水稻不同生育期根际与非根际土壤胞外酶对施氮的响应

与稻田土壤碳氮循环(矿化、转化等)密切相关的酶活性可以反映微生物的生长和代谢过程.为明确水稻不同生育期根际与非根际土壤胞外酶对施氮的响应,采用根际袋法区分水稻根际和非根际土壤,利用96微孔酶标板荧光分析法,测定其碳氮过程关键酶β-1,4-葡萄糖苷酶(BG)和β-1,4-N-乙酰氨基葡萄糖苷酶(NAG)活性,探讨根际效应、施氮和生育期对土壤酶活的影响及其调控机制.结果表明,施氮使拔节期土壤BG酶活性相对于不施氮处理降低了7.4~13.5 nmol·(g·h)~(-1),而使成熟期BG酶活性增大了7.0~31.4 nmol·(g·h)~(-1),同时根际与非根际土壤中BG酶活性也随水稻的生育期而发生相应的变化.与不施氮处理相比,施氮使水稻成熟期非根际土壤NAG酶活性增加了1.1倍,根际土壤降低了0.3倍.施氮和生育期显著影响土壤BG酶活性,而水稻生育期、施氮和根际效应及其交互作用均对NAG酶活性有极显著影响.RDA分析表明土壤微生物生物量碳(MBC)和可溶性有机碳(DOC)含量主要影响水稻根际土壤胞外酶活性;而非根际土壤中酶活性的变化主要受微生物生物量氮(MBN)和铵态氮(NH_4~+-N)的影响.土壤酶活性与多种因素存在复杂关系,需要综合考虑植物生理特征、土壤酶活性和土壤特征,分析N添加对微生物群落组成的影响.     

不同浓度锌离子污染土的工程力学性能试验研究

通过直剪试验、压缩试验和三轴试验对人工制备最优含水率下不同浓度锌离子污染土的工程力学性能进行测试,研究了不同锌离子浓度污染土的抗剪强度和压缩特性。结果表明:随着锌离子浓度的增加,污染土的内摩擦角和压缩系数增加,内聚力和压缩模量下降,而污染土的孔隙比随着锌离子浓度的增加先减小后增大;在不同垂直压力下,随着压力的增加,污染土的压缩系数整体先减小后增大,压缩模量先增大后减小。     

简讯

原油泄漏对生态系统服务功能的影响面对生态灾难时,决策学工具可以用来评估处置选项、并推论其对于生态系统服务(ES)的危险.影响图(DIs)是明确显示针对某一问题所作决定及其希望或不希望结果的概率网络图.为检验IDs对于泄露漏处置的概率性风险管理,制作1个ID来展示DWH事件中泄漏事件之间的潜在互动、费用与泄漏原没对ES的冲击之间的取舍及处置决定.定量认识并没有正式包含在内,但是检验了1个这样的ID平台.概率分配给ID中的条件关系,而不同处置行动对于     

污灌渠中有机氯农药对沿渠土壤的影响

为了研究污水灌渠侧渗对土壤的影响,采用气相色谱-电子捕获检测器(GC-ECD)方法对太原市小店污灌区9个剖面土和2个灌溉污水样进行有机氯化合物(OCPs)分析.结果表明退水渠中有机氯农药主要由六六六(HCHs)组成,滴滴涕(DDTs)及其它有机氯农药含量较低或未检出,在8个离渠较近剖面的地表土中ΣOCPs和HCHs含量一定程度上符合随垂直于渠的直线距离增加而逐步降低的趋势,表明污水渠侧渗对土壤存在着一定影响.8个剖面土壤中的HCHs含量随着深度的增加而降低,在水平方向上,同一深度土壤中的HCHs含量也沿远离渠的直线方向逐步递减.研究区土壤中HCHs含量与TOC之间存在较为显著的正相关性,而与pH之间不存在相关性.     

四氯乙烯和铬复合污染地下水的有机凹凸棒土吸附性能研究

研究了有机凹凸棒土对人工模拟地下水中PCE和Cr6+两者复合污染的吸附行为。分别探讨了振荡吸附时间、凹土投加量、pH值对添加了重金属Cr6+前后凹土吸附PCE效果的影响;通过凹土对PCE的吸附等温线,讨论其吸附的内在机理。结果表明:有机凹土对TCE的吸附10min内达到平衡,吸附率达63.5%,而铬离子存在时吸附率下降至38.2%;当凹土加入量为15.38g/L时,吸附率可达62.8%,铬离子存在时,达到饱和所需的凹土量增加。PCE单组分在有机凹土上的吸附符合langmuir等温式。PCE和Cr(Ⅵ)经复合之后,PCE的吸附效果有所下降,吸附过程采用langmuir及freundlich等温式拟合均不够准确。     

SPE-UFLC-MS/MS法测定制药废水中四环素类抗生素

文章建立了利用固相萃取-超快速液相色谱-串联质谱(SPE-UFLC-MS/MS)测定制药废水中四环素类抗生素(土霉素、四环素和金霉素)残留的方法。水样经(30%硫酸锌+20%亚铁氰化钾)溶液作为沉淀剂沉淀蛋白质后,上清液采用Oasis HLB固相萃取柱富集和净化,以(0.1%甲酸溶液+乙腈)为流动相进行梯度洗脱,经Agilent ZORBAX SB C18柱分离后,在串联质谱ES(I+)模式下进行MRM检测。该方法四环素类抗生素检出限(S/N=3时)0.02μg/L,3种目标物在0.010¹.0 mg/L范围内线性关系良好,线性相关系数在0.998 21.0 mg/L范围内线性关系良好,线性相关系数在0.998 2⁰.999 8之间。在0.20、0.40和0.60μg/L添加水平,各组分的回收率在80.8%0.999 8之间。在0.20、0.40和0.60μg/L添加水平,各组分的回收率在80.8%⁹7.2%之间,相对标准偏差在5.31%97.2%之间,相对标准偏差在5.31%⁹.92%之间。该方法可满足制药废水中四环素类抗生素残留检测的要求。     

2,2′-二硝基联苄生产废水的处理研究

对十六烷基三甲基溴化铵改性凹凸棒土、凹凸棒土负载TiO2采用XRD、FTIR以及TG等手段进行了分析和表征,对比了改性凹凸棒土、活性炭、大孔树脂等不同吸附剂和凹凸棒土负载TiO2对二硝基联苄生产废水的处理效果。结果表明:十六烷基三甲基溴化铵改性凹凸棒土的废水中污染物的去除率比凹凸棒土提高了2.5倍;凹凸棒土负载TiO2在波长λ=254 nm下光照0.5 h,对废水中污染物的去除率是凹凸棒土的2.0倍;投加量为3%活性炭在pH为2.0⁵.0时,对该类废水中污染物的去除率可达80%以上。     

污水土地处理系统重塑土渗透性及混合比的确定方法

污水土地处理系统的渗透性是能否实现污水处理设计要求的关键。本文采用地下水数值模拟方法刻画了污水土地处理系统复杂的结构和边界条件,准确地得到了能够满足污水处理设计要求的污水土地处理系统的渗透系数,并通过不同砂-土混合比例的重塑土渗透试验,研究了能够满足污水处理设计要求的重塑土的砂-土混合比,以为充分利用原场地黏土资源提供依据,也为类似研究和设计提供新的思路和方法。     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.     

Debromination of decabromodiphenyl ether by organo-montmorillonite-supported nanoscale zero-valent iron：Preparation, characterization and influence factors

An organo-montmorillonite-supported nanoscale zero-valent iron material(M-NZVI) was synthesized to degrade decabromodiphenyl ether(BDE-209). The results showed that nanoscale zero-valent iron had good dispersion on organo-montmorillonite and was present as a core-shell structure with a particle size range of nanoscale iron between 30–90 nm, characterized by XRD, SEM, TEM, XRF, ICP-AES, and XPS. The results of the degradation of BDE-209 by M-NZVI showed that the efficiency of M-NZVI in removing BDE-209 was much higher than that of NZVI. The efficiency of M-NZVI in removing BDE-209 decreased as the pH and the initial dissolved oxygen content of the reaction solution increased, but increased as the proportion of water in the reaction solution increased.