油松容器苗和裸根苗生长与造林效果对秋季施肥的响应

【目的】探究不同秋季施肥处理条件下油松容器苗和裸根苗苗期生长、养分积累和造林效果的差异,为生产上培育油松良种壮苗提供理论基础和技术支持。【方法】以大田培育的当年生油松播种容器苗和裸根苗为研究对象,设置0(对照)、12、24、36 mg/株4种秋季施肥水平,于90%以上苗木形成顶芽后进行施肥处理,并于翌年进行雨季造林试验。测定造林前的苗高、地径、生物量、根冠比、养分含量及造林后苗木成活率和苗高、地径相对生长量等指标,分析出圃苗木性状与造林效果之间的相关性。【结果】秋季施肥24 mg/株处理下的油松容器苗苗高、地径、生物量、氮、磷、钾含量均表现最佳,该处理下容器苗整株生物量、氮、磷、钾含量较对照分别增加了41.8%、31.4%、65.6%和48.8%;油松裸根苗受秋季施肥影响较小。容器苗氮含量在各器官中的分布从大到小表现为根>叶>茎,裸根苗氮含量在各器官中的分布从大到小表现为叶>根>茎;磷、钾含量在容器苗和裸根苗各器官中的分布从大到小均表现为叶>根>茎。雨季造林试验结果显示,油松造林效果受苗木类型影响显著,容器苗造林当年和第2年春季的苗高、地径相对生长量...     

冷再生泡沫沥青混合料水稳定性研究分析

通过控制新集料掺加比例、泡沫沥青用量、水泥剂量、集料温度和抗剥落剂等,研究各因素对冷再生泡沫沥青混合料的路用性能和水稳定的影响,并揭示其微观机理.结果表明,旧料利用率、泡沫沥青用量、水泥剂量和抗剥落剂宜分别控制在50%～75%、 2.5%～3.0%、 1.0%～1.5%和0.5%左右.此外,适当提高集料温度,有助于提高泡沫沥青分散均匀性,从而提升冷再生泡沫沥青混合料的水稳定性.泡沫沥青用量和水泥剂量是冷再生泡沫沥青混合料水稳定的关键因素.尽量使泡沫沥青分散均匀,避免产生结团现象,是保证冷再生泡沫沥青混合料水稳定性的基础,进一步通过水泥补强作用,可获得良好的水稳定性.     

Improvement in hydrogen storage performance of Mg by mechanical grinding with molten salt etching Ti3C2Clx

Mg-based materials are currently a hot research topic as hydrogen storage materials due to their considerable theoretical hydrogen storage capacity. However, the kinetic performance of hydrogen absorption and desorption of Mg is too slow and requires high temperature, which seriously hinders the application of this material. MXene is a new type of two-dimensional material with significant role in improving thermodynamics and kinetics. In this experiment, a two-dimensional layered MXene containing Cl functional group was prepared by molten salt etching using the Ti-containing MAX phase as the raw material. Then different ratios of Ti₃C₂Cl_x were uniformly dispersed onto the surface of Mg by high energy ball milling. The samples were characterized by hydrogen absorption and desorption kinetics, SEM, XRD, XPS, and DSC to investigate the effect of Ti₃C₂Cl_x on the hydrogen absorption and desorption performance of Mg. The onset hydrogen absorption temperature can be reduced to room temperature and the hydrogen release temperature is reduced by 200 ​°C by doping Ti₃C₂Cl_x. And there is also 5.4 ​wt% hydrogen storage in the isothermal hydrogen absorption test at 400 ​°C. The results of DSC demonstrate that the E_a of Mg+15 ​wt% Ti₃C₂Cl_x was reduced by 12.6% compared to pristine Mg. The ΔH is almost invariable. The results of XPS show that the presence of multivalent Ti promotes electron transfer and thus improves the conversion between Mg²⁺/Mg and H⁻/H. This study provides a guideline for further improving the hydrogen absorption and desorption performance of Mg-based hydrogen storage materials.     

蓄电池容量自动测试仪

本文根据国标《CB5008.1～3—85》的规定,设计了一种蓄电池容量自动测试仪.该仪器利用8位单片计算机进行控制,完成测试过程中的自动恒流、自动测量时间和温度、自动进行数据处理、自动停机等功能.它的优点是操作简单,测量精度高,成本低.本文介绍了蓄电池容量的测量原理和计算方法,对单片机的硬件和软件系统都做了全面的叙述.     

回流充气法处理中,高量含铁地下水的研究

本文介绍一种深井回流充气工艺,它兼具充氧和除铁综合性能的新型工艺形式,能改善含铁地下水的过滤性能.在此基础上提出了深井回流充气稳定期的概念,建立了深井回流充气系统中氧量的平衡关系.通过正交试验,提出了处理中、高量含铁地下水的推荐工艺流程和工艺参数.采用χ—射线衍射方法测试了井内铁泥和成熟滤料表面滤膜的成分和形态,分析了"充气"和"过滤》两过程中的除铁机理.     

秦淮河流域典型排涝泵站前池水质与降雨特征响应关系

为分析排涝泵站前池水质与降雨特征的响应关系,对南京市城区秦淮河沿线2个排涝泵站前池水质以及降水量开展高频在线自动监测,结合回归树方法分析了不同降雨强度、前期干旱时间条件下排涝泵站前池水质变化规律,探讨了不同类型排涝泵站前池水质的主要影响因素。结果表明:晴雨天均有生活污水汇入的A泵站前池氨氮质量浓度在大雨强下降低,中雨强下先升高后降低,小雨强下平缓上升,A泵站前池污染物质量浓度主要受降雨强度和次降水量影响;主要接收降雨径流,雨量大时有生活污水溢流汇入的B泵站,前池污染物质量浓度在大雨强下先升高后逐渐降低,中雨强下降低,小雨强下变化不大,B泵站前池水质主要受次降水量、前期干旱时间和降雨强度影响;2个泵站前池CODMn质量浓度变化与降雨的响应规律相似,但更多受到与前期干旱时间关联的地表径流冲刷作用影响;连续降雨均导致泵站前池氨氮质量浓度和CODMn质量浓度波动变化较大,而前期干旱时间越长,降雨发生后泵站前池水质越差。     

基于水光电力系统时序生产模拟模型的水光优化配比研究

基于考虑系统负荷、新能源发电出力等时序变化特性的时序生产模拟法,建立了水光电力系统时序生产模拟模型;从系统结构性、经济性、灵活性与可靠性方面综合确定最佳水光容量配比,并通过金沙江上游川藏段水光系统验证了模型的合理性。金沙江上游川藏段光伏电站与水电站出力具有较好的年内、日内互补特性;对于2030年水平年,考虑枯期水电留存,913.6万kW水电配套400万kW光伏的方案综合性能更优,其新增非水可再生电量约60亿kW·h。     

贵州省粮食储藏地理区划初步研究

通过对贵州省气象特征的分析,尤其是对影响粮食安全储藏的主要环境因素温度和相对湿度的分析,得出贵州省粮食储藏可划分为四个地理区域。依据各区域的储藏气候条件和主要粮食的储藏特点,提出相应的储藏技术措施。     

Sea water intrusion and salt water intrusion in the coastal area of Laizhou Bay

The characteristics, pattern, hydrodynamic and hydrochemical features, and the movement pattern of the salt waterfresh water interface of the sea water intrusion and the salt water intrusion, which occur in the coastal area of Laizhou Bay in Shandong Province, are analysed. The characteristics of the two kinds of intrusion are compared as well. A three-dimensional sea water intrusion model to describe the sea water intrusion with a transitional zone 1.5–6.0 km wide in the phreatic aquifer and a solute transport model describing the behavior of cations exchange in the process of sea water intrusion are established.