天津地区六六六的归宿和跨界面迁移

以天津市为研究区域，以80年代有机氯农药禁用前为时限，利用稳态非平衡逸度模型估算了稳态条件下六六六的四种异构体在环境各相中的迁移和分布。模型估算结果用同期各主要介质的实测浓度加以验证。结果表明，农业施用和农药厂排放是该地区环境中六六六的主要来源，最大的汇则是土壤和水体沉积物，该地区最主要的界面迁移过程包括大气向土壤的沉降、水体向沉积物的沉降以及气相平流输出等，发生在土壤和沉积物中的降解则是六六六消失的最主要途径。     

不同农业措施对稻田甲烷排放通量的影响

经过三年的田间试验发现,稻田甲烷排放通量随着农业措施的不同而大幅度地变化。在1990年至1992年的三个晚稻生长季节里,试验地块的甲烷排放通量分别为10.83、25.18及19.85mg/m~2·h。半旱式栽培使甲烷排放量减少了约1/3;施用硫酸铵、烤田、间歇灌溉亦可显著地降低甲烷排放通量。高有机肥与长期淹水是造成稻田甲烷排放量大的主要原因。控制稻田甲烷排放的关键在于调节灌溉水。只要采用合适的灌溉制度。有机肥用量的增加不一定引起甲烷排放量的增大。     

Analytical evaluation of mesoscale fluxes and pressure field

Terrain in natural areas is never homogeneous: there may be a variety of vegetation types and patches of vegetated and unvegetated areas which can modify the mesoscale atmospheric flow. Moreover, horizontal thermal inhomogeneities in the planetary boundary layer are a well known source of mesoscale circulation systems such as land and sea breezes, mountain-valley winds, and urban heat island circulations. Since those phenomena are not resolved in regional scale numerical models, therefore an analytic procedure able to evaluate the relative importance of mesoscale and turbulent heat fluxes associated with surface thermal heterogeneities is of crucial importance in the optic of developing a parameterization of mesoscale effects generated by these heterogeneities for use in larger scale models. In the present paper we analyze how small a horizontal variation in surface heating can be and still produce a significant mesoscale circulation, how the heat and momentum fluxes associated to mesoscale flows can penetrate deeply into the mid-troposphere, and how they modify tropospheric relevant climate parameters, such as the atmospheric static stability. In addition, we evaluate the terms of the pressure gradient force, nonlinear and linear, non-hydrostatic and hydrostatic, as function of time and space scales of the mesoscale flow. The present paper is mainly a review of analytical results, the numerical comparison and verification using RAMS is in progress.     

Quality control and flux gap filling strategy for Bowen ratio method: revisiting the Priestley–Taylor evaporation model

Micrometeorological measurements were made over an irrigated rice paddy during the Huaihe River Basin Experiment (HUBEX) in 1999. This study addresses the quality control and gap filling strategy for the heat fluxes with the Bowen ratio energy balance (BREB) method. It also endeavors to benefit future studies through comparing five methodologies to estimate the net water exchange. First, a three-step quality control strategy is constructed. Its first two steps guarantee the correct flux directions and reject suspicious data, respectively. The third step forbids supersaturation by considering the Bowen ratio ranges for different flux combinations (termed as “scenarios”). The quality-controlled latent heat (LE) and sensible heat (H) fluxes fall in three scenarios, namely I (LE > 0, H > 0), II (LE > 0, H < 0), and IV (LE < 0, H < 0). Second, the Priestley–Taylor evaporation model (PTEM) is applied to fill the gaps of LE, while the energy balance relationship is used to gap-fill H, namely H = R _N − G − LE (R _N : net radiation; G: soil heat flux). Central to the success of this strategy is the idea to calibrate the Priestley–Taylor parameter (α) in a scenario-specific manner. On average, α values are calibrated as 1.20 and 1.35 for scenario I and II, respectively. For scenario IV, most α values lie in a narrow range, namely from 0.9 to 1.0. Then, α is calibrated as 0.97 to extend the applicability of the PTEM to condensation (negative LE). The scenario-specific treatment explicitly explains the diurnal variation of α derived without distinguishing the scenarios. Third, five methodologies are compared in the calculation of net water exchange, including PTEM-gap-filled BREB method (M1), energy-balance-based eddy covariance method (M2), and three simplified models to estimate LE, respectively as R _N − H, R _N − G, and R _N . A major finding is that G and H have a similar effect of about 3% in the net water exchange. Thus, if either is neglected, the net evaporation should be slightly lowered to avoid overestimate, by 3% as a rule of thumb from this work.     

不同耕作制度对南方稻田甲烷排放的影响

以南方稻田温室气体甲烷排放为研究对象,选取冬季休闲和种植绿肥作物紫云英(AstragalussinicusL.)两种主要模式,在早稻(OryzasativaL.)移栽之前进行旋耕和翻耕两种处理,以全年休闲为空白对照,利用静态箱法测定甲烷排放通量。结果表明,甲烷排放在水稻抽穗期达到极大值,至收获甲烷排放呈减少趋势,以无稻全年休闲区甲烷排放通量最低,在抽穗至收获阶段平均排放速率为3.43mg·m-2·h-1,冬闲及冬季种植紫云英处理分别比无稻休闲区排放通量高114.3%和420.3%;甲烷浓度具有强烈的空间异质性,地表以上50cm空间内,早稻抽穗至成熟阶段甲烷浓度是大气甲烷浓度的35.2倍;稻田甲烷高浓度低排放速率以及低浓度高排放速率现象表明,甲烷排放速率与其浓度之间具有非一致性。     

鼎湖山针阔叶混交林地表CH4通量

用静态箱-气相色谱法对鼎湖山针阔叶混交林的地表CH4通量进行了为期一年的原位观测和研究.结果表明,该林型土壤总体为大气CH4的吸收汇,通量年变化范围60～-120 μg·m-2·h-1,在雨季向旱季过渡的9、10月份,土壤对CH4的吸收较为强烈,而在冬季的1月份,吸收通量最小;凋落物层对该林型地表CH4的吸收没有明显的阻隔作用;多元回归分析发现CH4通量与地下5 cm温度显著相关,尤其是在土壤湿度变化不大的旱季,土壤表层温度为影响CH4通量的主导因子.     

论水污染物排放统计指标体系

水污染物排放统计指标体系包括水污染物排放统计指标以及排放管理指标,统计对象主要是规模以上点源。实施统计的污染源的规模应当是全国统一的。统计指标区分为指标、主要参数和辅助参数,既便于理解也便于管理;将排放指标细化为污染源排放量、入河排放量和通量使得排放概念更加清晰,有利于水环境管理。对入河排放量和污染源排放量的比较,可以确定纳入统计范围的污染源的代表性,对通量和入河排放量的比较可以推断非点源污染物排放状况。以流域为单元的,以通量、入河排放量和污染源排放量为主要概念的排放统计管理方式,有助于提高流域水污染防治的确定性和一致性。     

A Simple Field Method to Determine Mercury Volatilization from Soils (3 pp)

Background Estimations of gaseous mercury volatilization from soils are often complex, stationary and expensive. Our objective was to develop a mobile and more simple, easy to handle and more cost-effective field method allowing rapid estimates of potential Hg emissions from soils. Methods. The study site is located in Germany, about 100 kilometers south-westerly of Berlin and influenced by the river Elbe and its tributary Saale river. The site is representative for a lot of other floodplain locations at the river Elbe and highly polluted with Hg and other heavy metals. For our study we developed a system consisting of a glass chamber gas, two gold traps, a battery operated pump and a gas meter. Adsorbed total gaseous mercury (TGM) in the gold traps was determined by use of atomic absorption spectrometry (AAS). Results and Discussion. In contrast to the common used flux chambers we designed a chamber without inlet and named it gas suck up chamber (GSC). TGM fluxes determined with the GSC showed a very close linear correlation (r = 0.993) between the TGM content in the gold traps and the corresponding pumped gas volume. The TGM adsorbed, increased proportional with increasing gas volume indicating homogenous concentrations of gaseous mercury in the soil air sucked. In contrast to the commonly used dynamic flux chamber with the aim of precisely measuring actual fluxes of Hg from a defined soil area, we focused on developing of a measurement system which will allow rapid estimates of potential Hg emissions of a site. Earlier research at the study site indicated a high potential for releasing volatile Hg from the soil to the atmosphere. Indeed, due to the high Hg content of the soil significant amounts of TGM could be detected and no shortage was reached. Conclusion. Our initial measurements are still too few in number neither to generalize the achieved results nor discuss controlling factors and processes. However, we are pleased to communicate that the developed GSC is well suited to become an effective sampling set up to rapidly estimate the magnitude of Hg volatilization from soils. Outlook. Further measurements at other polluted locations are necessary to verify the GSC method. In addition the use of a mercury analyzer instead of gold traps is planned for faster risk assessments.     

高效藻类塘氮磷去除机理的研究进展

首先介绍了高效藻类塘的发展历史和特点,其次简述了高效藻类塘的生物特性和物理化学变化规律,并重点论述了高效藻类塘的氮磷去除机理及其影响因素,最后对高效藻类塘在控制非点源污染中的应用前景进行展望.