旱区经营人工植被对土壤干化过程的调控

人工植被在北方旱区具有重要的意义,但在干旱少雨的条件下开展建设,必须讲求水分平衡。基于此,作者通过考察长期的经营实践,从土壤水分角度讨论人工植被与环境之间的耦合匹配问题。阐述了普遍发生的人工植被作用下的土壤干化对植被自身的不利影响以及其可调控性,并进一步对调控途径和措施进行了分析。表明人为采取措施可以将土壤干化现象加以调节和控制,如局部带状或团块状种植、疏伐、轮作、休闲、灌溉等。在贯彻适地适种原则的基础上,还需选择耗水量少的抗旱节水植物和可维持土壤水库水平的密度或盖度,这是保证人工植被稳定持久值得重视的又一重要方面。预防土壤干化是首要的,需多途径相互结合进行调控。对土壤干化过程的调控实际上就是有效经营人工植被。需要结合经营目标评定人工植被的稳定性。     

Biogeochemical model (BGC-ES) and its basin-level application for evaluating ecosystem services under forest management practices

It is important for humans to live in harmony with ecosystems. Evaluation of ecosystem services (ES) may be helpful in achieving this objective. In Japan, forest ecosystems need to be re-evaluated to prevent their degradation due to lack of forest management.In order to evaluate the effects of forest management on forest ES, we developed a process-based biogeochemical model to estimate water, carbon, and nitrogen cycles in forest ecosystems (BGC-ES). This model consists of four submodels: biomass, water cycle, carbon-nitrogen (CN) cycles, and forest management. The biomass submodel can calculate growth of forest biomass under forest managements.Several parameters of the model were calibrated using data from observations of evapotranspiration flux and quality of stream flow in forests. The model results were compared with observations of runoff water from a dam catchment site and with carbon flux observations.Our model was coupled with a basin-level GIS database of forests. Evaluations under various forest management scenarios were carried out for forests in a basin contained in the Ise Bay basin (Chubu region, Japan), where plantations (artificial forests) seemed to have degraded from poor forest management.Comparing our simulation results with those of forests without management in the basin, we found that the amounts of absorbed carbon and runoff were larger in managed forests. In addition, the volume of harvested timber was larger and its quality (diameter) was better in managed forests. Changes of ES within the various scenarios were estimated for their economic value and were compared with the cost of forest management.     

临江灌区工程环境影响评价中盐分平衡的分析与计算

灌区盐分平衡状态的分析与计算是灌区工程环境影响评价工作中的重要内容之一。通过以临江灌区工程为例,详细分析和计算了该灌区建成前后的盐分平衡状况,为灌区生态与环境保护提供了科学依据。盐分平衡动态过程的分析应建立在灌区水量平衡的基础上,应获取灌区土壤、地表水、地下水、灌区水源水以及灌区排水中的盐分浓度,同时还应获取灌区建成前后化肥使用量变化、地表生物量的累积变化以及生物质中的盐分含量等相关参数。文中所提供的灌区盐分平衡分析与计算方法对丰富农林水利类工程的环境影响评价理论具有参考意义。     

Modelling above- and below-ground mass loss and N dynamics in wooden dowels (LIDET) placed across North and Central America biomes at the decadal time scale

This article focuses on modelling above and below-ground mass loss and nitrogen (N) dynamics based on the wooden dowels (Gonystylus bancanus [Miq.] Kurz) of the decadal Long-term Intersite Decomposition Experiment (LIDET) data. These dowels were placed at 27 locations across North and Central America, involving tropical, temperate and boreal forests, grasslands, wetlands and the tundra. The dowel, inserted vertically into the soil with one half remaining exposed to the air, revealed fast mass and N losses under warm to humid conditions, and slow losses under wet as well as cold to dry conditions. The model formulation, referred to as the Wood Decomposition Model, or WDM, related these losses to (i) mean annual precipitation, mean monthly January and July air temperatures, and (ii) mean annual actual evapotranspiration (AET) at each location. The resulting calibrations conformed well to the time-in-field averages for mass remaining by location: R² = 0.83 and 0.90 for the lower and upper parts, respectively. These values dropped, respectively, to 0.41 and 0.55 for the N concentrations, and to 0.28 and 0.43 for N remaining. These reductions likely refer to error propagation and to as yet unresolved variations in N transference into and out of the wood specific to each individual dowel location. Recalibrating the model parameters by ecosystem type reduced the R² values for actual versus best-fitted mass loss by about 0.15. Doing the same without location- or ecosystem-specific adjustments reduced the R² values further, by about 0.3.     

路边微环境PM2.5化学组分特征及来源解析

采集并分析了武汉市机动车尾气源PM_2.5样品,并于2019年10月18~27日采集了武汉市不同路边微环境（市区路边、环线路边、环境背景点）PM_2.5样品并分析其化学组分特征,利用化学质量平衡模型（CMB）解析评估了机动车尾气对城市不同路边微环境PM_2.5的贡献.结果表明,机动车尾气成分谱以OC和EC为主,汽油车OC质量分数约为柴油车的1.14倍,柴油车EC质量分数是汽油车的1.08倍.路边碳组分主要来源于机动车尾气,其中OC浓度在市区路边最高,EC浓度在环线路边最高;市区路边NO₃^-和NH₄⁺浓度较高,与二次转化有关;环线路边Fe、Si、Al质量浓度高于市区路边.CMB来源解析结果显示,机动车尾气源是环线路边、市区路边微环境的主要来源,分担率为35.20%和38.89%,是环境背景点的2倍左右.不同路边微环境污染源贡献差异明显,与环线路边相比,市区路边机动车尾气源与二次来源均相对较高,而扬尘源贡献低于环线路边.     

Flow analysis of major and trace elements in residues from large-scale sewage sludge incineration

Increase of sewage sludge (SS) has led to the construction of more incineration plants, exacerbating to the production of SS incineration residues. However, few studies have considered the mass balance of elements in large-scale SS incineration plants, affecting the residues treatment and utilization. In this study, flow analysis was conducted for major and trace elements in the SS, the fly ash (sewage sludge ash, SSA) and bottom ash from two large-scale SS incineration plants. The elemental characteristics were compared with those of coal fly ash (CFA), and air pollution control residues from municipal solid waste incineration (MSWIA), as well as related criteria. The results showed that the most abundant major element in SSA was Si, ranging from 120 to 240 g/kg, followed by Al (76–348 g/kg), Ca (26–113 g/kg), Fe (35–80 g/kg), and P (26–104 g/kg), and the trace elements were mainly Zn, Ba, Cu, and Mn. Not all the major elements were derived from SS. Most trace elements in the SS incineration residues accounted for 82.4%–127% of those from SS, indicating that SS was the main source of trace elements. The partitioning of heavy metals in the SS incineration residues showed that electrostatic precipitator ash or cyclone ash with high production rates were the major pollutant sinks. The differences in some major and trace elements could be indicators to differentiate SSA from CFA and MSWIA. Compared with related land criteria, the pollutants in SSA should not be ignored during disposal and utilization.     

省会城市不同功能区大气PM2.5化学组分季节变化及来源分析

为探究城市不同功能区大气PM_2.5污染水平、成分季节差异特征以及来源,采集了省会城市济南市2019年不同季节（春、秋、冬）3类典型功能区（城市市区、工业区、城乡结合区）和环境背景点植物园区的PM_2.5样品,对其浓度[ρ(PM_2.5)]、化学组分（水溶性离子、碳质组分、元素）和来源进行分析.结果表明采样期间3类功能区ρ(PM_2.5)在空间上呈现：工业区[（89.88±49.25）μg·m^-3]>城乡结合区[（86.73±57.24）μg·m^-3]>城市市区[（70.70±44.89）μg·m^-3],远大于植物园区[（44.36±21.54）μg·m^-3].各功能区ρ(PM_2.5)秋冬季明显高于春季,冬季最高值出现在城乡结合区,春季和秋季均为工业区最高.工业区各季PM_2.5中的水溶性离子浓度较高,主要的水溶性离子NO^-₃     

秦皇岛市陆地植被与大气碳平衡研究

地球的碳循环已成为全球气候变化的一个热点,陆地植被是地球破循环中的一个重要贮存库。本文在分析秦皇岛市陆地植被状况的基础上,对CO_2排放量和吸收量进行了估算,结果表明,陆地植被吸收CO_2的数量占排放量的79％。结合秦皇岛市的实际,提出有利于大气碳平衡的对策。     

EVAPOTRANSPIRATION AND SOIL MOISTURE DYNAMICS ON A SEMIARID PONDEROSA PINE HILLSLOPE1

ABSTRACT: Detailed measurements of soil moisture and ET in semiarid forest environments have not been widely reported in the literature. In this study, soil moisture and water balance components were measured over a four‐year period on a semiarid ponderosa pine hillslope, with evapotranspiration (ET) determined as the residual of measured precipitation, runoff, and change in soil moisture storage. ET accounts for approximately 95 percent of the water budget and has a distinctly bimodal annual pattern, with peaks occurring after spring snowmelt and during the late summer monsoon season, periods that coincide with high soil moisture. Weekly growing season ET rates determined by the hillslope water balance are found to be invariably below calculated potential rates. Normalized ET rates are linearly correlated (r²= 0.62) with soil moisture; therefore, a simple linear relation is proposed. Growing season soil moisture dynamics were modeled based on this relation. Results are in fair agreement (r²= 0.63) with the observed soil moisture data over the four growing seasons; however, for two dry summers with little surface runoff, much better results (r² > 0.90) were obtained.