Realizing 3 Layers Transport Model in the Communication Between Embedded System and PC     

CHEN Hua-hong  PANG Tao  ZHOU Sha 《保鲜与加工》2005,(3):65-68

This article puts forward a 3 Layers Model for the communication between embedded system and PC. It is based on the speciality of them and the TCP/IP model. The model defines the communicate process of embedded system to be three layers: Transport Layer, Control Layer and Application Layer. Each layer serves for its higher-up. It can keep the efficiency and credibility of the communicate process and the authors prove and analyse that in the article. the concept of the model is also suitable for Bluetooth, IrDA and other kinds of communication about embedded system.  相似文献   

A STUDY ON HEAT AND MOISTURE STATE OF HULL LAYER FOR THERMAL INSTULATION OF A COLD STORAGE     

Chen Qigao Feng Ya 《保鲜与加工》1993,(1)

This paper analyses the thermal moist characteristics of the hull layer beside an air layer at lower temperature in an envelope for a cold storage and presents a new method of waterproof by air layer. With test data from engineering practice, the theory on the barrier of self moisture proof at the surface sublayer of the hull layer in an attic on a cold storage is proven. The dried zone about three phase point is confirmed. It is a new knowledge for thermophysics on thermal design of a cold storage with an optimum thermal performance.  相似文献   

紫坪铺水利枢纽引水系统取消厂前伸缩节研究   总被引：3，自引：0，他引：3  

申艳  伍鹤皋  蒋逵超  郭志兵  杨志宏 《中国农村水利水电》2004,(6):72-74

结合紫坪铺水利枢纽工程的实际情况，采用三维有限元方法对该工程发电引水系统取消伸缩节的可行性进行了研究。计算结果表明，主厂房上游永久分缝处以一段垫层管代替常规伸缩节，结构位移和应力完全可以满足使用要求，从而达到了取消伸缩节、节省工程投资的目的。  相似文献   

新疆夏季行星边界层参数化方案模拟特征研究     

张海亮  李火青  买买提艾力·买买提依明 《干旱区研究》2021,38(1):154-162

行星边界层参数化方案(PBL)对天气气候和大气环境的模拟与预报具有重要影响.通过基于单柱模式(SCM)的乌鲁木齐单点理想实验,以及新疆2019年8月15—18日的一次降水天气过程的模拟检验及诊断分析,研究了YSU、ACM2、BOULAC、GBM、MYJ和QNSE 6种常用的PBL参数化方案模拟的大气比湿、位温等气象要素...  相似文献   

Soil bacterial characteristics between surface and subsurface soils along a precipitation gradient in the Alxa Desert,China     

TENG Zeyu  XIAO Shengchun  CHEN Xiaohong  HAN Chao 《干旱区科学》2021,13(3):257-273

Bacteria in desert soil have unique phylogeny and important ecological functions, and theirresponses to changes in precipitation need further attention. However, relevant studies have mainlyfocused on the surface soil, and studies on the responses of bacteria at different soil depths to variationsin precipitation are rare. Thus, we used 16S rDNA high-throughput sequencing to investigate the changesin soil bacterial distribution along a mean annual precipitation gradient (50–150 mm) in the Alxa Desert,China, and compared the variation characteristics in the surface soil layer (0–10 cm) and subsurface soillayer (10–20 cm). Results showed that soil bacterial communities significantly changed along theprecipitation gradient in both soil layers. However, the subsurface soil layer could support bacterialcommunities with higher diversity and closer internal relationships but more internal competition than thesurface soil layer. Additionally, compared with the surface soil layer, variations in diversity andco-occurrence patterns in the subsurface soil layer were more in line with the changes in the mean annualprecipitation, while bacterial community structure was less variable in the subsurface soil layer. Comparedwith the mean annual precipitation, soil moisture had little influence on the structure and diversity of soilbacterial community but had a high correlation with intercommunity connectivity. Therefore, soilmoisture might play a complex role in mediating environmental conditions and soil bacterial communitycharacteristics. Due to the different responses of surface and subsurface soil bacteria to the changes inprecipitation, it is necessary to distinguish different soil layers when predicting the trends in desert soilbacterial conditions associated with precipitation, and prediction of subsurface soil bacteria may be moreaccurate.  相似文献   

区域尺度喀斯特区石漠化强度对土壤流失的影响     

李瑞  袁江 《农业工程学报》2022,38(15):84-92

石漠化和水土流失是西南喀斯特区突出的生态问题,制约着社会经济的发展。目前,石漠化与土壤流失的耦合关系尚未系统探明,石漠化强度评价因子植被盖度、土层厚度和基岩裸露率的交互作用如何影响土壤流失知之甚少。基于石漠化现状的调查,采用RUSLE模型、Getis-OrdGi*、地理探测器等方法,测算了贵州喀斯特区土壤侵蚀状况并识别了冷热区分布,量化了石漠化强度评价因子与土壤侵蚀之间的关系,解析了因子组合对土壤流失的交互影响。结果表明：1)贵州喀斯特区土壤侵蚀以中度和微度侵蚀为主,平均土壤流失率17.69t/(hm²·a),侵蚀热区(重点防治区)主要集中在贵州西部经济相对欠发达区,侵蚀冷区(轻微区)则主要集中在黔北遵义市和黔中贵阳市等经济相对发达区。2)土壤流失随石漠化强度评价指标植被盖度、土层厚度的增加呈降低趋势,随基岩裸露率的增加则呈增加趋势;石漠化与土壤流失之间并非简单的线性关系,而呈复杂的非线性关系,3个评价因子分别以三次曲线函数、指数函数和反正弦函数拟合优度最高。3)石漠化强度评价因子对土壤流失空间分异的解释力依次为植被盖度、基岩裸露率和土层厚度,且因子组合对土壤流失...  相似文献   

黄淮海旱作区土壤压实度空间分布特征及其影响因素   总被引：2，自引：2，他引：0  

李勇  赵云泽  勾宇轩  黄元仿 《农业工程学报》2021,37(13):83-91

为探究旱作区农田不同层次土壤压实度特征,基于2017年采集的255个土壤样品,运用Mann-Kendall突变检验法、地统计学和冗余分析等方法,探究黄淮海旱作区耕作层和压实层空间分布特征,分析不同层次的土壤压实度的空间变异特性及影响因素,并提出了最佳土壤压实度范围。研究结果表明:旱作区耕作层和压实层厚度均呈现由北向南递增的趋势,耕作层最大厚度可达22.50 cm,最低仅有10.21 cm;压实层厚度最大可达17.50 cm,最小值也达到7.50 cm。从不同层次来看,耕作层和压实层的压实度具有空间分布一致性,耕作层压实度高值区主要分布在河南省东部、安徽北部及河北北部地区,最大值可达87.68%以上,低值区则主要集中在山东西北部以及河北南部地区。和压实层压实度相比,耕作层压实度是影响粮食产量的主要因素,且在70%～80%时获得较高产量。分析表明,土壤压实度受到年降水量、平均气温、土壤自然属性等环境因子和机械耕作等人为因素综合作用的影响。研究结果可为黄淮海农田土壤压实情况的改善及管理措施的科学制定提供理论支撑。  相似文献   

河南省主要土壤耕层有效养分含量分析   总被引：4，自引：0，他引：4  

陈翠玲  张玉兰  蒋爱凤  胡喜巧  陈丽敏  陈维新  兰和平  吴生良 《河南农业科学》2007,(2):60-62

对河南省主要土壤耕层21个样区的土样有效养分含量进行测定分析,结果表明:河南省主要土壤耕层的有机质含量稍缺;有效氮含量中等;有效磷含量稍丰;有效钾含量丰富;有效铜含量丰富;有效锌含量缺乏。  相似文献   

气力式1JH-2型秸秆深埋还田机设计与试验     

田阳  林静  李宝筏  张桐嘉  齐林  王佳琦 《农业工程学报》2018,34(14):10-18

针对东北黑土区合理耕层构建秸秆深埋还田的技术要求,实现虚实并存合理耕层结构,研制了气力式1JH-2型秸秆深埋还田机,能够一次完成破茬、秸秆捡拾粉碎、开沟碎土、行间深松、秸秆深埋、覆土镇压等功能。机具主要由传动系统、破茬装置、捡拾粉碎装置、气力输送装置、开沟装置、覆土装置、镇压装置等组成。其关键部件是气力输送装置,应用离散元气固耦合数值模拟法对秸秆在气力气力输送装置中不同转速下的运动过程进行了数值模拟研究,得到了秸秆和气流输送气固耦合的运动规律。正交试验结果表明,机具运行最优参数组合为开沟装置转速215 r/min,风机转速1 850 r/min,机具作业速度3.0 km/h。田间试验表明,在最优参数组合条件下,秸秆深埋率为94%,秸秆粉碎合格率为94.2%,碎土率为95.4%,满足了东北黑土区秸秆深埋还田技术指标要求,为秸秆深埋还田机的改制和评价提供参考。  相似文献   

Desiccation and cracking behaviour of clay layer from slurry state under wetting-drying cycles   总被引：3，自引：0，他引：3  

Chao-Sheng Tang  Yu-Jun Cui 《Geoderma》2011,166(1):111-118

Laboratory tests were conducted to investigate the effect of wetting-drying (W-D) cycles on the initiation and evolution of cracks in clay layer. Four identical slurry specimens were prepared and subjected to five subsequent W-D cycles. The water evaporation, surface cracks evolution and structure evolution during the W-D cycles were monitored. The effect of W-D cycles on the geometric characteristics of crack patterns was analyzed by image processing. The results show that the desiccation and cracking behaviour was significantly affected by the applied W-D cycles: the measured cracking water content θ_c, surface crack ratio R_sc and final thickness h_f of the specimen increased significantly in the first three W-D cycles and then tended to reach equilibrium; the formed crack patterns after the second W-D cycle were more irregular than that after the first W-D cycle; the increase of surface cracks was accompanied by the decrease of pore volume shrinkage during drying. In addition, it was found that the applied W-D cycles resulted in significant rearrangement of specimen structure: the initially homogeneous and non-aggregated structure was converted to a clear aggregated-structure with obvious inter-aggregate pores after the second W-D cycle; the specimen volume generally increased with increasing cycles due to the aggregation and increased porosity. The image analysis results show that the geometric characteristics of crack pattern were significantly influenced by the W-D cycles, but this influence was reduced after the third cycle. This is consistent with the observations over the experiment, and indicates that the image processing can be used for quantitatively analyzing the W-D cycle dependence of clay desiccation cracking behaviour.  相似文献