火山喷出物发育土壤的比重及颗粒组成测定

利用比重瓶法对火山喷出物发育土壤的比重进行测定,结果表明:玄武岩质火山喷出物发育土壤的比重大于粗面岩质火山喷出物发育土壤的比重;基于粒径小于1 mm土粒测定的比重,玄武岩质火山喷出物和粗面岩质火山喷出物发育土壤的比重均小于一般土壤的平均比重2.65 g cm~(-3);基于粒径小于0.1 mm土粒测定的比重,除个别玄武岩质火山喷出物发育土壤外也小于2.65 g cm~(-3)。分别取比重值为2.65 g cm~(-3)、粒径小于1 mm土粒的实测比重和粒径小于0.1 mm土粒的实测比重,计算不同粒级土粒的沉降时间,并进行颗粒组成的实验研究表明:取不同比重值测定的土壤颗粒组成含量相差较大而且影响土壤质地定名。由于成土母质的矿物组成决定土壤的比重,且土壤颗粒组成的静水沉降实验是在粒径小于0.1 mm土粒的悬液中进行的,所以,准确测定土壤颗粒组成含量,需要区分成土母质的矿物组成,并测定其小于0.1 mm粒径的土粒比重,重新计算沉降时间。     

环境因子对山西太岳山土壤微生物量的影响

本文以山西太岳山两个林型(华北落叶松人工林、灌木林)下阴坡和阳坡的土壤样品为研究对象,研究了不同坡向下土壤微生物量碳、氮、土壤理化性质、土壤微生物碳氮比值的变化特征。研究结果表明:土壤有机碳、全氮、微生物量碳、氮含量在0~10 cm土层均显著高于10~20 cm土层。在华北落叶松人工林和灌木林下,土壤微生物量碳、可溶性有机碳及两者之和在阳坡均显著高于阴坡;土壤微生物量碳占两者之和的比例约为81%~87%,在不同坡向下没有显著性差异。土壤微生物量碳氮比在灌木林阳坡下为6.5~7.2,阴坡为7.3~9.9;在华北落叶松人工林阳坡下为7.3~8.6,阴坡为8.2~8.6。两种林型下土壤微生物熵在阳坡均高于阴坡。相关性分析结果表明,土壤微生物量碳、氮与土壤pH值、可溶性有机碳呈显著正相关,土壤有机碳与土壤全氮、微生物量碳、pH值和含水率均有显著正相关性。总的来说,不同坡向对土壤微生物量产生重要影响,进而使土壤微生物熵不同,阴坡土壤有机碳活性较小,碳库的稳定性较好。本文从土壤微生物量及其与环境因子相互关系的角度探讨了土壤环境对土壤微生物的影响,以期为更好的理解该地区土壤碳周转和植被恢复生态效应提供参考。     

土壤盐渍化高光谱特征分析与建模

基于高光谱遥感技术快速、无损的检测优势,以新疆渭干河-库车河三角洲绿洲为例,探讨利用反射光谱来预测土壤含盐量的可行性。利用野外采集的土壤样本,在实验室内测得了土壤含盐量及原始光谱反射率。利用光谱分析技术计算高光谱指数,与土壤样本含盐量进行相关性分析,筛选出土壤含盐量的光谱特征波段,基于逐步多元线性回归和偏最小二乘回归建立土壤盐分动态监测模型。通过精度检验,结果表明:基于偏最小二乘回归方法,以对数二阶微分光谱特征波段所构建的盐渍化遥感监测模型最优,模型的稳定性和预测精度最高。利用反射光谱来预测土壤含盐量可实现区域尺度上的土壤盐渍化实时监测和评价。     

长期不施钾肥对华北平原潮土钾素动态演变的影响研究

利用长期定位试验探讨了施氮磷肥、秸秆还田和不同耕作方式下长期不施钾肥对土壤速效钾变化及其对作物产量的影响。结果表明:长期不施钾肥土壤速效钾处于下降趋势:30年内耕层(0~20 cm)土壤速效钾含量降低了26.46%~54.64%,年均降低0.88%~1.82%;而亚耕层(20~40 cm)降低了10.66%~42.22%,年均降低0.36%~1.41%。在前15年(1985~2000年)土壤速效钾含量减少的速度较缓慢,而中10年(2000~2010年)则较快,2010年以后则较为平缓。长期不施钾肥、但同时施用氮磷肥将促进作物对土壤钾素的消耗;较高作物产量可导致速效钾的大量减少,而单施氮肥或磷肥处理的土壤速效钾含量变化较小。秸秆还田缓解了土壤钾素的减少,但对弥补土壤钾素的亏损作用很小。免耕相对于秸秆覆盖还田和秸秆翻耕还田对土壤钾素亏损的影响较少,但因其作物产量较低,秸秆翻耕还田较有利于作物产量的提高。     

北美中部大平原半干旱农业生态系统中覆盖作物和灌溉对土壤微生物群落和酶活性的影响

Cover crops can have beneficial effects on soil microbiology by increasing carbon (C) supply, but these beneficial effects can be modulated by precipitation conditions. The objective of this study was to compare a fallow-winter wheat (Triticum aestivum L.) rotation to several cover crop-winter wheat rotations under rainfed and irrigated conditions in the semiarid US High Plains. Experiments were carried out at two sites, Sidney in Nebraska and Akron in Colorado, USA, with three times of soil sampling in 2012--2013 at cover crop termination, wheat planting, and wheat maturity. The experiments included four single-species cover crops, a 10-species mixture, and a fallow treatment. The variables measured were soil C and nitrogen (N), soil community structure by fatty acid methyl ester (FAME) profiles, and soil β-glucosidase, β-glucosaminidase, and phosphodiesterase activities. The fallow treatment, devoid of living plants, reduced the concentrations of most FAMEs at cover crop termination. The total FAME concentration was correlated with cover crop biomass (R = 0.62 at Sidney and 0.44 at Akron). By the time of wheat planting, there was a beneficial effect of irrigation, which caused an increase in mycorrhizal and protozoan markers. At wheat maturity, the cover crop and irrigation effects on soil FAMEs had subsided, but irrigation had a positive effect on the β-glucosidase and phosphodiesterase activities at Akron, which was the drier of the two sites. Cover crops and irrigation were slow to impact soil C concentration. Our results show that cover crops had a short-lived effect on soil microbial communities in semiarid wheat-based rotations and irrigation could enhance soil enzyme activity. In the semiarid environment, longer time spans may have been needed to see beneficial effects of cover crops on soil microbial community structure, soil enzyme activities, and soil C sequestration.     

使用便携式X射线荧光（PXRF）法原位区分酸性和非酸性冻土带

Frozen soils or those with permafrost cover large areas of the earth’s surface and support unique vegetative ecosystems. Plantsgrowing in such harsh conditions have adapted to small niches, which allow them to survive. In northern Alaska, USA, both moistacidic and non-acidic tundra occur, yet determination of frozen soil pHs currently requires thawing of the soil so that electrometric pHmethods can be utilized. Contrariwise, a portable X-ray fluorescence (PXRF) spectrometer was used in this study to assess elementalabundances and relate those characteristics to soil pH through predictive multiple linear regressions. Two operational modes, SoilMode and Geochem Mode, were utilized to scan frozen soils in-situ and under laboratory conditions, respectively, after soil sampleswere dried and ground. Results showed that lab scanning produced optimal results with adjusted coefficient of determination (R²) of0.88 and 0.33 and root mean squared errors (RMSEs) of 0.87 and 0.34 between elemental data and lab-determined pH for Soil Modeand Geochem Mode, respectively. Even though the presence of ice attenuated fluoresced radiation under field conditions, adjusted R² and RMSEs between the datasets still provided reasonable model generalization (e.g., 0.73 and 0.49 for field Geochem Mode). Principalcomponent analysis qualitatively separated multiple sampling sites based on elemental data provided by PXRF, reflecting differences inthe chemical composition of the soils studied. Summarily, PXRF can be used for in-situ determination of soil pH in arctic environments without the need for sample modification and thawing. Furthermore, use of PXRF for determination of soil pH may provide highersample throughput than traditional eletrometric-based methods, while generating elemental data useful for the prediction of multiplesoil parameters.     

基于奇点分布法的轴流泵叶片翼型设计与计算

为将奇点分布法这一有优势的流体机械叶片翼型设计方法应用于轴流泵叶轮叶片设计,以平面势流理论及数值计算为基础,推导了基于适合轴流泵叶片翼型边界条件的漩涡密度函数的系统应用性计算公式,所获结果将准确确定各翼型骨线关键节点位置,它们形成的翼型骨线在满足给定设计点泵的性能参数的同时,还能形成要求的流动奇点与驻点,由此产生流动损失最小的叶片翼型。以该方法改型设计的一台轴流泵的型式试验表明,设计泵在设计点的效率由原来的78%提升到85%,特性曲线符合要求。该研究深化了轴流泵叶轮叶栅流动理论,将奇点分布理论转化为轴流泵叶轮翼型的实用设计方法,为设计技术人员提供了开发新产品的工具。     

树型喷洒靶标外形轮廓探测方法

为了在线探测靶标外形并为变量喷药提供基础支持,研究了树型喷洒靶标外形轮廓探测方法。该文基于超声传感器搭建了靶标外形轮廓探测试验平台,该平台能够驱动步进电机精确匀速运动,以0.02 m为步长密集测量树冠形状,将获得的数据传给计算机实时显示,并能够在Access数据库中长期存储。使用该测试平台针对自制规则树树冠和花期樱桃树树冠分别进行了试验。试验结果显示规则树冠和樱桃树冠体积探测精度分别为92.8%和90.0%,表明该方法具有较高探测精度。     

高养分富集植物凤眼莲的农田利用研究

研究不同凤眼莲施用量条件下土壤养分变化以及小麦生长情况的结果表明:当凤眼莲施用量低于8.1kg·m-2,小麦出苗数不受影响;但当凤眼莲施用量超过8.1kg·m-2时,小麦出苗率显著降低。凤眼莲施用量为13.5kg·m-2时,尽管小麦出苗率显著降低,但由于具有较多的分蘖数和较高的每穗粒数,小麦最终产量与常规单施化肥处理间无显著差异。不同凤眼莲施用处理的土壤速效氮苗期差异显著,但分蘖期后处理间无显著差异;而速效磷和速效钾总体表现为随凤眼莲施用量增加而升高。此外,凤眼莲施用还可促进小麦茎秆对N、P、K的吸收和籽粒粗蛋白含量的增加。由此可见,凤眼莲是一种经济有效的农田有机肥料,其施用量以10.8～13.5kg·m-2为宜,施用后土壤N、P、K、有机质含量较高,且对产量影响不大,当季还可节约施用化学N141.75kg·hm-2、P36～45kg·hm-2,K可免施。     

利用磷进行铅污染土壤原位修复中需考虑的几个问题

由于土壤中磷与铅形成难溶性的磷酸铅类化合物[Pb5(PO4)3X,X=Cl-,OH-,F-等],利用不同廉价含磷物质进行铅污染土壤原位修复被认为是目前最好的铅污染土壤管理措施,受到国内外广泛关注。本文对目前国内外利用磷进行铅污染修复研究的现状进行了综述,对该研究领域中的关键问题,如磷酸铅类化合物形成的反应动力学过程控制、最佳pH、土壤中磷/铅摩尔比等进行了较深入的探讨,并展望了今后的研究方向,以期为铅污染土壤的修复及其效果评价提供参考。