东北老工业基地振兴中农村公共服务职能改革

中央做出的振兴东北地区等老工业基地的重大战略决策给东北地区等老工业基地中的农业和农村经济发展带来了很大机遇。改革东北地区等老工业基地中的政府农村公共服务体系,对夯实东北地区等老工业基地的产业发展基础和实现全面建设小康社会的目标具有重大的意义。     

基于GIS的绿色农产品基地适宜性评价

建立和完善绿色农产品基地适宜性评价方法,提高评价结果的实用性和准确性,是实现农产品安全的根本保障。研究依据基地认证者、规划者、生产者3种评价主体实际需求,分别引入污染潜在风险指标和经济状况指标,建立面向不同评价主体需求的多种主导因子评价指标体系,并借助GIS的空间分析方法进行定量评价,最后以北京大兴区为例进行了案例分析研究。结果表明,基地与工矿企业距离、与居民地距离等潜在污染风险对基地适宜性限制大,且不同评价主体下建立不同指标体系使评价更具针对性,利用GIS功能可提高效率,评价结果可视化程度好,具有很强的     

水资源开发利用状况综合评价方法研究

在简单评述主成分分析法、灰色关联分析法、层次分析法和物元分析法等综合评价方法的基础上,将这些方法应用于对我国重要粮食基地松辽流域的水资源利用现状的综合分析,不仅对松辽流域的水资源利用及粮食生产安全现状给出了综合评判,还根据评判结果,对比分析上述方法的适用范围和限制条件等,指出了相应的改进方向.     

专家控制技术在设施园艺中的应用

设施园艺环境有多因素、线性大、时间滞后和不确定性的特点。随着现代化控制技术的发展,专家控制技术可以取得较好的控制效果。为此,介绍了专家控制技术的基本概念和其在温室环境控制中的应用,并叙述了知识库、数据库和推理机的设计过程。     

基于耕地机犁体自由曲面的数控铣削加工

耕地机犁体曲面是空间任意的曲面。设计合理的犁体曲面,应采用CAD/CAM软件进行实体造型,曲面设计成高速梨曲面,既可以降低无效阻力,又能减轻犁的质量,增强曲面的光滑程度。为此,采用数控加工中心对耕地机犁体空间自由曲面进行铣削加工,选择不同的加工方式和合理的参数,对粗加工时间和精加工结果进行对比分析。结果表明:流线式粗加工和环绕等距式精加工组合有更高的加工效率和更好的质量,能使耕地机减少抛扔的能量消耗,提高耕地机零部件的加工效率。     

亚热带花岗岩地区土壤矿物风化过程中盐基离子的释放特征

矿物风化过程中盐基离子释放遵从一定的化学计量关系,这种化学计量关系一般只能通过模拟实验来获取。本研究采用pH 7.0的EDTA-乙酸铵溶液将土壤中的交换性盐基离子完全洗脱出来,然后用Batch方法模拟不同pH溶液淋溶洗脱盐基和未洗脱盐基土壤,旨在消除土壤中交换性盐基离子的影响后更为准确地判断土壤矿物风化的盐基离子释放特征。结果表明:未洗脱盐基土壤的淋出液pH由3.73±0.14逐渐上升到4.23±0.06,主要原因是淋溶液中有高浓度的NH_4~+;洗脱盐基土壤矿物风化后淋出液pH从7.39±0.02逐渐下降到5.39±0.17,主要是由于土壤中可风化矿物减少。土壤交换性盐基离子会改变盐基离子释放特征、释放总量:未洗脱盐基土壤经酸雨淋溶后,各盐基离子释放均呈现急速下降后逐渐平缓的趋势,洗脱盐基土壤矿物风化后,K~+及盐基离子释放总量呈波动上升趋势,且盐基离子释放总量比未洗脱盐基土壤低。土壤交换性盐基离子的存在还会改变淋出液中的盐基离子化学计量关系:未洗脱盐基土壤的K~+︰Ca~(2+)︰Mg~(2+)︰Na+化学计量关系为11︰13︰4︰1(当量比),而洗脱盐基土壤为7︰2︰2︰1。K~+是盐基离子中风化释放量最多的,大部分K~+来自于土壤中云母的风化。因此,只有利用洗脱盐基土壤的盐基离子释放量才能准确计算矿物风化速率并获得准确的化学计量关系。土壤矿物风化作用随着淋溶液酸度增大而增强,但模拟一年降雨量的情况下,p H 3.5、4.5和5.5三种不同p H溶液对矿物风化后盐基离子的释放在实验期间没有显著性影响,较长时间后的差异性有待观察。本研究表明,可以通过预洗脱盐基土壤然后模拟酸雨淋溶的方法,观察矿物风化特征,特别是盐基离子释放的化学计量特征。     

温室用轻型方钢管柱脚底板压力及其简化计算模型

为研究半刚性柱脚底板压力分布,以轻型方钢管柱脚底板为研究对象,首先利用数值模拟方法,考虑柱脚与混凝土基础间非线性静力接触效应,针对4种加劲肋布置方式、6种偏心矩,分别计算24个轻型方钢管柱脚模型的底板受力情况,得到了底板压力分布规律,在此基础上提出了三折线底板压力分布模型,给出了轻型方钢管柱脚底板压力简化计算模型,并确定了相应关键参数。将简化计算模型结果与数值模拟、基于Winkler弹性地基梁模型的解析解和三角形压力分布的底板压力计算结果相对比。结果表明:三角形压力分布计算得到的底板最大压力值位于底板端部,而数值模拟、解析解及该文简化计算模型得到的最大压力值均位于柱截面翼缘处,且三角形压力分布的底板压力最大值明显大于该文简化计算模型结果,简化计算模型计算的底板压力最大值与数值模拟结果较为接近,且二者与解析解底板压力分布曲线亦吻合良好(误差大约为10%)。研究成果为轻型方钢管柱脚设计提供了更为精确适用的计算方法。     

Deforestation effects on soil degradation and rehabilitation in western Nigeria. IV. Hydrology and water quality

Hydrological and water-quality measurements were made on a 44·3 ha watershed under forest cover and following deforestation and conversion to an agricultural land-use. Under secondary tropical rainforest, water yield ranged from 2·2 per cent to 3·1 per cent of annual rainfall. Deforestation of 7 per cent of the watershed area increased water yield to 7·0 per cent of annual rainfall. Baseflow increased with deforestation, and increased progressively with time after deforestation. It was 5·1 per cent of annual rainfall in 1979, 15·1 per cent in 1980, 16·4 per cent in 1981 and 17·9 per cent in 1982. In comparison, surface flow was 4·5 per cent in 1979 and 6·2 per cent in 1980, but decreased to 2·3 per cent in 1981 and 2·4 per cent in 1982. Total water yield following deforestation and conversion to agricultural land-use ranged from 9·6 per cent to 21·3 per cent of the annual rainfall received. The dry season flow decreased with time as the dry season progressed, but increased over the years following deforestation. Surface runoff during the rainy season depended on ground cover and soil quality. The extent and severity of soil degradation affected the dynamics of surface flow. Because of actively growing crops, plant nutrient concentrations in surface runoff were low. Forested lysimeters had higher seepage losses than cropped lysimeters, and the water-use efficiency was 1·9–3·6 kg ha⁻¹ mm⁻¹ for cowpeas compared with 6·1–11·0 kg ha⁻¹ mm⁻¹ for maize. The delivery ratio was high immediately after deforestation and decreased to a steady value of about 3·2 per cent within 7 years. The data show five distinct phases of soil degradation in relation to generation of surface runoff. © 1997 John Wiley & Sons, Ltd.     

地下灌排兼用系统中田间土基透水管的机理分析及其现场成型机研制

通过对现有地下灌溉系统的分析，论述了田间地下土基透水管灌溉、排水兼用的可行性及机理分析。在对国内外暗管施工机进行分类归纳的基础上，研制出土基透水管现场成型机，可现场一次完成土基管的成型、固壁、防渗、镶嵌渗水条等工序，初步对样机进行了田间试验，验证其结构合理性、经济性、并对土壤的破坏成型机理进行了分析     

Effects of enhanced supplies of nitrogen and sulphur on rhizosphere and soil chemistry in a Norway spruce stand in SW Sweden

Rhizophere and bulk soil chemistry were investigated in a Norway spruce stand in SW Sweden. The rhizosphere and bulk soil chemistry in water extracts in control plots (C) and plots repeatedly treated with ammonium sulphate (NS) were compared. Treatment regime was started in 1988. Cylindrical core samples of the LFH-layer and mineral soil layers were collected in 1992 and used for water extract analyses. Samples of soil from LFH-layer and mineral soil layers were taken in 1991 and 1993 for determination of CEC and base saturation. Soil pH and NH₄-N, NO₃-N and SO₄-S, Al, Ca, K and Mg concentrations in water extracts were measured for rhizosphere and bulk soils. The pH-values of bulk and rhizosphere soils in NS plots decreased compared with those in control plots, whereas concentrations of NH₄-N, NO₃-N, SO₄-S, base cations and Al in water extract increased. In both bulk and rhizosphere soils the concentration of NH₄-N was much higher than that of NO₃-N. A significant difference in the pH and Mg concentration of bulk and rhizosphere soil between the treated and control plots was found only in the 0–10 cm layer. For all layers, there was a significant difference in NH₄-N concentrations in the bulk and rhizosphere soil between the NS treatment and control plots. Concentrations of exchangeable base cations and the base saturation level in the LFH-layer decreased in the NS plots. The concentration of extractable SO₄-S increased in the NS plots. The NS treatment enhanced the amount of litter in L-layer, owing to increases in needle biomass and litterfall but led to losses of base cations, mainly K and Mg, from LFH-layer. It was concluded that the NS treatment displaced cations from exchangeable sites in the LFH-layer leading to higher concentrations of these elements in both rhizosphere and bulk soil.