其中在堆渣下伏土壤中主要以富集为主,而外围土壤中主要以迁移为主,且已经向土壤深处约30cm处进行了迁移.这些重金属污染物在表层土壤中未达到饱和状态,将继续在下伏土壤表层发生累积作用并且使横向土壤受污染的范围进一步扩大.     

快速溶剂提取-气相色谱法测定土壤中19种多氯联苯单体

采用快速溶剂提取-Florisil固相萃取柱净化-气相色谱法测定土壤中多氯联苯单体,探讨了有机氯农药对测定的干扰。方法在0ug／L-100ug／L范围内线性良好,19种多氯联苯单体的检出限为0．06ug／kg-0．36ug／kg,基体加标回收率为78．6％-120％,RSD为0．2％-5．1％。     

POPs监测技术在环境样品中应用

利用超声提取、固相萃取(SPE)净化和GC-MS技术对某市四个区的的果蔬基地7个土壤样品进行了土壤中持久性有机氯污染物分析.结果显示,土壤样品中主要有机污染物为γ-HCH、异狄氏剂和α-HCH,其中γ-HCH的检出率为100%,不同样品中γ-HCH和异狄氏剂差异明显,异狄氏剂和α-HCH检出率分别为86%和71.4%.     

Health Risks Associated with Predicted Increase of Cadmium in Cultivated Soils and in the Diet

We have assessed the change of the dietary intake and the potential health risks of cadmium in Finland, assuming that a high level of cadmium in fertilizers (138 mg Cd/kg P) would prevail for the next 100 years. Soil measurements and modelling were used to derive the predicted level of cadmium in foods. In three important cultivars, wheat, potato and sugar beet, the cadmium concentration would increase by 20–35%. Consequently, the average dietary intake of cadmium in Finland would increase from 7.9 to 10.0 μg/day, corresponding with the urinary level of about 0.2 μg/l, a level that has not been associated with effects on the human health. However, in the risk group with 1) high dietary intake of cadmium, 2) elevated gastrointestinal absorption, and 3) tobacco smoking, the estimated urinary level of cadmium would be 2.0 μg/l. Recent epidemiological studies have shown that urinary level of 1–2 μg Cd/l is associated with an increased risk of bone demineralization and fractures, and 2–4 μg Cd/l with pre-clinical kidney damage. People characterized by more than one of the above-mentioned risks factors, may develop the adverse health effects at an old age, when cadmium has accumulated in the body.     

超声波萃取/气相色谱法测定土壤中的多氯联苯

采用超声波萃取法提取土壤中的多氯联苯系列7种混合物Arochlor1016、Arochlor1221、Arocldor1232、Arochlor1242、Arochlor1248、Arochlor1254、Arochlor1260,萃取溶液经弗罗里硅土柱净化,用气相色谱GC/ECD进行测定,方法检出限0.01mg/kg,加标回收率在62.3%～106%之间,RSD 5.4%～11.1%.     

4种替代植物对黄顶菊入侵土壤养分和酶活性的影响

入侵植物对土壤环境的影响是植物竞争取胜的重要生态策略之一,而选择合适的植物可以替代控制和抵御外来植物的入侵。比较了高丹草、向日葵、紫花苜蓿和多年生黑麦草4种植物与黄顶菊单种和混种后不同时期的土壤养分和土壤酶活性变化规律。结果表明：（1）黄顶菊单独种植根区土壤NH4＋-N、NO3-N含量均显著低于紫花苜蓿和黄顶菊混种群落,其有效磷含量显著低于高丹草和黄顶菊混种群落;（2）紫花苜蓿和黄顶菊混种群落土壤脲酶、磷酸酶、蔗糖酶活性均显著高于黄顶菊单种群落。因此,在本试验条件下,高丹草、紫花苜蓿对土壤氮素转化利用能力比黄顶菊高,且能竞争性抑制黄顶菊对土壤磷素的吸收,利于实现对黄顶菊的替代控制。     

Uncertainty in future soil carbon trends at a central U.S. site under an ensemble of GCM scenario climates

This study uses DAYCENT model to investigate the sensitivity of soil organic carbon (SOC) at an intensely cultivated site in the U.S. Midwest under an ensemble of scenario climates predicted by IPCC models. The model ensemble includes three IPCC models (Canadian, French, German), three emission scenarios (B1, A1B, A2) and three time periods (late 20th, mid-21st, late 21st century). DAYCENT shows that SOC at the site would decline by 0.3-2.6 kg m⁻² (5-35%) depending on the models and scenarios from late 20th to mid-21st century despite a larger increase of future net primary production (NPP) than respiration. The future SOC decrease is mostly attributable to harvest loss. The wide spread in future SOC decline rates are in part because SOC decrease (by respiration) is directly proportional to SOC itself. Any uncertainty in absolute SOC in DAYCENT would translate directly into its trend, unlike other variables such as temperature whose trends are independent of their values themselves, contrasting the reliability of SOC trend with temperature change.     

Vegetation competition model for water and light limitation. I: Model description, one-dimensional competition and the influence of groundwater

Vegetation growth models often concentrate on the interaction of vegetation with soil moisture but usually omit the influence of groundwater. However the proximity of groundwater can have a profound effect on vegetation growth, because it strongly influences the spatial and temporal distribution of soil moisture and therefore water and oxygen stress of vegetation. In two papers we describe the behavior of a coupled vegetation-groundwater-soil water model including the competition for water and light. In this first paper we describe the vegetation model, compare the model to measured flux data and show the influence of water and light competition in one dimension. In the second paper we focus on the influence of lateral groundwater flow and spatial patterns along a hillslope. The vegetation model is based on a biophysical representation of the soil-plant-atmosphere continuum. Transpiration and stomatal conductance depend both on atmospheric forcing and soil moisture content. Carbon assimilation depends on environmental conditions, stomatal conductance and biochemical processes. Light competition is driven by tree height and water competition is driven by root water uptake and its water and oxygen stress reaction. The modeled and measured H₂O and CO₂ fluxes compare well to observations on both a diurnal and a yearly timescale. Using an upscaling procedure long simulation runs were performed. These show the importance of light competition in temperate forests: once a tree is established under slightly unfavorable soil moisture conditions it can not be outcompeted by smaller trees with better soil moisture uptake capabilities, both in dry as in wet conditions. Performing the long simulation runs with a background mortality rate reproduces realistic densities of wet and dry adapted tree species along a wet to dry gradient. These simulations show that the influence of groundwater is apparent for a large range of groundwater depths, by both capillary rise and water logging. They also show that species composition and biomass have a larger influence on the water balance in eco-hydrological systems than soil and groundwater alone.     

Estimation of annual potential evapotranspiration at regional scale based on the effect of moisture on soil respiration

Potential evapotranspiration (PET) is an important component of water cycle. For traditional models derived from the principle of aerodynamics and the surface energy balance, its calculation always includes many parameters, such as net radiation, water vapor pressure, air temperature and wind speed. We found that it can be acquired in an easier way in specific regions. In this study, a new PET model (PETP model) derived from two empirical models of soil respiration was evaluated using the Penman-Monteith equation as a standard method. The results indicate that the PETP model estimation concur with the Penman-Monteith equation in sites where annual precipitation ranges from 717.71 mm to 1727.37 mm (R² = 0.68, p = 0.0002), but show large discrepancies in all sites (R² = 0.07, p = 0.1280). Then we applied our PETP model at the global scale to the regions with precipitation higher than 700 mm using 2.5° CMAP data to obtain the annual PET for 2006. As expected, the spatial pattern is satisfactory overall, with the highest PET values distributed in the lower latitudes or coastal regions, and with an average of 1292.60 ± 540.15 mm year⁻¹. This PETP model provides a convenient approach to estimate PET at regional scales.     

Experimental Zn(II) retention in a sandy loam soil by very small columns

The use of column experiments, usually performed to better approximate field conditions, may provide information that is not available from batch experiments. In such experiments heavy metals are often adsorbed until saturation followed by desorption experiments. When the affinity of the metal to soil is high, the retention factor (R) could be greater than thousands and the duration of experiments can become impractically long. In order to use reasonable laboratory time, the flow rate should be increased or the column size decreased. The increase in flow rate produces undesirable kinetic and dispersion effects, so we used very small soil columns (pore volume = 0.31–0.70 ml) and relatively high flow rates (0.03–0.12 ml min⁻¹) in studies of Zn(II) adsorption and retention in soils. Conservative tracer flow column experiments under saturation conditions were carried out to determine flow parameters for different flow rates. Column pore volume (V_p), Peclet numbers (Pe) and longitudinal dispersion coefficients (D_L) were determined from breakthrough curves. The effect of type of electrolyte and ionic strength on the Zn(II) retention onto soil was determined. The influence of flow rate and bed height on the retention coefficient and on the mass transfer zone was also studied. The effect of different influent Zn(II) concentrations on the R values obtained was analyzed. Freundlich parameters from column experiments were compared with batch ones. The leaching efficiency of different electrolytes, salts of weak organic acids and EDTA was also studied.