“最小存活种群”和“种群生存力分析”理论在生物多样性评价中的应用——以黔北20万吨/年竹浆林一体化工程中原料林基地建设工程为例

概述了“最小存活种群”和“种群生存力分析”概念、产生过程、研究内容及在生物多样性保护中的应用步骤,并运用该理论,以敏感种豹为关键种,分析了黔北新建20万吨/年竹浆林一体化工程中原料林基地建设工程对拟建项目区生物多样性的影响。分析结果表明,如原料林基地远离豹的栖息地,则栖息地面积尚可满足对豹短期保护（50代）的要求。因此,原料林基地的建设对绝大多数野生动物的影响不大,项目区的生物多样性是可以维持的。     

校园人工湿地科教基地建设及研究

2006年课题组在校园内组建了一套复合人工湿地实验系统,用于处理学生宿舍的部分生活污水,开展人工湿地净化水质的研究。经过3a的追踪分析测试,使学生掌握了人工湿地的工艺设计及净化机理,取得了较好的研究成果和教学效果,为学校搭建了一个科教平台,促进了教学与科研的同步发展。     

Polyphenylene sulfide based anion exchange fiber: Synthesis, characterization and adsorption of Cr(VI)

A fibrous strong base anion exchanger (QAPPS) was prepared for the first time via chloromethylation and quaternary amination reaction of polyphenylene sulfide fiber (PPS), and its physical-chemical structure and adsorption behavior for Cr(VI) were characterized by FT-IR, Energy Dispersive Spectrometry, TG-DTG, elemental analysis and batch adsorptive technique, respectively. The novel fibrous adsorbent could effectively adsorb Cr(VI) over the pH range 1-12, the maximum adsorption capacity was 166.39 mg/g at pH 3.5, and the adsorption behavior could be described well by Langmuir isotherm equation model. The adsorption kinetics was studied using pseudo first-order and pseudo second-order models, and the t_1/2 and equilibrium adsorption time were 5 and 20 min respectively when initial Cr(VI) concentration was 100 mg/L. The saturated fibers could be regenerated rapidly by a mixed solution of 0.5 mol/L NaOH and 0.5 mol/L NaCl, and the adsorption capacity was well maintained after six adsorption-desorption cycles.     

水泵系统噪声与振动控制

从水泵系统振动噪声传播途径控制的角度,着重分析了水泵机座二次隔振系统、水泵接管隔振、隔振系统位移限制、管道支架减振、管道穿墙隔振、管道阻尼隔声包扎等水泵系统振动固体传递途径的控制,消除与建筑结构之间的刚性连接。分析了振动噪声空气传播的阻隔与吸收。     

基于大比例尺地形图的抗震规划工作底图缩编研究

工作底图的编制是开展抗震规划的基础工作之一,好的工作底图不仅能突出抗震规划专题信息,更有利于规划成果的应用。本文以1∶5 000地形图缩编成1∶5万抗震规划工作底图为例,分析了规划底图缩编过程中存在的问题,探索了基于AutoCAD、南方Cass软件以及Arcgis的缩编方法,从而有效提高抗震规划的工作效率。     

通信技术在近海环境监测中的应用

本文针对海洋环境监测覆盖面广、站位分散、数据间断和频繁少量的特点以及海洋环境监测自动化、实时化和连续化的发展趋势,提出一种基于水上移动通信和水声通信技术的海底观测链方式,并以海床基监测数据实时传输系统为例,对系统组成、技术特点、技术原理和应用分别阐述,旨在推广通信技术在海洋环境监测领域中的应用。     

种植基地有机磷农药污染土壤的微生物修复

针对我国土壤普遍受到有机磷农药污染的现状,从有机磷农药污染土壤中筛选出降解作用大、生理性状稳定的5种抗性菌株,根据细菌形态观察、生理生化指标检测及16SrDNA基因序列分析,初步确定其生物学分类地位。通过富集培养及固定化技术,分别研究其对甲拌磷、对硫磷、甲基异柳磷和氯氰菊酯等农药的生物降解作用及其影响因素。初步探讨了微生物对甲拌磷农药的降解机理。上述研究结果表明：利用微生物降解农药是一种较有开发前景的有效方法。     

Effects of two forest types on the dynamics of four base cations along with rainfall partitioning in middle subtropical forests北大核心CSCD

盐基离子随穿透雨和树干茎流的迁移成为森林元素输入的重要组成部分.在迁移过程中,冠层淋溶、树干冲刷等改变了盐基离子含量,而不同林型的林冠特征、树皮性质等存在差异,因此盐基离子含量在不同林型中可能存在差异对米槠次生林和杉木人工林穿透雨、树干茎流进行为期4年的监测,对比研究4种盐基离子(K+、Ca2+、Na+、Mg2+)浓度和输入量的动态特征.结果显示:(1)米槠次生林树干茎流Ca2+、Mg2+浓度显著低于杉木人工林而K+浓度显著高于杉木人工林;穿透雨除Na+浓度外均为米槠次生林显著高于杉木人工林.穿透雨和树干茎流Na+浓度林型差异不显著.(2)两种林型盐基离子季节动态变化基本一致,在雨季旱季各有一个峰值,雨季浓度普遍低于旱季.米槠次生林盐基离子浓度稳定性普遍高于杉木人工林.(3)分析盐基离子浓度与降雨强度的关系发现:Ca2+、K+、Mg2+浓度随雨量级的增加而降低,Na+浓度随雨量级的增加而增加.(4)观测期间米槠次生林穿透雨累计输入Ca2+、K+、Mg2+和Na+总量分别为47.97、35.17、7.15和12.94 kg/hm2,树干茎流累计输入Ca2+、K+、Mg2+和Na+总量分别为11.38、6.21、1.54和3.00 kg/hm2;杉木人工林穿透雨累计输入Ca2+、K+、Mg2+和Na+总量分别为47.24、26.63、6.43和11.55 kg/hm2,树干茎流累计输入Ca2+、K+、Mg2+和Na+总量分别为4.11、1.20、0.50和0.83 kg/hm2.米槠次生林的林内雨盐基离子输入量大于杉木人工林.总体而言,米槠次生林比杉木人工林有更高的养分输入,能更好地维持生态系统养分的供应;上述结果有助于进一步认识森林物质随水文过程的流动,可为人工林经营管理提供一定科学基础数据.(图6表1参36)     

Spatiotemporal Evaluation of Simulated Evapotranspiration and Streamflow over Texas Using the WRF‐Hydro‐RAPID Modeling Framework

This study assesses a large‐scale hydrologic modeling framework (WRF‐Hydro‐RAPID) in terms of its high‐resolution simulation of evapotranspiration (ET) and streamflow over Texas (drainage area: 464,135 km²). The reference observations used include eight‐day ET data from MODIS and FLUXNET, and daily river discharge data from 271 U.S. Geological Survey gauges located across a climate gradient. A recursive digital filter is applied to decompose the river discharge into surface runoff and base flow for comparison with the model counterparts. While the routing component of the model is pre‐calibrated, the land component is uncalibrated. Results show the model performance for ET and runoff is aridity‐dependent. ET is better predicted in a wet year than in a dry year. Streamflow is better predicted in wet regions with the highest efficiency ~0.7. In comparison, streamflow is most poorly predicted in dry regions with a large positive bias. Modeled ET bias is more strongly correlated with the base flow bias than surface runoff bias. These results complement previous evaluations by incorporating more spatial details. They also help identify potential processes for future model improvements. Indeed, improving the dry region streamflow simulation would require synergistic enhancements of ET, soil moisture and groundwater parameterizations in the current model configuration. Our assessments are important preliminary steps towards accurate large‐scale hydrologic forecasts.     

Improvement in HSPF's Low‐Flow Predictions by Implementation of a Power Law Groundwater Storage‐Discharge Relationship

We have enhanced the ability of a widely used watershed model, Hydrologic Simulation Program — FORTRAN (HSPF), to predict low flows by reconfiguring the algorithm that simulates groundwater discharge. During dry weather periods, flow in most streams consists primarily of base flow, that is, groundwater discharged from underlying aquifers. In this study, HSPF's groundwater storage‐discharge relationship is changed from a linear to a more general nonlinear relationship which takes the form of a power law. The nonlinear algorithm is capable of simulating streamflow recession curves that have been found in some studies to better match observed dry weather hydrographs. The altered version of HSPF is implemented in the Chesapeake Bay Program's Phase 5 Model, an HSPF‐based model that simulates nutrient and sediment loads to the Chesapeake Bay, and is tested in the upper Potomac River basin, a 29,950 km² drainage area that is part of the Bay watershed. The nonlinear relationship improved median Nash‐Sutcliffe efficiencies for log daily flows at the model's 45 calibration points. Mean absolute percent error on low‐flow days dropped in five major Potomac River tributaries by up to 12 percentage points, and in the Potomac River itself by four percentage points, where low‐flow days were defined as days when observed flows were in the lowest 5th percentile range. Percent bias on low‐flow days improved by eight percentage points in the Potomac River, from ?11 to ?3%.