Phosphorus recovery from biogas fermentation liquid by Ca–Mg loaded biochar

Shortage in phosphorus (P) resources and P wastewater pollution is considered as a serious problem worldwide. The application of modified biochar for P recovery from wastewater and reuse of recovered P as agricultural fertilizer is a preferred process. This work aims to develop a calcium and magnesium loaded biochar (Ca–Mg/biochar) application for P recovery from biogas fermentation liquid. The physico-chemical characterization, adsorption efficiency, adsorption selectivity, and postsorption availability of Ca-Mg/biochar were investigated. The synthesized Ca–Mg/biochar was rich in organic functional groups and in CaO and MgO nanoparticles. With the increase in synthesis temperature, the yield decreased, C content increased, H content decreased, N content remained the same basically, and BET surface area increased. The P adsorption of Ca–Mg/biochar could be accelerated by nano-CaO and nano-MgO particles and reached equilibrium after 360 min. The process was endothermic, spontaneous, and showed an increase in the disorder of the solid–liquid interface. Moreover, it could be fitted by the Freundlich model. The maximum P adsorption amounts were 294.22, 315.33, and 326.63 mg/g. The P adsorption selectivity of Ca–Mg/biochar could not be significantly influenced by the typical pH level of biogas fermentation liquid. The nano-CaO and nano-MgO particles of Ca–Mg/biochar could reduce the negative interaction effects of coexisting ions. The P releasing amounts of postsorption Ca–Mg/biochar were in the order of Ca–Mg/B600 > Ca–Mg/B450 > Ca–Mg/B300. Results revealed that postsorption Ca–Mg/biochar can continually release P and is more suitable for an acid environment.     

Diurnal and spatial variations of soil NOx fluxes in the northern steppe of China

NO_x emissions from biogenic sources in soils play a significant role in the gaseous loss of soil nitrogen and consequent changes in tropospheric chemistry. In order to investigate the characteristics of NO_x fluxes and factors influencing these fluxes in degraded sandy grasslands in northern China, diurnal and spatial variations of NO_x fluxes were measured in situ. A dynamic flux chamber method was used at eight sites with various vegetation coverages and soil types in the northern steppe of China in the summer season of 2010. Fluxes of NO_x from soils with plant covers were generally higher than those in the corresponding bare vegetation-free soils, indicating that the canopy plays an important role in the exchange of NO_x between soil and air. The fluxes of NO_x increased in the daytime, and decreased during the nighttime, with peak emissions occurring between 12:00 and 14:00. The results of multiple linear regression analysis indicated that the diurnal variation of NO_x fluxes was positively correlated with soil temperature (P < 0.05) and negatively with soil moisture content (P < 0.05). Based on measurement over a season, the overall variation in NO_x flux was lower than that of soil nitrogen contents, suggesting that the gaseous loss of N fromthe grasslands of northern China was not a significant contributor to the high C/N in the northern steppe of China. The concentration of NO_x emitted from soils in the region did not exceed the 1-hr National Ambient Air Quality Standard (0.25 mg/m³).     

Can arbuscular mycorrhiza and fertilizer management reduce phosphorus runoff from paddy fields?

Our study sought to assess how much phosphorus (P) runoff from paddy fields could be cut down by fertilizer management and inoculation with arbuscular mycorrhizal fungi. A field experiment was conducted in Lalin River basin, in the northeast China: six nitrogen–phosphorus–potassium fertilizer levels were provided (0, 20%, 40%, 60%, 80%, and 100% of the recommended fertilizer supply), with or without inoculation with Glomus mosseae. The volume and concentrations of particle P (PP) and dissolved P (DP) were measured for each runoff during the rice growing season. It was found that the seasonal P runoff, including DP and PP, under the local fertilization was 3.7 kg/ha, with PP, rather than DP, being the main form of P in runoff water. Additionally, the seasonal P runoff dropped only by 8.9% when fertilization decreased by 20%; rice yields decreased with declining fertilization. We also found that inoculation increased rice yields and decreased P runoff at each fertilizer level and these effects were lower under higher fertilization. Conclusively, while rice yields were guaranteed arbuscular mycorrhizal inoculation and fertilizer management would play a key role in reducing P runoff from paddy fields.     

跨区域生态合作利益冲突的动态演化博弈分析

跨区域的生态合作是破解我国生态环境保护困境的途径之一,参与博弈各方的利益冲突情况是决定生态合作能否顺利开展的关键。采用非对称动态演化博弈模型对博弈过程中各方的利益冲突进行分析,结果表明:演化博弈的最终结局只与保护实施方的决策有关;政府干预可以显著改善生态合作的博弈结果;政府对跨区域生态合作结局的调整主要通过两条途径,其一是影响博弈双方的初始状态,其二是影响博弈双方的策略调整速度;政府干预并非总是带来好的生态保护结局。最后,在博弈均衡的基础上为我国跨区域生态合作提供了政策建议。     

低浓度苯系物在新疆干旱区土壤中的吸附行为研究

采集新疆干旱区石化废水库附近区域土壤,以苯、甲苯、乙苯、二甲苯(间、对二甲苯)等典型苯系物为研究对象,系统研究低浓度苯系物在干旱区土壤上的吸附行为,分析土壤有机质含量,溶液p H、溶液含盐量、温度对苯系物吸附的影响。结果显示土壤对低浓度苯系物的吸附16 h达到平衡;吸附等温线经拟合后符合Henry直线型吸附模型;土壤对苯系物的吸附量随着土壤有机质含量的增加而增加,土壤有机质含量与吸附量呈显著正相关(P0.01,R2≥0.919);溶液p H值对吸附过程无明显作用;随着溶液含盐量增大,土壤对苯系物的吸附量表现为先减小,再稳定;温度升高会抑制土壤对苯系物的吸附作用。     

土壤和沉积物中多氯萘的GC-MS/MS测定法

建立了同位素稀释GC-MS/MS法测定土壤和沉积物中多氯萘的分析方法。样品加入同位素内标,经ASE提取后,使用多层硅胶柱和氧化铝柱净化,再添加进样内标,采用三重四极杆串联质谱测定。方法检出限为0.26~1.6 ng/kg,回收率为55.6%~104.5%,采集电子垃圾场的土壤和沉积物实际样品进行验证性检测,结果显示,方法准确可靠,能够适用土壤和沉积物两种复杂基质样品的多氯萘检测。     

不同有机废水厌氧产酸过程的研究

主要研究了不同类废弃有机物厌氧产酸过程中产生的挥发性脂肪酸的产量和组成比例。研究发现,废糖蜜溶液、蛋白废液和淀粉废液在达到最高产酸量时,超过50%的VFAs是乙酸,其次是丙酸,还含有少量的丁酸和戊酸。废甘油溶液在达到最高产酸量时,产生的VFAs的主要成分是丙酸。4种有机废液中,相同初始COD浓度条件下,淀粉废液产生的VFAs产量最多,初始COD为5000mg/L时最高产量为2.321g/L,其次是废甘油溶液,最高产量是2.244g/L。     

连续流动法测定沉积物中的酸挥发性硫化物

优化沉积物中酸挥发性硫化物(Acid Volatile Sulfide,AVS)的提取方法并采用连续流动分析法检测提取液中的硫化物.研究了吸收液的种类、氮气流量与吹气的时间和反应温度对AVS提取效果的影响以优化提取方法.结果表明,与传统的氢氧化钠或硫酸镉-氢氧化钠吸收液相比,以氯化锌-羧甲基纤维素钠溶液为吸收液吸附效率好,稳定性高且无毒.用连续流动分析法检测提取液中的AVS快速、准确、稳定性好.     

裂隙对雾龙洞岩溶发育及地下径流的影响分析

尝试利用裂隙测量结果探究区域岩溶发育规律。采用统计窗口法对湖北鄂西地区雾龙洞岩溶流域的碳酸盐岩地层进行了大量的裂隙测量,分析了流域内裂隙发育的情况,研究了裂隙的几何参数——倾向、倾角、隙宽、线密度、面裂隙率等在不同层位、不同裂隙分组内的变化情况;结合构造、岩溶洼地发育方向、洞穴野外探测结果,综合分析了裂隙发育对本区岩溶发育的影响;运用渗透张量理论对岩溶流域裂隙的各向异性和非均质性进行了研究,并分析了雾龙洞岩溶流域地下水的主要渗流方向形成的原因,对查明雾龙洞岩溶流域岩溶发育规律以及地下水的运移、赋存规律具有一定的指导作用。     

某农药厂废弃场地土壤中甲拌磷垂向分布特征

为了解废弃农药厂土壤中甲拌磷的垂向分布特征,在前期表层土壤筛查的基础上,进一步在原甲拌磷生产车间开展了钻孔取样工作,布置了3个钻孔,钻孔深度43.0、41.0和45.0m,根据土壤颜色、岩性、电导率和pH的变化,共采集土壤样品39个,利用高效液相色谱仪对土壤中的甲拌磷进行了定量分析,同时测试了总有机碳、阳离子交换量、土壤粘粒含量、土壤含水率和温度等土壤的理化性质参数。测试结果显示,甲拌磷主要富集在表层土壤中,随着深度的增加,甲拌磷含量逐渐降低。根据相关性分析,土壤中甲拌磷含量和总有机碳含量有着显著的相关性,R分别为0.767、0.893和0.917,这表明土壤总有机碳含量对甲拌磷垂向分布有着非常重要的影响。