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961.
962.
963.
Cu是大众生活中经常接触的重金属之一,它在土壤中的量很高时也会给生态、人体带来伤害.同时土壤Cu污染的修复方法很多,现对其化学修复原理作一个探讨. 相似文献
964.
Influence of Spartina alterniflora on the mobility of heavy metals in salt marsh sediments of the Yangtze River Estuary, China 总被引:1,自引:0,他引:1
Yongjie Wang Limin Zhou Xiangmin Zheng Peng Qian Yonghong Wu 《Environmental science and pollution research international》2013,20(3):1675-1685
Using bio-disturbed sulphide to trace the mobility and transformation of Cu, Pb, Ni and Zn in the sediments of the Spartina alterniflora-dominated salt marsh in the Yangtze River Estuary, measurements were made of the seasonal variations of acid-volatile sulphide (AVS) and of the simultaneously extracted metals (SEM) in the rhizosphere sediments. Microcosm incubation experiments recreating flooding conditions were conducted to evaluate the effect of AVS and other metal binding phases upon the dynamics of Cu, Pb, Ni and Zn in the salt marsh sediments. The results demonstrate that the ratio values of SEM/AVS have a significant seasonal variation in the rhizosphere sediments and that the anoxic conditions in the sediments were likely enhanced by S. alterniflora during the summer and autumn compared with the anoxic conditions resulting from the native species Phragmites australis and Scirpus mariqueter. The incubation experiments suggest that Fe(III) and Mn(IV/III) (hydr)oxides provide important binding sites for heavy metals under oxic conditions, and sulphide provides important binding sites for the Cu and Pb under anoxic conditions. Our observations indicate that the mobility of heavy metals in the salt marsh sediments is strongly influenced by biogeochemical redox processes and that the invasive S. alterniflora may increase the seasonal fluctuation in heavy metal bioavailability in the salt marsh ecosystem. 相似文献
965.
Li Q. Liu L. Cai Y. Pei S. Luo Y. Liu L. Fan H. Sun F. Zhou C. Shen X. Chen Y. 《应用与环境生物学报》2018,(3):441-449
Desertification has emerged as a serious threat to the alpine meadows of Northwest Sichuan in recent decades. Artificial vegetation had certain effects on desertification recovery, while how the CO2 flux changed and its reasons are still unclear. During the growing season in 2016 (i.e., from July to September), we selected the desertified alpine meadows with different recovery degrees, including the early stage of restoration, the middle stage of restoration, the late stage of restoration, and control (the unrecovered desertification meadow) as four transects. CO2 flux was measured by the instrument LI-8100, and the microenvironment factors that affected CO2 flux changes were analyzed. The results showed that the carbon sequestration function of desertified alpine meadows gradually increased with the degree of recovery. Net ecosystem exchange (NEE) were -1.61, -3.55, and -4.38 μmol m-2 s-1 in the early, mid-term, and late transects, respectively, and the most dramatic changes occurred from the early stage to mid-term stage, increasing by 120.50%. Both ecosystem respiration (ER) and soil respiration (SR) were enhanced significantly with restoration (P < 0.05). In mid or late July, NEE, ER, and SR reached their maximum values, and thereafter, the indicators varied to near zero (P < 0.05). During the whole growing season, the daily dynamic in CO2 flux for the control alpine meadow was mild and retained the trend of continuous release all day, but that in the desertified alpine meadow was a single peak pattern. Moreover, with restoration process, the peak of CO2 flux increased and reached a peak in the late stage of the recovery process. The regression analysis showed that there was a significant positive correlation between CO2 flux and vegetation coverage, aboveground biomass, and soil moisture (0-5 cm) (P < 0.01), and a weak correlation with 0-5-cm soil temperature (P < 0.01). This indicates that topsoil moisture (5 cm) is a more significant factor for CO2 flux than topsoil temperature during the growing season in the restoration of desertified alpine meadows in Northwest Sichuan. In general, the vegetation recovery significantly improved the carbon-sequestration ability of the desertified alpine meadows during the growing season in Northwest Sichuan, and at the middle stage of restoration, the carbon-sequestration ability improved significantly due to vegetation restoration and increase in topsoil (0-5 cm) moisture. © 2018 Science Press. All rights reserved. 相似文献
966.
土地利用方式对紫色土丘陵区土壤剖面碳、氮影响 总被引:3,自引:0,他引:3
采取野外调查与室内分析相结合的方法研究了紫色土丘陵区林地、撂荒地、水田、旱地土壤剖面(0~40 cm)有机碳、全氮变化特征.结果表明.有机碳、全氮均随土层深度增加而逐渐减小,且林地、撂荒地有机碳递减幅度高于水田、旱地.相对于撂荒地和旱地,水田、林地更利于有机碳、全氮的积累.林地有机碳和全氮在0~5 cm土层表现出绝对优势;随土层递增,与水田、撂荒地和旱地的差异逐渐减小.水田有机碳和全氮在大于10 cm土层显示最大值.而撂荒地有机碳和全氮仅在土壤表层高于旱地.有机碳与全氮存在显著正相关关系;w(C)/w(N)随土层深度增加而降低,且林地、撂荒地降低幅度较大.因此相对于水田、旱地,林地和撂荒地w(C)/w(N)仅在0~10 cm显示较大值.可见,土地利用方式对陆地生态系统碳、氮蓄积有明显影响,通过旱地还林或撂荒可以增加土壤特别是表层土壤对碳、氮的积累. 相似文献
967.
Fenton-混凝法处理焦化废水的试验研究 总被引:12,自引:0,他引:12
对Fenton预氧化-混凝法联用技术处理焦化废水进行了研究,探讨了Fenton氧化阶段H2O2投加量、混凝阶段pH值以及混凝剂投加量等因素对焦化废水COD去除率的影响,确定了最佳处理条件。结果表明,Fenton预氧化一混凝法处理焦化废水取得了良好效果,COD去除率达97.5%,为该工艺实际处理焦化废水提供了实验依据。 相似文献
968.
969.
Fang Fang Yan Yang Jinsong Guo Hong Zhou Chuan Fu Zhe Li 《Frontiers of Environmental Science & Engineering in China》2011,5(3):426-434
Three-dimensional fluorescence spectroscopy was used to investigate the fluorescent properties of soil dissolved organic matter
(DOM) in the water-level-fluctuation zone (WLFZ) of Kai County, Three Gorges Reservoir (TGR). Most of the soil DOM analyzed
in this study was found to contain four fluorescence peaks. Peaks A and C represent humic-like fluorescence, whereas peaks
B and D represent tryptophan-like fluorescence. Peaks E and F, which represent tyrosine-like fluorescence, only appeared in
certain soils. Soil humus was the main source of DOM in soil, and higher concentration of soil DOM was found in the exposed
soil than submerged soil. Compared to the peaks A and B, the fluorescence intensities of peaks C and D were strongly influenced
by the fluctuating water level. Analysis of fluorescence intensities of different peaks in soil DOM showed that WLFZ soil
was not contaminated significantly. Soil DOM contained at least two types of humic-like fluorescence groups and two types
of protein-like fluorescence groups. The proportion of the content of peak A in soil organic matter was quite stable. The
soil DOM in exposed soil had relatively high humification and aromaticity, and periodic submerging and exposure of soil had
an impact on the humification of soil DOM. 相似文献
970.