水稻土肥力特性的微形态诊断

水稻土是我国的一种主要耕作土壤,分布面积广,土壤类型多,肥力特性多种多样.广大农民群众在长期生产实践中积累了丰富的识土经验^[9]1).多年来我国许多土壤工作者曾相继从土壤学各分支学科的角度对不同类型水稻土的肥力特性进行过一系列的研究.     

狗猪鹿牙齿的高耐磨特性对比

为解决土壤工作部件磨损严重的问题,该文以狗牙、猪牙、鹿牙为研究对象,采用摩擦磨损试验机进行摩擦磨损试验,考察了狗牙、猪牙、鹿牙的摩擦学性能,通过激光共聚焦扫描显微镜测量磨损深度,利用扫描电子显微镜观察狗牙、猪牙、鹿牙的磨损形貌,利用纳米压痕仪分别对狗牙、猪牙、鹿牙进行力学性能试验,测试其纳米硬度和弹性模量。试验表明：狗牙釉质磨斑表面磨屑剥落严重、附着大量的细小磨粒、有明显的龟裂现象,磨损体积为1.91×107 μm3,猪牙釉质磨斑表面主要是磨屑剥落,磨损体积为1.56×107 μm3,鹿牙釉质磨斑表面也表现为磨屑剥落,磨损程度比猪牙齿的轻,磨损体积为1.39×107 μm3;牙齿的耐磨性与其硬度密切相关;鹿牙釉质的耐磨性、纳米硬度和弹性模量最大,狗牙釉质的最小。该文以动物牙齿为仿生原型,为耐磨触土部件的研发提供新的参考方向和理论依据。     

减粘脱附柔性内衬的设计与应用

针对挖掘、装卸及运输机械的与物料接触部件,在以粘性物料为工作对象时明显存在物料粘附积留问题,依据典型脱土动物功能防粘机制所提供的信息,设计了具有明显减粘脱附效果的柔性内衬,并进行了柔性内衬用于滚轮堆取料机轮斗、挖掘机挖斗及装载机铲斗的实际试验。文中介绍了柔性内衬结构特点、设计方法及实际试验结果。     

南方红壤区植被覆盖因子估算模型构建与验证

研究红壤区植被覆盖因子变化规律、构建植被覆盖因子计算模型可为该区域水土流失防治及动态监测提供科学依据。该研究基于广东省五华县水土保持试验推广站200余场降雨试验观测数据,分析了影响水土流失的各关键因子与次降雨土壤侵蚀模数(Individual Rainfall Event Soil Erosion Modulus,ISEM)间定量关系,基于中国土壤流失方程计算了系列次降雨事件不同植被覆盖度对应植被覆盖因子值,构建了植被覆盖因子值与植被覆盖度间数学模型,从点、面2个尺度对模型计算精度进行了验证。结果表明:1)ISEM随植被覆盖度增加而降低;ISEM与雨前土壤表层含水率间存在显著正相关对数关系;ISEM随坡度增加呈先增后减的变化规律;ISEM随次降雨量、次降雨侵蚀力和次降雨径流深呈显著正相关线性变化关系。2)构建了植被覆盖因子值与植被覆盖度间二阶指数衰减模型,该模型决定系数和纳什系数分别达0.947和0.876。点尺度验证结果表明90%样本模型计算值与观测值相对误差均小于0.30;面尺度验证结果表明,70%～80%的植被覆盖因子计算值相对误差不超过0.1。总体而言,该模型计算精度较为理想,但由于研究对象典型的时空尺度特征,仍需要更多观测数据对该模型进行完善和验证。研究成果可为深入理解红壤区土壤侵蚀规律、水土流失动态监测提供有益参考。     

离心泵射流自吸装置的研究

介绍一种新型离心泵射流自吸装置的工作原理及结构，通过在普通离心泵的进口处增设一个带“文氏管”的自循环射流器，使该射流器与压水室第六断面的回流孔贯通形成自循环，当泵运转时，不仅可以完成自吸过程，而且可以将自循环射流器上的阀关闭，射流器同时停止工作，因此：泵的效率提高了3%以上。泵的性能试验分析表明，该泵不仅可以实现自吸，性能曲线稳定、平坦，高效率区范围宽，工况佳，而且泵的各项技术指标均满足设计要求。     

Inorganic and organic carbon dynamics in forested soils developed on contrasting geology in Slovenia—a stable isotope approach

Purpose

Soil carbon dynamics were studied at four different forest stands developed on bedrocks with contrasting geology in Slovenia: one plot on magmatic granodiorite bedrock (IG), two plots on carbonate bedrock in the karstic-dinaric area (CC and CD), and one situated on Pleistocene coalluvial terraces (FGS).

Materials and methods

Throughfall (TF) and soil water were collected monthly at each location from June to November during 2005–2007. In soil water, the following parameters were determined: T, pH, total alkalinity, concentrations of Ca²⁺ and Mg²⁺, dissolved organic carbon (DOC), and Cl^? as well as δ¹³C_DIC. On the other hand, in TF, only the Cl^? content was measured. Soil and plant samples were also collected at forest stands, and stable isotope measurements were performed in soil and plant organic carbon and total nitrogen and in carbonate rocks. The obtained data were used to calculate the dissolved inorganic carbon (DIC) and DOC fluxes. Statistic analyses were carried out to compare sites of different lithologies, at different spatial and temporal scales.

Results and discussion

Decomposition of soil organic matter (SOM) controlled by the climate can explain the ¹³C and ¹⁵?N enrichment in SOM at CC, CD, and FGS, while the soil microbial biomass makes an important contribution to the SOM at IG. The loss of DOC at a soil depth of 5 cm was estimated at 1 mol m^?2 year^?1 and shows no significant differences among the study sites. The DOC fluxes were mainly controlled by physical factors, most notably sorption dynamics, and microbial–DOC relationships. The pH and pCO₂ of the soil solution controlled the DIC fluxes according to carbonate equilibrium reactions. An increased exchange between DIC and atmospheric air was observed for samples from non-carbonate subsoils (IG and FGS). In addition, higher δ¹³C_DIC values up to ?19.4?‰ in the shallow soil water were recorded during the summer as a consequence of isotopic fractionation induced by molecular diffusion of soil CO₂. The δ¹³C_DIC values also suggest that half of the DIC derives from soil CO₂ indicating that 2 to 5 mol m^?2 year^?1 of carbon is lost in the form of dissolved inorganic carbon at CC and CD after carbonate dissolution.

Conclusions

Major difference in soil carbon dynamics between the four forest ecosystems is a result of the combined influence of bedrock geology, soil texture, and the sources of SOM. Water flux was a critical parameter in quantifying carbon depletion rates in dissolved organic and inorganic carbon forms.

     

黄河流域陕西片土壤侵蚀预报模型研究

以气候、地质、地形、植被及人类活动 5类因素中的 6个因子为预报因子 ,以陕西黄河流域水蚀区内 5大类型区中 3 3条小流域的实验观测资料和实地调查资料及有关科研单位的研究成果为基础 ,建立了适用于该区域的土壤侵蚀预报模型。据运用该模型对本区域内 4条小流域水土保持遥感普查成果和建模所用 3 3条小流域土壤侵蚀模数进行验证 ,证明该模型具有较高的精度 ,可以在陕西黄河流域水蚀区及条件相近的其他地区推广应用     

蒸煮爆破处理过程中毛竹材加工剩余物主要化学成分的变化研究

采用硫酸水解法(aldito-acetate procedure)、X射线粉末衍射(XRD)、傅里叶变换红外光谱(FTIR)分析了蒸爆过程中毛竹材加工剩余物纤维聚集态结构及主要化学成分的变化.研究结果表明,(1)毛竹材加工剩余物经蒸爆处理,60%左右的半纤维素水解,木质素低分子化且裸露到纤维表面,易被80%乙醇及木质素溶剂提取,从而实现毛竹材加工剩余物主要组分的有效分离.(2)毛竹材加工剩余物经蒸爆处理,80%乙醇抽提物得率提高,综纤维素得率减少,木质素含量减少:葡萄糖相对含量增加,半纤维素降解明显.(3)210℃处理10 min和220℃处理10 min的蒸爆浆的化学组成变化几乎没有区别,但两者与200℃处理10 min差别较大,210℃处理10 min是毛竹材加工剩余物适宜的处理温度.(4)FTIR结果显示蒸爆处理后在1040～1060 cm-1区的吸收峰分裂为明显的2个峰表明半纤维素降解,1166 cm-1处的吸收强度明显减弱,表明C-O-C键有不同程度的断裂.X-身寸线衍射分析结果显示毛竹材加工剩余物蒸爆处理后纤维素相对结晶度增加.     

基于反射光谱的山核桃幼苗氮素营养状况分析

山核桃(Carya cathayensis)是世界著名的干果之一,也是重要的木本油料作物,其油味清香、营养丰富,是优良的休闲保健食品.山核桃长期以来产量不稳、大小年现象明显,通过肥水管理、病虫害防治等有效管理措施,大部分产区大小年现象都明显趋缓,产量逐年上升(黎章矩,2003).我国山核桃研究起步较晚,在其营养方面的研究甚少.