统筹城乡背景下农机社会化服务的现状与实践—以成渝经济区为例

农机社会化服务是推动农业机械化发展的有效方式,新时期成渝经济区在统筹城乡社会经济发展背景下农机社会化服务正在进行着多元化的实践。为此,通过实证研究,分析了成渝经济区农机社会化服务的现状及作用,探讨了农机社会化服务与统筹城乡发展二者之间双向互动支撑的发展态势。同时,提出了促进成渝经济区农机社会化服务的针对性建议。     

太原经济技术开发区用地效益评价

通过对太原经济技术开发区的实际调查和对2002—2011年10 a间的相关统计及国家商务部历年发布的国家级经济技术开发区发展报告的信息进行分析,从开发区土地利用现状、年度建设用地供给、科工贸收入、工业总产值、GDP、税收收入、国内外资金利用等方面,综合评价了太原经济技术开发区的经济效益和用地效益。结果表明,该区独立运行10 a来成绩显著,整体效益逐步提高,在山西所有开发区中经济效益名列前茅,在全省经济技术开发区中每年的综合评价都名列第1;与国内中西部或中部的同类开发区相比,该区经济总量和单位面积产生的效益排名中后;与国内先进经济技术开发区相比,差距较大;该区内部分企业规模大、影响广泛,经济效益和用地效益均好,起到了带头和示范作用,但仍有部分企业规模小、投入水平低、建设周期长、产生效益低,影响了全区整体效益的发挥。建议开发区管委会引导入区企业加大投入,加快建设步伐,及早产生经济效益;尽快实施扩区计划,保证经济快速、健康发展;落实土地供给和退出政策,使有限的土地发挥更大的效益。     

A survey on the use of rugs in Australian horses

The practice of horse rugging has important implications for horse welfare and performance, but in Australia, rugging practices have not been properly documented. The objective of this study was to obtain an understanding of Australian horse rugging practices. An online survey reviewed the management of 2659 Australian horses over 12 months. Of the reported horses a total of 84.8% were rugged, although most owners (69.5%) indicated that they were unsure whether horses needed to be rugged at all. Rugging was felt by 59.8% of owners to be a requirement for horses in competition. Riding and competition were significantly associated with the use of rugs. Nearly all respondents (89.0%) felt that ‘over-rugging’ was a concern. However, 4.8% of owners would use up to 4 rugs at any one time on their horse and 21.4% of horses were still rugged in temperatures above 20°C in Australia. Many Australian horse owners (42.8%) also believe that horses feel cold if they are not rugged. Anthropomorphism when it comes to rugging horses cannot be justified as the horse has a much wider thermoneutral zone (TNZ) than humans. Australian climate, owner opinions, equestrian discipline and whether a horse is used for riding influence Australian horse rugging practices. However, current practices are based on limited available research and are not necessarily to the benefit of the horse. The major limitation was that the survey likely attracted respondents who are interested in the topic creating a self-selection bias.     

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

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.     

使用迭代重加权最小二乘法求解平面度误差

提出了几何误差评定的迭代重加权最小二乘（IRLS-Iterative Reweighted Least Squares)算法。该算法采用一个迭代过程求解一系列加权最小二乘问题，并在每一步迭代中按照一定的规则对权系数进行调整，使其逐步逼近最优拉格朗日乘子。对于用CMM(坐标测量机)和其他设备得到的数据，可得到平面度误差的精确值。     

农田优化灌溉动态管理基本程序与方法研究

从土壤———作物———大气连续体角度出发 ,利用田间试验资料和气象资料 ,分析了影响优化灌溉方案制定的有关因子 ,确定出春小麦、春玉米不同生长阶段土壤水分控制下限标准 ;在土壤水分平衡理论的基础上 ,建立了时域滚动预报灌溉日期的方法 ;并以春小麦、春玉米农田为例进行了检验 ,结果比较理想     

基于土地利用结构的河流岸带生态系统服务簇识别

河流岸带生态系统服务功能的有效发挥是河流生态系统稳定且健康的重要保障之一。为识别河流岸带土地利用与生态服务价值的空间结构,本文从河流岸带保护角度选取水资源保护、净化环境、水文调节、土壤保持、维持养分循环、生物多样性六项生态服务功能,基于遥感影像解译的土地利用数据,运用修正的当量因子法估算得到生态服务价值的空间分布规律,进而进行层次聚类分析识别河流岸带生态服务簇,并应用于太湖流域湖西区溧阳市县级河流——竹箦河作为实例研究。结果表明：（1）竹箦河河流岸带六项生态服务价值呈现出显著的空间异质性和聚集性。（2）竹箦河河流岸带可划分为五大类生态服务簇,分别为水源涵养型、绿色多元型、经济生态型、生态脆弱型以及耗水污染型。（3）各类服务簇的生态系统服务特点与空间布局分异明显,与岸带实际土地利用结构相协调,揭示了竹箦河河流岸带生态服务功能普遍较薄弱的现状。本文的研究结果可为竹箦河及类似平原地区骨干河流岸带功能区划分以及河流岸带生态保护与修复方案的制定提供理论参考。     

层状非均质包气带渗透性特征及其对降水入渗的影响

不同的岩性界面影响了降水在包气带中的入渗、运移与再分布过程,其影响机制仍是有待研究的学科前沿问题。针对上述问题,基于层状非均质包气带6 m×4 m×5 m样方,开展了多场次自然降水入渗过程的原位试验监测,研究结果表明层状非均质结构对降水入渗过程和速率影响明显:(1)地层分界面处土壤含水率呈现陡降变化特征;(2)220 cm深度以上包气带中土壤含水率对降水入渗响应变化敏感,呈含水率陡变的多峰谷式脉冲响应变化特征,其中20～100 cm地层土壤含水率变化幅度为22.58%～29.76%,120～200 cm地层土壤含水率变化幅度为13.74%～20.74%;220 cm深度以下包气带中土壤含水率对降水入渗响应滞缓,年内呈现平缓单峰响应变化特征,反映了多场次降雨的累积效应,其中220～400 cm地层土壤含水率变化幅度为2.3%～12.15%,430～460 cm地层土壤含水率变化幅度为2.5%～3.41%;(3)层状非均质结构阻滞了水分的运移(湿润锋通过亚砂土-粉砂界面时,平均运移速度由10.53 cm·d~(-1)下降为0.77 cm·d~(-1);湿润锋通过亚砂土-亚粘土界面时,平均运移速度由12 cm·d~(-1)下降为1.86 cm·d~(-1)),当岩性界面处水分不断蓄积克服阻力后才能向下运移;受上部界面水分蓄积的影响,下部层状非均质结构的阻滞作用将被减弱甚至不明显。