硅肥对农田镉轻度污染水稻修复效果的研究

为探讨硅肥对农田土壤Cd污染的修复效果,在田间试验条件下,研究了不同硅肥处理对Cd轻度污染农田水稻的修复效果。结果表明:不同硅肥处理可以降低Cd轻度污染农田中水稻糙米Cd含量,降幅为2.02%~16.00%,提高土壤pH值0.36~0.45,降低土壤有效态Cd含量,降幅为34.88%~45.47%,水稻产量增加3.63%~6.23%,基施与叶面喷施联合施用硅肥对农田土壤Cd污染的修复效果最好。     

江苏省风险管控和修复名录地块污染特征分析及对策建议

根据《中华人民共和国土壤污染防治法》,建立并公开《江苏省建设用地土壤污染风险管控和修复名录》（以下简称“名录”）。对2020—2022中江苏省纳入名录的116个污染地块开展系统性分析,结果表明：纳入名录的污染地块数量和面积与地区经济发展水平有关,南京、无锡、常州和苏州排名前列;土水复合污染地块占53%,其中64%的地块地下水最大污染深度大于同一地块土壤最大污染深度;共统计到167种污染物,重金属、石油烃和多环芳烃最为常见,约50%的污染物不在我国现行建设用地土壤及地下水污染评价标准中;已完成修复并移出名录的31个地块中,17%的污染土壤和25%的污染地下水采用原位修复技术。提出了完善土壤环境质量标准体系,探索土水协同治理修复模式,推进土壤污染绿色低碳修复等针对性的对策建议,为促进土壤、地下水环境管理和污染防治行业科学发展提供参考依据。     

镉砷复合污染土壤稳定化修复技术研究与应用

通过实施江西省某农田土壤中镉、砷污染修复项目,对各修复技术进行比选,并对优选出的稳定化修复技术涉及的钝化药归纳分析。通过小试筛选出合适的药剂种类,中试确定药剂的最佳添加量,再进行工程实施的系统性工艺研究和技术应用。结果表明：该技术在保证修复区增产的前提下实现了污染农田土壤的安全利用,形成了控源-降活-低吸-农产品安全达标生产的修复模式,构建了具有针对性的稳定化-农艺调控的联合修复技术体系,可实现重金属污染农田土壤修复、生态建设、经济效益的有机结合。     

陇川县甘蔗土壤pH值时空变化特征及影响因素

通过统计2007年和2020年陇川县甘蔗种植区土壤pH值数据，应用全局Moran，s I指数、冷热点分析、半方差函数和克里金插值等方法对蔗区土壤pH值的时空变化特征及影响因素进行研究，结果表明，2007—2020年蔗区土壤总体呈快速酸化趋势，pH值下降了0.38个单位，降幅达7.54%，与非甘蔗种植区相比，显著下降了1.03个单位。研究区中部和西南部土壤pH值下降显著，在土壤类型上红壤、水稻土和赤红壤的pH值显著下降，降幅分别为10.94%、9.98%和3.83%。在成土母质上第四纪冲积物土壤pH值降幅最大，达0.52个单位。蔗区土壤pH值时空变异主要受人为因素和自然条件的综合影响，人为因素对土壤pH值的变化具有主导作用。     

混合溶剂解吸土壤中多环芳烃的研究

对比了水溶性有机溶剂乙醇、正丙醇、丙酮、已戊醇和水对土壤中多环芳烃(PAHs)的解吸效果,结果综合实验效果、安全性和经济等因素,主要采用了乙醇和戊醇作为混合试剂的主要成分。对比了乙醇、戊醇和水不同配比的混合试剂对土壤的解吸效果,最终选用混合试剂(5%戊醇+20%水+75%乙醇)研究污染土壤中PAHs的解吸行为,分别进行了解吸动力实验、分阶段解吸实验和pH值影响实验。结果表明,土壤中PAHs的解吸是一个快速反应,5h基本达到解吸平衡,高环物质(4～6环PAHs)比低环物质(2～3环PAHs)的解吸速率慢。分步解吸率表明,随着环数的增加,第一步解吸率逐渐降低,第二、三步的解吸率则逐渐增大,第二、三步的解吸作用对高环PAHs更为明显。pH值对混合溶剂解吸土壤中PAHs有显著影响,pH值在5 5～7之间时,对土壤中PAHs的解吸影响最明显,碱性环境(pH>7)有利于土壤中PAHs的解吸,酸性环境则不利于解吸实验的进行。     

钝化材料对Cd污染农田修复及其后效探究

在田间试验条件下,考察不同钝化材料对农田Cd轻度污染水稻修复效果及稻麦轮作后第二年水稻修复后效。结果表明,在轻度Cd污染农田中,各钝化材料处理均能不同程度降低土壤有效态Cd含量和水稻籽粒中Cd含量。其中,在钝化材料施用当季和稻麦轮作后第二季水稻中修复效果最好的处理为中量纳米材料处理和石灰配施中量纳米材料处理,这两种处理对土壤有效态Cd含量降低率分别为50.94%和47.15%,对水稻籽粒中Cd含量降低率分别为73.74%和69.41%。     

铅锌矿区耕地重金属污染土壤环境磁学监测方法研究

用环境磁学方法对甘肃徽县铅锌矿区典型耕地污染土壤、自然土壤和修复土壤进行监测研究,结果表明：污染土壤的磁化率（χlf）与频率磁化率（χfd）呈显著的负相关,表明污染土壤磁性增强主要由铅锌矿厂在选矿冶炼过程中释放的含铁矿物所致;污染土壤χlf值在0 cm～30 cm深度范围内最高,污染严重;χlf值在30 cm～60 cm深度范围内明显降低,污染程度减弱;在60 cm～70 cm深度范围内与自然土壤的χlf值接近,污染基本消失。土壤污染程度随深度增加而降低,污染深度范围为0 cm～60 cm;从污染土壤、修复土壤到自然土壤χlf值依次降低,且污染土壤χlf值与重金属元素Pb、Zn等的变化趋势一致。     

污染场地修复工程环境监理的实践与探索

环境监理是污染场地修复过程中不可或缺的关键环节,在我国起步相对较晚,可供借鉴的实例很少。以苏州市某化工厂遗留场地污染土壤和地下水修复工程为例,阐述了不同阶段环境监理的工作内容,突出了原位和异位修复技术的环境监理工作要点,并提出建立污染土壤和地下水修复效果质量控制体系和原位修复效果长期跟踪监测机制等建议。     

我国典型村庄农村环境质量监测与评价

选取典型村庄,基于农村环境质量监测和评价方法,对典型村庄2014年农村环境质量进行监测和评价,结果表明:典型村庄环境空气质量状况总体良好,达标比例为82.0%,超标村庄多分布在中国西北地区;农村饮用水源地水质较差,总体水质达标比例为67.1%,地表水和地下水饮用水源地水质达标比例分别为89.8%和52.6%;农村地表水环境质量欠佳,Ⅰ~Ⅲ类水质断面占72.7%,饮用水水源地和地表水水质各地区均存在超标村庄;部分地区土壤重金属超标问题较为突出,出现监测项目超标情况村庄占20.6%,土壤超标村庄主要集中在中国东北、华中和华南等地区;农村生态质量状况相对较好,"较差"和"差"的县域主要分布在中国西北和华中北部地区。     

广州市建设用地土壤污染风险管控和修复现状、问题与对策

通过调研广州市已经开展风险管控和修复的污染地块,分析其基本特征、调查评估和治理修复等情况,总结出该市建设用地土壤污染风险管控和修复工作中存在的土壤环境背景值研究缺乏、重金属污染地块修复面临困难、地下水风险管控起步晚、修复过程技术标准缺失等问题,并有针对性地提出开展土壤环境背景值研究、探索重金属污染地块适用修复模式、重视地下水风险管控、完善技术标准支撑体系等对策建议。     

乌鲁木齐河水环境质量及变化趋势分析

通过对乌鲁木齐河近十年(2001—2010年)水质监测数据的分析,结果表明,"十一五"期间乌鲁木齐河上游水质较好,为Ⅰ类或Ⅱ类水质,中下游均受到较为严重的有机污染,为劣Ⅴ类水质,主要污染物为粪大肠菌群、化学需氧量、氨氮、石油类;各监测断面水质总体保持稳定,水质污染形势依然严峻。水污染治理措施取得一定成效。与"十五"相比,"十一五"期间乌鲁木齐河水质明显改善,综合污染指数进一步下降,跃进桥断面水质类别由Ⅱ类水质变为Ⅰ类,英雄桥断面水质类别由Ⅲ类水质变为Ⅱ类。根据分析评价结果,提出了改善水环境质量的对策和建议。     

An Environmentally Sound Method for Disposal of Both Ash and Sludge Wastes by Mixing with Soil: A Case Study of Bangkok Plain

This study reported the test done on ash-sludge mixture foramendment of soil in pot experiments. Ash-sludge mixture ratiostudies revealed that 1:5 fly ash-sludge mixture and 1:10 bottom ash-sludge mixture were the optimum mixture ratio thatminimized toxic element and provided sufficient nutrients. Experiments indicated that ash-sludge mixtures is more suitablefor amendment of acid soil than neutral soil which can increasesoil pH and reduce available heavy metal toxicity. The maximumheavy metal adsorption occurred in a pH range of 4 to 6 for allsoil studied. The finding also revealed that fly ash applicationseemed more effective than bottom ash, due to its higher loadingrate and metal contents. Heavy metal toxicity was monitored usingseed germination test. Marigold and tomato seeds were the two crops selected for this test. Seed germination test result showsthat percentage of seed germination increased in pot experimentswith sludge only and ash-sludge mixtures. In addition, higherpercentages of seed germination were observed to vary with longer incubation time (1–8 weeks). After week 12 of the incubation period, percentage of seed germination began to decline, as a result of reduced soil pH and release of toxic heavy metals.     

Effects of soil amendments on the bioavailability of heavy metals from zinc mine tailings

A study was conducted to test the effects of soil amendments on the bioavailability of heavy metals in a zinc mine tailings containing soil to plants, using the Indian mustard plant (Brassica juncea) as a test organism. Zinc mine tailing containing soil was amended with humus soil (HS) and phosphatic clay (PC). The zinc mine tailing containing soil (ZMTS) was characterized for heavy metals. It was mixed with PC and HS, and four mixtures were prepared. The first mixture contained ZMTS, and served as a control. The second mixture contained ZMTS and PC in the ratio of 1:1 (w/w). The third mixture contained ZMTS and HS in the ratio of 1:1(w/w). The fourth mixture containing ZMTS, PC and HS in the ratio of (2:1:1) (w/w). A slight increase in the bioavailability of Pb, Cu, Zn and Mn was noticed with increase in the incubation time from 14 to 42 days. The bioavailability of Pb, Cu, Zn and Mn from ZMTS alone in Brassica plant was in the range of 94-99% up to 42 days. Addition of PC and HS to the ZMTS soil reduced the bioavailabilities of Pb by (15%), of Cu by (20%), of Zn by (20%) and of Mn by (25%) in the mustard plant. The data showed that PC in the presence of HS had a high affinity for the heavy metals in the order of Pb, Cu, Zn and Mn.     

高效液相色谱法测定稻田中丙草胺残留

用二氯甲烷提取稻田水和水稻植株样品中的丙草胺，稻田土壤样品用二氯甲烷-甲醇混合溶剂（体积比为9∶1）提取，再用高效液相色谱仪测定。方法在0．02 mg/L～2．00 mg/L的范围内线性良好，相关系数为0．9998；稻田水、土壤，水稻植株中丙草胺的检出限分别为0．001 mg/L、0．005 mg/kg、0．01 mg/kg；对稻田水、土壤和水稻植株分别做3个浓度水平的加标回收试验，重复5次，平均回收率在75．5％～84．7％之间，测定结果的相对标准偏差为2．0％～10．5％。     

GC-C-IRMS测定污染场地土壤中苯系物单体碳同位素比值

选取苯系物中的代表性组分苯、甲苯和二甲苯等化合物,通过热脱附、气相色谱质谱条件的优化及方法学考察,建立了热脱附进样-气相色谱-同位素比值质谱(GC-C-IRMS)测定苯系物单体碳同位素比值的方法。结果表明,单体化合物进样量在0.3μg以上均能满足测定要求;与直接进样方式相比,热脱附进样对单体碳同位素比值测定无分馏影响;标准溶液和苯系物土壤样品测定结果的RSD分别为1.0%~1.7%和0.3%~2.6%。     

Labile pools of Pb in vegetable-growing soils investigated by an isotope dilution method and its influence on soil pH

Pollution of Pb in the surface of agricultural soils is of increasing concern due to its serious impact on the plant growth and the human health through the food chain. However, the mobility, activity and bioavailability of Pb rely mainly on its various chemical species in soils. In the present study, E and L values, the labile pools of isotopically exchangeable Pb, were estimated using the method of isotope dilution in three vegetable-growing soils. The experiments involved adding a stable enriched isotope ((206)Pb > 96%) to a soil suspension and to soils in which plants are subsequently grown, the labile pools of Pb were then estimated by measuring the isotopic composition of Pb in soil solutions and in the plant tissues, respectively. In addition, the correlation of E values and soil pH was investigated at the ranges of pH 4.5-7.0. The amount of labile Pb in soils was also estimated using different single chemical extractants and a modified BCR approach. The results showed that after spiking the enriched isotopes of (206)Pb (>96%) for 24 hours an equilibration of isotopic exchanges in soil suspensions was achieved, and the isotope ratios of (208)Pb/(206)Pb measured at that time was used for calculating the E(24 h) values. The labile pools of Pb by %E(24 h) values, ranging from 53.2% to 61.7% with an average 57%, were found to be significantly higher (p < 0.05) than the values estimated with L values, single chemical extractants and the Σ(BCR) values obtained with the BCR approach, respectively. A strong negative correlation (R(2) = 0.984) between E(24 h) values and soil pH was found in the tested soil sample. The results indicate that the %E(24 h) value can more rapidly and easily predict the labile pools of Pb in soils compared with L values, but it might be readily overestimated because of the artificial soil acidity derived from the spiked isotopic tracer and the excess of spiked enriched isotopes. The results also suggest that the amounts of Pb extracted with EDTA and the Σ(BCR) values extracted with the modified BCR approach are helpful to detect the labile pools of Pb in soils. In addition, the negative correlation between soil pH and the labile pools of Pb in soils may be useful for further remediation to reduce the bioavailability of Pb in contaminated soils.     

Accumulation of different sulfur fractions in Chinese forest soil under acid deposition

Atmogenic sulfur (S) deposition loading by acid rain is one of the biggest environmental problems in China. It is important to know the accumulated S stored in soil, because eventually the size (and also the "desorption" rate) determines how rapidly the soil water pH responds to decrease in S deposition. The S fractions and the ratio of total carbon/total sulfur (C/S) of forest soil in 9 catchments were investigated by comparing soils at the rural and urban sites in China. The S fractions included water-soluble sulfate-S (SO(4)-S), adsorbed SO(4)-S, insoluble SO(4)-S and organic S. The ratio of C/S in soil at the rural site was significantly (p < 0.05) greater than that at the urban site. C/S of soil in the A horizon was significantly (p < 0.05) and negatively correlated with the wet S-deposition rate. The ratio of C/S presents a better indicator for atmogenic S loading. Organic S was the dominant form in soils at rural sites; contributing more than 69% of the total S in the uppermost 30 cm soil. Organic S and adsorbed SO(4)-S were the main forms of S in soil at urban sites. High contents of water-soluble SO(4)-S and adsorbed SO(4)-S were found in uppermost 30 cm soils at urban sites but not at rural sites. Decades of acid rain have caused accumulation of inorganic SO(4)-S in Chinese forest soil especially at the urban sites. The soil at urban sites had been firstly acidified, and the impacts on the forest ecosystem in these areas should be noticed.     

The combined use of electrokinetic remediation and phytoremediation to decontaminate metal-polluted soils: a laboratory-scale feasibility study

The use of a combination of electrokinetic remediation and phytoremediation to decontaminate two metal-polluted soils has been demonstrated in laboratory-scale reactors. One soil was heavily contaminated with copper, the other with cadmium and arsenic (2500 g g^-1 Cu; 300-400 g g^-1 Cd and 230 g g^-1 As, respectively). Test reactors with twoseparated chambers, each with a capacity of 5.25 kg soil, wereconstructed, then the respective chambers were filled with eithera mixture of the polluted soil and a control topsoil (75:25) ortopsoil alone. Reactors were sown with perennial ryegrass (Lolium perenne cv Elka) and a constant voltage of 30 V was applied continually across the soils in each reactor. Soil sampling took place at the start and the end of the test run, whilst plant foliage was sampled after approximately 3 weeks (both reactors) 6 weeks (Cd soil reactor only) and at the conclusion of each test run (98 days Cu soil, 80 days Cd soil). Soil and plant metal concentrations were measured, together withsoil pH. Results showed that in both soils there was a significant re-distribution of metals from anode to cathode in the test reactors, coupled with an enhancement of plant Cu uptakein the cathode region for the Cu soil. Patterns of plant Cd uptake were less clear cut and were not as clearly related to theredistribution of Cd measured in the soil. There was significant acidification of soil at the anode in each test reactor, but soilpH in other parts of the reactor changed little during the courseof the experiment. Plant growth was affected at the anode, but was not affected in other parts of the reactor. There was no visual evidence of metal toxicity in the ryegrass in either polluted soil. Some effects on soil fungi were apparent, with a stimulation of Fusarium infection of ryegrass in the cathode region of all reactors and the appearance of sporophoresof Coprinus in the same location. It is concluded that the combination of the two techniques represents a very promising approach to the decontamination of metal polluted soils that nowrequires validation in field conditions.