草原沙化和人工固沙草地生态演替中昆虫群落多样性变化的数值分析

对宁夏沙坡头自然保护区不同沙化和人工固沙草地地段昆虫和植物群落特征参数、环境因子进行了调查．按不同营养层类群、栖息型类群和重要目分别进行了昆虫多样性变化规律的研究,应用主分量分析法和相关分析法,分析了草原沙化和人工固沙草地生态演替中昆虫不同类群多样性间以及多样性变化与植物、环境因子的关系．结果表明,昆虫多样性随草地沙化的加重而降低,以直翅目、膜翅目和食叶类群的下降率最大;随草地的恢复昆虫多样性趋于增加,以鳞翅目、同翅目、半翅目、脉翅目及捕食类群增长率为大．寄生类群和捕食类群多样性取决于植食类群多样性;杂食类群与地栖性类群成显著性相关．影响昆虫多样性变化的主要环境因子为植物种类、层次结构、盖度和表土层厚度、坚硬度等．     

The GANE Roof Project: The impact of reduced N & S deposition and experimental warming in an acid grassland

A field-based system used to quantify the response of acid grassland to reduced atmospheric nitrogen and sulphur deposition, and to investigate the effects of elevated soil temperature on acid grassland development is described. The system is based on 12 retractable roofs, covering undisturbed experimental plots of acid grassland and three controls. Nine roofs are used to exclude natural precipitation and three roofs used to retain emitted IR radiation at night. An irrigation system has been developed to simulate natural precipitation, allowing for the application of specific treatment regimes of ambient, reduced nitrogen and reduced nitrogen/sulphur deposition beneath the nine rain exclusion plots. Plant, soil parameters, leachate chemistry and gaseous fluxes are being monitored and initial results on soil water chemistry are described. Warming appeared to enhance nitrate concentrations in soil water but this was not sustained beyond the first year of treatment. In contrast, the deposition reduction treatments decreased soil water nitrate concentrations within a few weeks of reducing deposition. This was not observed for other solutes such as sulphate or ammonium suggesting a more direct link between deposition of nitrate and leaching losses.     

外源Cl-添加对不同母质土壤溶液Cd2+浓度的影响

土壤镉(Cd)的环境行为与其在土壤溶液中的存在形态以及陪伴离子有关,然而外源Cl~-与土壤溶液中Cd~(2+)的关系以及不同母质土壤对Cd~(2+)的环境行为的影响并没有明确的结论.选取2种水稻土(第四纪红色黏土母质发育的红黄泥、紫色砂页岩母质发育的紫泥田)为研究对象,添加离子态外源Cd~(2+)(0、1、2.5、5 mg·kg~(-1)),平衡老化后添加外源Cl~-(0、0.6、1.2 mg·kg~(-1)),在保持水分恒定的情况下进行模拟培养试验,研究外源Cl~-添加对土壤溶液Cd~(2+)浓度的影响.结果表明,随着外源Cd~(2+)的增加,土壤溶液Cd~(2+)的浓度提高,红黄泥土壤溶液Cd~(2+)的浓度显著高于紫泥田;添加Cl~-会使土壤溶液中Cd~(2+)浓度升高,且Cd~(2+)浓度与外源Cl~-呈显著正相关,红黄泥和紫泥田土壤溶液中Cd~(2+)的平均浓度比不添加Cl~-时Cd~(2+)的平均浓度分别增加了12.74%、51.49%;土壤对Cd~(2+)的吸附关系符合Freundlich等温吸附方程,紫泥田对Cd~(2+)的吸附量显著高于红黄泥,添加Cl~-对红黄泥Cd~(2+)的吸附影响很小,而对紫泥田的影响显著.Cl~-存在下,红黄泥和紫泥田的解吸率分别为12.50%～19.25%、14.76%～24.99%,外源Cl~-添加对Cd~(2+)解吸影响小.综合分析认为,Cl~-对不同土壤Cd~(2+)的吸附解吸行为影响有较大的差异.     

西安市大气颗粒物数浓度分布及典型天气条件特征变化

利用2013年3月到2014年12月期间西安市大气中0.25～32μm颗粒物监测数据和同期气象参数、散射消光系数等数据,分析了大气颗粒物数浓度分布及典型天气条件下变化特征.结果表明:采样期间西安市大气颗粒物平均数浓度为206.27个/cm3, 99%以上为<1μm的颗粒物数.大气颗粒物数浓度冬季最高,其次为秋、夏和春季,分别为267.66、231.31、141.82和135.77个/cm3.四季的数浓度低值均出现在18:00左右,之后数浓度上升,且晚上高于白天,冬季6:00左右达到峰值,夏季的昼夜差最小,秋季最大.春夏秋冬的大气颗粒物数浓度与散射消光系数的Pearson相关系数分别为0.756、0.702、0.411、0.377.大气颗粒物数浓度在沙尘天气发生前、中、后会升高、下降和再下降,霾天气出现前、后会升高和下降;高温干燥天气下,大气颗粒物数浓度相对较低;降雨对大气颗粒物的清除作用明显,但降雨后大气颗粒物数浓度又很快回升.     

春季不同天气城市街头绿地内PM2.5质量浓度分布特征研究

于2012年春季,采用水平分布监测法监测了3种天气下距交通污染源不同距离的街头绿地中的PM2.5质量浓度,研究了不同天气下PM2.5的日变化、水平分布规律及绿地对PM2.5的净化效应,为城市街头绿地、城市公园建设及市民合理选择休闲锻炼时间和地点提供理论依据。结果表明：1）晴天和多云时,PM2.5质量浓度上午高于下午,7：00浓度最高,15：00最低;雨后阴天基本保持上升趋势。2）PM2.5日均质量浓度为晴天（61.67μg·m-3）〈多云（187.98μg·m-3）〈雨后阴天（291.48μg·m-3）。晴天除5：00和7：00外,其他时刻均达到国家二级标准,且13：00—15：00达到国家一类功能区空气质量要求;多云和雨后阴天PM2.5质量浓度分别超过国家二级浓度限值150.6%和288.6%。3）观测时段内,无论哪种天气,5：00、7：00、11：00和15：00绿地的净化功能较强,19：00净化功能均最差,所有监测点无一例外的表现为负效应。4）3种天气下,PM2.5质量浓度在距离道路10~25 m最高,绿地的净化效应最差,55 m外基本可以形成稳定的森林内环境。5）在南方高湿环境下,空气相对湿度是影响PM2.5质量浓度的主要因素,晴天和多云天气PM2.5浓度与相对湿度呈显著正相关,而雨后阴天二者呈负相关关系。6）在一定阈值内,街头绿地能够缓解PM2.5污染,为居民提供良好的休闲环境。从游憩时间来看,市民可以选择晴天进入街头绿地休闲,多云和雨后阴天尽量减少外出;从活动最佳地段来看,距离污染源55 m以上适宜休闲锻炼;从街头绿地的规划面积来看,半径以不小于55 m为宜。     

放牧与围栏羊草草原土壤呼吸作用及其影响因子

基于静态箱式法连续2a的测定资料,比较分析了内蒙古典型羊草草原放牧与围栏样地土壤呼吸作用及其与各影响因子的关系.结果表明:①围栏内外土壤呼吸作用日、季动态差异不大,但围栏样地土壤呼吸速率明显高于放牧样地,其平均值分别是219.18 mg·(m²·h)^-1和111.27 mg·(m²·h)^-1,围栏样地土壤呼吸作用的升高可能与地下生物量增加和土壤水分改善有关;②对影响土壤呼吸作用的因子分析表明,放牧使土壤水分和相对湿度的影响明显降低,而对气温、大气CO₂浓度和光合有效辐射的影响并不大,且放牧使羊草净光合速率的影响明显增加,而对气孔导度和胞间CO₂浓度影响不大;③围栏样地土壤呼吸作用与各影响因子的相关性从大到小依次为土壤水分、净光合速率、气温、相对湿度、大气CO₂浓度、胞间CO₂浓度、气孔导度和光合有效辐射,其中土壤水分和气温是影响土壤呼吸作用的主要环境因子,净光合速率是主要的生物因子.尽管放牧改变了土壤呼吸速率,但土壤呼吸作用各影响因子的排列顺序基本上没有改变,只是发生了量的变化.     

持续放牧和围封对科尔沁退化沙地草地碳截存的影响

研究了科尔沁退化沙地草地持续放牧和围封恢复下土壤-植物系统的碳(C)贮存,以揭示草地管理对C动态的影响.结果表明,0～15cm土壤OC和植物系统贮存的C(包括初级生产固定的C,立枯和地表凋落物C和根系C)贮量大小为:围封10年草地(584g·m^-2和309 g·m^-2)＞围封5年草地(524g·m^-2和146g·m^-2)＞持续放牧草地(493g·m^-2和95 g·m^-2).在围封10年,围封5年和持续放牧草地中,0～15cm土壤贮存C分别占各自土壤-植物系统C的65.3%,78.2%和83.9%.在风蚀严重的科尔沁沙地,持续放牧对植被,土壤及其周围环境有极严重的恶化作用.采取围封恢复措施后,植被恢复和凋落物积累使土壤免遭风蚀,也显著增加了土壤有机质的输入,因而显著作用于大气C的截存.但排除家畜放牧的长期围封使植物C向土壤C的再循环受到限制,截存的大部分C以凋落物的形式积存在土壤表面,需进一步深入研究围封的时间尺度.研究结果表明,退化沙地草地在采取有效的保护措施后,可以由C源变为C汇.     

Does low N-mineralisation rate in soils under grass help limit nitrate leaching in summer?

This paper aimed to confirm the hypothesis that rates of ammonification and net mineral-N production in soils under grass in summer are low and this, rather than nitrate uptake by plants, reduces mineral leaching from soils in summer. Six sets of soil samples were collected from under mown grass on the University of York campus in the UK. Samples were taken from two depths in late summer (August) and late autumn (November) to compare seasonal differences in N species transformations when field-moist soils were incubated for a week at ambient outdoor temperatures after prior removal of vegetation. Ammonification and net mineral-N production rates were low in August in spite of warm temperatures. Net mineral-N production rates were also low in November. The results agreed with those of an earlier study in a different year after considering weather differences between years. They support the hypothesis that litter accumulated over autumn/winter will be minimally mineralised and retain N before the temperature rises in spring. The study shows the merit of measuring concentrations of mineral-N species in both fresh soils and soils incubated at ambient outdoor temperatures after removing plant material to eliminate plant N uptake effects. The results suggest that soil C% and N% are more important than soil C:N ratio alone in understanding controls on N transformations.     

Temporal change of water quality of the typical rural domestic sewage in Chaohu Lake basin

为揭示巢湖流域典型村庄生活污水水质特征,本文采用定点定期采样法,对巢湖流域两类典型村庄生活污水水质进行了2年测定研究.结果显示,不同月份两村生活污水的COD、NH4＋-N、TN、TP等指标呈现出相同的变化趋势,各指标浓度在6—8月较低,而COD和TN浓度在12—2月较高;两村的生活污水COD、NH4＋-N、TN、TP全年变化范围为46.77—424.80 mg.L-1、4.30—17.40 mg.L-1、9.36—34.38 mg.L-1、0.27—3.06 mg.L-1;大汤村和电厂新村两村生活污水全年COD、NH4＋-N、TN、TP平均值分别为171.98 mg.L-1和219.60 mg.L-1、8.07 mg.L-1和11.52 mg.L-1、17.80 mg.L-1和21.33 mg.L-1、1.15 mg.L-1和1.53 mg.L-1.     

Changes in CO2 flux for different recovery processes of desertification in the alpine meadows of Northwest Sichuan北大核心CSCD

Desertification has emerged as a serious threat to the alpine meadows of Northwest Sichuan in recent decades. Artificial vegetation had certain effects on desertification recovery, while how the CO2 flux changed and its reasons are still unclear. During the growing season in 2016 (i.e., from July to September), we selected the desertified alpine meadows with different recovery degrees, including the early stage of restoration, the middle stage of restoration, the late stage of restoration, and control (the unrecovered desertification meadow) as four transects. CO2 flux was measured by the instrument LI-8100, and the microenvironment factors that affected CO2 flux changes were analyzed. The results showed that the carbon sequestration function of desertified alpine meadows gradually increased with the degree of recovery. Net ecosystem exchange (NEE) were -1.61, -3.55, and -4.38 μmol m-2 s-1 in the early, mid-term, and late transects, respectively, and the most dramatic changes occurred from the early stage to mid-term stage, increasing by 120.50%. Both ecosystem respiration (ER) and soil respiration (SR) were enhanced significantly with restoration (P < 0.05). In mid or late July, NEE, ER, and SR reached their maximum values, and thereafter, the indicators varied to near zero (P < 0.05). During the whole growing season, the daily dynamic in CO2 flux for the control alpine meadow was mild and retained the trend of continuous release all day, but that in the desertified alpine meadow was a single peak pattern. Moreover, with restoration process, the peak of CO2 flux increased and reached a peak in the late stage of the recovery process. The regression analysis showed that there was a significant positive correlation between CO2 flux and vegetation coverage, aboveground biomass, and soil moisture (0-5 cm) (P < 0.01), and a weak correlation with 0-5-cm soil temperature (P < 0.01). This indicates that topsoil moisture (5 cm) is a more significant factor for CO2 flux than topsoil temperature during the growing season in the restoration of desertified alpine meadows in Northwest Sichuan. In general, the vegetation recovery significantly improved the carbon-sequestration ability of the desertified alpine meadows during the growing season in Northwest Sichuan, and at the middle stage of restoration, the carbon-sequestration ability improved significantly due to vegetation restoration and increase in topsoil (0-5 cm) moisture. © 2018 Science Press. All rights reserved.