Identification of Acceleration Pulses of Near-Fault Earthquake Ground Motion by Wavelet

Acceleration pulses have been found in near-fault earthquake ground motions long ago and attracted lots of researchers, since such pulses, especially low frequency pulses have great impact on engineering structures. Many people previously focused on velocity pulses which result from acceleration pulses, however, recently a few researchers began to directly study acceleration pulses, such as to get high frequency pulses and low frequency pulses with empirical mode decomposition. Wavelet transform was utilized to decompose acceleration records. Subsequently high frequency and low frequency components of the records were obtained and acceleration pulses were identified. By comparisons in response spectra and structural nonlinear responses, it is proved that the decomposition of acceleration records with wavelet is reliable and the identification of acceleration pulses is correct.     

农村土地流转的理论审视与现实路径解析

促进和规范农村土地流转是当前农村全面小康社会建设和新农村建设的重要内容之一。当前,应积极进行农村土地流转的理论分析,促进农村土地流转的法制化,完善政府的引导、管理和服务职能,积极建立和完善农村土地流转机制,建立健全农村社会保障体系。     

不同水分条件下冬小麦浅层地下水利用试验研究

使用蒸渗仪群开展了冬小麦对浅层地下水利用试验,讨论了在降雨、灌溉和不同地下水埋深等多种水分条件下冬小麦对浅层地下水的利用规律,并确定了适宜冬小麦生长的地下水埋深上限和相应的合理灌水量。结果表明,从返青至收获期,在40~150 cm埋深范围内,无灌溉无降雨条件下地下水对作物腾发的贡献率可达到90.0%以上,而降雨和灌溉处理的地下水贡献率减小到54.0%~78.9%。另外,无论是否有降雨影响,随着地下水埋深的增加,地下水贡献率都降低。试验结果还表明,150 cm是适宜冬小麦生长的地下水埋深上限,每公顷穗数较大是冬小麦产量高于其他埋深处理的主要原因。从返青至灌浆期,在150 cm埋深下,只需在拔节期灌水约60.0 mm,冬小麦产量就可达到8 846 kg/hm2,在无灌水和降雨时产量可达到拔节灌溉处理的80.0%左右。     

集对分析法在地下水水质评价中的应用

同一级别不同地区的地下水水质会因评价指标数值的差异而有所差别,将集对分析法运用到地下水水质评价中,可以先通过计算评价样本与评价指标之间的联系度对样本作初步的排序,再对样本作进一步的同一、差异、对立的集对分析以判断出评价样本的等级.研究结果表明:评价结果与采用其他评价方法时基本一致,且集对分析法简便、实用,计算结果客观、稳定,是一种有效的水质评价方法.     

秸秆覆盖的土壤温度效应及其对玉米生长的影响

针对黑龙江西部风沙土区气温偏低影响玉米生长的问题,在黑龙江省杜蒙县进行了免耕秸秆覆盖研究.结果表明,秸秆覆盖处理较对照表现为白天降温晚上增温的效应,增温效果与土壤深度呈抛物线形,15～20 cm增温效果最好.整个生育期表现为拔节期前降温,拔节后增温的效应.前期降温影响大于后期增温影响,玉米各生育期生物性状均差于对照,说...     

内蒙古河套灌区隆胜节水农业示范区水盐动态分析

通过水管部门组织科技人员对河套灌区调研为基础,以农业综合节水为目的,在灌区的中游永济灌域隆胜乡境内建设了节水农业示范区,面积为0.28万hm2.节水农业改造工程主要措施:渠道防渗衬砌、平地缩块.节水农业改造工程2002年竣工后,在运行中监测了3年,得出灌溉水量平均减少了12.3%;对示范区水盐动态进行了分析.     

地源热泵稻谷干燥机板翅换热器的设计与试验

针对稻谷干燥机作业成本过高和干燥后的物料品质差的问题,将地源热泵技术应用于稻谷干燥机,设计了一套板翅式换热器加热空气,计算得出芯体结构与技术参数,以降低单位作业量成本,提高干燥后的物料品质。试验研究表明:当环境温度为环境温度16℃、空气相对湿度53.2%时,地源热泵稻谷干燥机与燃油稻谷干燥机的稻谷含水率降低速率无明显区别,稻谷干燥性能可达到同等效果;地源热泵稻谷干燥机干燥稻谷的单位作业量成本0.040 7元,而燃油稻谷干燥机干燥稻谷的单位作业量成本为0.190 5元,单位作业量成本明显降低;地源热泵稻谷干燥机的稻谷干燥不均度干燥前后降低幅度0.40%小于燃油稻谷干燥机的0.72%;地源热泵稻谷干燥机的破损率增加值0.16%,小于燃油稻谷干燥机的0.31%,地源热泵稻谷干燥机的爆腰率增加值2.0%,小于燃油稻谷干燥机的3.0%,干燥后的物料品质明显提高。     

地温空调井抽回灌效果影响关键因子识别

为了探析引起地温空调井抽回灌效果的主要制约因素,通过单相关系数分析、主成分绝对得分的源解析模型、拟合度检验和多元线性回归的方法分析影响单井回灌效率的影响因素。结果表明:井径、滤水管孔隙率及抽回灌井数比与单井回灌效率的相关性和拟合度较好,故将井径、滤水管孔隙率及抽回灌井数比作为影响单井回灌效率的关键因子,同时分析了单井回灌效率与关键因子的之间的拟合方程及多元线性回归方程,得到了单井回灌效率与关键因子之间的定量关系。     

The importance of sub‐peat carbon storage as shown by data from Dartmoor,UK

Peatlands are highly valued for their range of ecosystem services, including distinctive biodiversity, agricultural uses, recreational amenities, water provision, river flow regulation and their capacity to store carbon. There have been a range of estimates of carbon stored in peatlands in the United Kingdom, but uncertainties remain, in particular with regard to depth and bulk density of peat. In addition, very few studies consider the full profile with depth in carbon auditing. The importance of sub‐peat soils within peatland carbon stores has been recognized, but remains poorly understood and is included rarely within peatland carbon audits. This study examines the importance of the carbon store based on a study of blanket peat on Dartmoor, UK, by estimating peat depths in a 4 × 1 km survey area using ground penetrating radar (GPR), extraction of 43 cores across a range of peat depth, and estimation of carbon densities based on measures of loss‐on‐ignition and bulk density. Comparison of GPR estimates of peat depth with core depths shows excellent agreement, to provide the basis for a detailed understanding of the distribution of peat depths within the survey area. Carbon densities of the sub‐peat soils are on average 78 and 53 kg C/m³ for the overlying blanket peat. There is considerable spatial variability in the estimates of total carbon from each core across the survey area, with values ranging between 56.5 kg C/m² (1.01 m total depth of peat and soil) and 524 kg C/m² (6.63 m total depth). Sub‐peat soil carbon represents between 4 and 28 per cent (mean 13.5) of the total carbon stored, with greater values for shallower peat. The results indicate a significant and previously unaccounted store of carbon within blanket peat regions which should be included in future calculations of overall carbon storage. It is argued that this store needs to be considered in carbon audits.