模拟状态下高尔夫球场果岭区域土壤氮磷浸出物对铁岗水库水质影响研究

通过采集高尔夫球场即将淹没的果岭土壤进行实验室条件下的模拟库基样品试验,对水库扩容后蓄水初期水质的变化情况进行了研究.结果表明:库水所含主要成分pH、高锰酸钾盐指数、总氮、总磷、氨氮和硝酸盐氮分别为7.4(mg/L)、30.8(mg/L)、1.16(mg/L)、1.189(mg/L)、0.21(mg/L)和0.11(mg/L);果岭20 cm土层库基土样pH、有机质、硝酸盐氮、氨态氮和有效磷分别为6.41(mg/kg)、10.29(mg/kg)、25.48(mg/kg)、25.76(mg/kg)和140.77(mg/kg).现有库基成分会改变库水高锰酸钾盐指标的升高.库水本身的总磷和总氮含量就严重超标.果岭库基本身的磷氮含量也很高.浸泡后果岭库基土样对降低浸出物总磷的严重超标起到了对冲的作用,致使总磷含量大为降低.     

Floodplain Trapping and Cycling Compared to Streambank Erosion of Sediment and Nutrients in an Agricultural Watershed

Floodplains and streambanks can positively and negatively influence downstream water quality through interacting geomorphic and biogeochemical processes. Few studies have measured those processes in agricultural watersheds. We measured inputs (floodplain sedimentation and dissolved inorganic loading), cycling (floodplain soil nitrogen [N] and phosphorus [P] mineralization), and losses (bank erosion) of sediment, N, and P longitudinally in stream reaches of Smith Creek, an agricultural watershed in the Valley and Ridge physiographic province. All study reaches were net depositional (floodplain deposition > bank erosion), had high N and P sedimentation and loading rates to the floodplain, high soil concentrations of N and P, and high rates of floodplain soil N and P mineralization. High sediment, N, and P inputs to floodplains are attributed to agricultural activity in the region. Rates of P mineralization were much greater than those measured in other studies of nontidal floodplains that used the same method. Floodplain connectivity and sediment deposition decreased longitudinally, contrary to patterns in most watersheds. The net trapping function of Smith Creek floodplains indicates a benefit to water quality. Further research is needed to determine if future decreases in floodplain deposition, continued bank erosion, and the potential for nitrate leaching from nutrient‐enriched floodplain soils could pose a long‐term source of sediment and nutrients to downstream rivers.     

Microbial bioavailability of dissolved organic nitrogen (DON) in the sediments of Lake Shankou, Northeastern China

Dissolved organic nitrogen(DON)extracted from Lake Shankou sediments using KCl was isolated into hydrophobic and hydrophilic fractions.The bioavailabilities of the hydrophobic and hydrophilic fractions to three types of bacterial communities collected from sediments,activated sludge and compost products were examined.The DON recoveries obtained by DAX-8 and cation exchange resins treatment were 96.17% ± 1.58% and 98.14% ±0% for the samples obtained from N4 and N14 stations,respectively.After 25 days of incubation at 25°C,most DON(59% to 96%)was degraded.Hydrophilic DON exhibited a higher reduction rate than hydrophobic DON during the growth phase.Untreated wastewater from Changshuihe town was the main degradable DON source to station N4,and 93% of hydrophilic DON and 80% of hydrophobic DON were degraded.Station N14 received a large amount of refractory DON from forest soils and exhibited DON degradation rates of 82% and 71% for the hydrophilic and hydrophobic fractions,respectively.Amino acid contents and fluorescence intensities were also analyzed.Approximately 27% to 74% of amino acids were taken up by day 5,and their concentration gradually increased in the following days due to the decomposition of dissolved proteins.Parallel factor analysis resulted in identification of tryptophan-like proteins,tyrosine-like proteins and FA-like substances.During the growth phase,40%–51% of the tryptophan-like proteins were taken up by bacteria,and the accumulation of tyrosine-like proteins was attributed to the release of biotic substances.The concentration of the FA-like substances decreased due to microbial decomposition.     

成都市中心城区春季大气颗粒物PM_(2.5)的污染特征研究

于2012年5月11日至5月15日同时对成都中心城区及其大气环境监测对照点都江堰灵岩寺大气PM2.5进行采集,并分析其中的化学组分。研究结果表明:成都市中心城区PM2.5的总体质量浓度大于灵岩寺,且各化学组分的质量浓度也均大于灵岩寺。两站点PM2.5中OC/EC均大于2,有2次有机碳的存在;中心城区WSOC和TN日均浓度大于灵岩寺,同时发现中心城区TN日变化趋势与灵岩寺一致,WSOC变化不明显;水溶性二次离子(SO2-4、NO-3和NH+4)浓度相对较高,中心城区SO2-4/NO-3值比灵岩寺小,说明成都市机动车尾气是主要排放源。     

氚在黏土矿物等多孔介质中的滞留机制

通过电感耦合等离子体光谱(ICP)、热重(TG)等分析方法对黏土矿物的结构成分、加热特性等进行了检测;通过蒸馏冷凝等实验,实现了对吸附后黏土矿物的吸附水、层间水、结构水的分离,检测了氚在黏土矿物结构内外各类型水中的分布;通过红外吸收光谱(IR)等分析方法对氚在黏土矿物结构中的吸附位置及形态进行了检测研究;通过同位素效应...     

A^2O脱氮除磷工艺及其变型工艺比较分析

传统的A2O工艺及其变型工艺,由于工艺流程简单、控制方便、运行费用低等特点,目前仍广泛应用于污水处理的脱氮除磷。对传统的A2O工艺及其变型工艺的原理和特点进行了系统归纳和比较分析。     

清洁生产审核在氮肥企业的应用

某氮肥企业通过开展清洁生产审核,确定以节水、减少废水及水污染物排放量为目标,将企业供排水系统作为本轮清洁生产审核的重点,针对审核重点制定了定量的清洁生产审核目标,通过清洁生产方案的实施实现了环境效益、社会效益与经济效益的统一,为氮肥企业实施清洁生产提供了良好的借鉴。     

寿山石的成矿地质条件和矿物组成

长期研究表明,寿山石的成矿地质条件主要受地层、构造、火山机构和火山成矿等综合作用控制。寿山石的矿物成分主要为地开石、高岭石和叶蜡石。因寿山石的成矿地质条件、矿物组成和产出部位的不同,形成色彩绚丽、命名异样、品种繁多、分类殊异。但通常以其成因、产状和历史传统分为田坑石、山坑石和水坑石三类。为便于识别、研究和讨论,将寿山石的主要品种及其特征一并简介。     

四丰山水库富营养化状况

通过对四丰山水库2006至2010年监测数据的统计,分析水库水质富营养化状况,指出水质富营养化的危害,并提出避免水质恶化的建议.     

鸟粪石法回收养猪废水中磷时pH对沉淀物组分的影响

采用鸟粪石沉淀法对养猪废水中的磷进行回收,应用红外光谱和X射线衍射法,并结合物料衡算研究pH变化对沉淀物组分的影响.结果表明,当pH由8.0升至9.0时,磷去除率从85%增加到94%;pH在9.0～11.0范围,磷去除率稳定在94%左右;当pH升高至12.0,磷去除率急剧下降至70％.沉淀物组分为鸟粪石(MgNH₄PO₄·6H₂O)、 钾型鸟粪石(MgKPO₄·6H₂O)、 Ca₃(PO₄)₂·xH₂O和Mg(OH)₂,不含有硫酸盐和碳酸盐.当pH<9.0,沉淀物组分主要为鸟粪石;pH在9.0～10.0范围时,鸟粪石含量降低,钾型鸟粪石、 Ca₃(PO₄)₂·xH₂O含量呈逐渐增加趋势;pH由10.0升至12.0时,鸟粪石含量急剧下降,Ca₃(PO₄)₂·xH₂O和Mg(OH)₂含量快速增加,而钾型鸟粪石快速增加并在pH 11.0达到最大后急剧下降.因此,回收养猪废水中的磷时要获得纯度高的鸟粪石产品,pH值应控制在8.0～9.0.