基于局部建模方法的卧式柔性清土辊性能优化     

牛丛  徐丽明  闫成功  谭好超  沈聪聪  马帅 《农业工程学报》2023,39(1):50-59

针对基于整体建模的卧式柔性清土辊性能优化方法存在仿真成本高的问题,该研究提出一种局部预测整体的建模方法,既降低仿真计算量,同时可以对柔性清土辊进行优化设计。首先,提取柔性清土辊的最小结构特征,并基于几何相似性原理构建整体性能预测模型。其次,基于离散元法（Discreteelementmethod,DEM）与多柔性体动力学（multi-flexible-bodydynamics,MFBD）耦合仿真技术优化求解最小特征结构的最优作业性能。最后,依据预测模型估算柔性清土辊的整体性能。柔性清土辊的清土率和阻力矩与其刷片数量的线性拟合决定系数分别为0.987和0.99。基于局部建模方法和EDEM-RecurDyn耦合技术建立最小特征结构与土壤互作模型,其接触计算量仅为整体建模方法的8%左右。前进速度、安装角、轴向长度和叶片锥角对最小特征结构和刷片的作业性能影响显著,仿真优化结果分别为0.3 m/s、30°、50 mm和0°。上述条件下最小特征结构的清土率和阻力矩为36.87%、18.91 N·m,单个刷片的清土率和阻力矩为2.80%和2.78 N·m,最小特征结构的物理试验结果与仿真结果的相对误...  相似文献   

Adsorption and Transformation Reactions of L-DOPA in Soils     

《Soil Science and Plant Nutrition》2013,59(6):819-825

3-(3′,4′-Dihydroxyphenyl)-L-alanine (L-DOPA), which is a component of velvetbean (Mucuna pruriens), displays a high inhibitory activity to plant growth. The inhibitory activity is influenced by the presence of soils, because L-DOPA is eliminated in soils. In the present study, the effect of several soil types (volcanic ash, calcareous, and alluvial soils) on the L-DOPA disappearance was investigated at constant equilibrium pH values. In the presence of soils, L-DOPA disappeared with the reaction time, and the disappearance was associated with three reactions: adsorption reaction (characterized by fast and sudden disappearance of L-DOPA within the initial 8 h period), catalytic transformation reaction (constant L-DOPA disappearance throughout the reaction period), and biotransformation caused by microbial activity (accelerated L-DOPA disappearance observed after 72 h of reaction time). The adsorption and transformation reactions consisted of physicochemical reactions mediated by the presence of soils. The amount of L-DOPA adsorbed was largest in the presence of volcanic ash soil among the three soil types. It is likely that the mechanism of L-DOPA adsorption includes a ligand exchange reaction. In the presence of soils, L-DOPA transformation was observed at equilibrium pH values higher than 4 and it increased with increasing equilibrium pH values. In the absence of soil, however, L-DOPA transformation did not occur at an equilibrium pH value lower than 6.0, indicating that L-DOPA transformation was accelerated by the presence of soil. The rate of L-DOPA transformation mediated by soils at constant equilibrium pH value was in the following order: alluvial soil > calcareous soil > volcanic ash soil. The plant-growth-inhibitory activity of L-DOPA was also reduced by the presence of soils, and the reduction in the case of L-DOPA was more obvious than in the case of 2,4-dichlorophenoxyacetic acid (2,4-D). Based on the reduction effect of soils on the plant-growth-inhibitory activity of L-DOPA (without pH-adjustment), calcareous soil ranked first, followed by volcanic ash soil, then alluvial soil. This was because the calcareous soil showed the highest soil pH value (7.8), and thereby the L-DOPA transformation reaction was accelerated. In soils with high pH values, the plant-growth-inhibitory activity of L-DOPA could therefore not be detected.  相似文献   

Zinc Nutrition in ‘Nagpur’ Mandarin on Haplustert     

A. K. Srivastava  Shyam Singh 《Journal of plant nutrition》2013,36(7):1065-1081

ABSTRACT

Zinc (Zn) deficiency is the most prevalent nutritional disorder in citrus orchards world over. The management strategy of Zn deficiency today is still governed by the efficacy of two conventionally used methods of Zn supply to plants via soil or foliar fertilization. A field experiment with 12-yr-old ‘Nagpur’ mandarin (Citrus reticulata Blanco) orchard was, therefore, carried out during 2004–07 comparing soil application versus foliar application of Zn, each at three levels viz., 100, 200, and 300 g tree^?1 with constant doses of N (600 g tree^?1), P (200 g tree^?1), K (300 g tree^?1), and Fe(60 g tree^?1) on Haplustert soil type with reference to response on flowering intensity, fruit set, tree volume, fruit yield, changes in soil fertility/leaf nutrient status, fruit quality, and transformation of native soil Zn fractions. Soil application of Zn at all the three levels, produced significantly higher increase in tree volume over foliar application on equivalent rates viz., T₁ (2.53 m³) vs. T₄ (2.06 m³) and T₂(4.30 m³) vs. T₅ (2.23 m³). The yield-determining parameters like flowering and fruit set intensity (no. m^?1 shoot length) were, respectively, much higher with soil applied (135.74 and 21.90) than foliar applied Zn (31.20 and 11.6). These observations set the favorable conditions required for yield response, e.g., all the three treatments involving soil application of Zn, T₁ (32.1 kg tree^?1), T₂ (52.6 kg tree^?1), and T₃ (51.8 kg tree^?1) were correspondingly superior over T₄ (22.5 kg tree^?1), T₅ (34.3 kg tree^?1), and T₆ (42.1 kg tree^?1) as foliar application treatments. All the three major fruit quality parameters (juice, acidity, and TSS) were likewise more influenced by soil application than foliar application of Zn. Improvements in soil Zn fractions (mg kg^?1) viz., exchangeable Zn (0.25–0.60), complex-Zn (2.71 to 4.86), organically bound Zn (0.86 to 2.0), and Zn-bound to carbonates and acid soluble minerals (2.56–4.96) were observed in response to Zn fertilization with treatments T₁–T_3. On the other hand, foliar applied Zn treatments (T₄–T₆) produced no such changes in any of the soil Zn fractions.  相似文献   

A short discussion on the chemical composition of allophane based on the data of Yoshinaga in 1966     

Yasuo Kitagawa 《Soil Science and Plant Nutrition》2013,59(4):321-324

Many scientists have attempted to discern the chemical composition and the structure of allophane (2, 4–6). Yoshinaga (7) presented the chemical composition of eighteen samples of pure allophane in detail, and concluded as follows: All samples consisted principally of silica, alumina, and water. The silica-alumina molecular ratio ranged from about 1.3 to 2. Molecular ratios of ignition loss (+H₂0) and total water (±H₂O) to alumina were nearly constant, with the averages about 2.5 and 5.7, respectively. The chemical composition of soil allophane fell into a relatively narrow range, and the change in the percentage composition of the three major elements had a regularity.  相似文献   

The oxidation products formed from: Soil organic matter by hydrogen peroxide treatment     

Yasuo Harada  Akio Inoko 《Soil Science and Plant Nutrition》2013,59(4):513-521

The oxidation products formed from soil organic matter during hydrogen peroxide digestion were studied by means of analyses of carbon and nitrogen, thin layer chromatography, infrared Spectroscopy, and redox titration.

The carbon remaining after hydrogen peroxide digestion, as expressed in percentage by WeIght of the original soil was 0.57 to 4.09, corresponding to 17.81 to 29.00 per cent of the carbon fOUnd in the original soil. The nitrogen remaining after the same treatment was 75 to 100 per cent of total nitrogen in the original soil. The greater part of the remaining water soluble nItrogen was NH₃-N. The thin layer chromatography showed the presence of oxalic acid and V.V. light-ahsorbing substances in the oxidation products. No organic matter other than oxalate Was indicated on the infrared spectra. The amount of water soluble oxalate formed from 100 g of soil determined by means of redox titration was 5.7 to 117.0 mmole. Assuming that the ratio of solution: soil is 5:1 at the final stage of per oxidation, the concentration of oxalate in the SUpernatant solution was in the range from 0.011 to 0.234 M.  相似文献   

基于室内高光谱数据的多种类型土壤有机质估算模型比较     

郄欣  齐雁冰  刘姣姣  王珂  陈敏辉 《干旱地区农业研究》2021,39(4):109-116

基于高光谱数据的土壤有机质反演是土壤遥感及精准农业的重要研究内容,然而不同的光谱处理及建模方法使得模型的估算能力及精度差异明显,限制了模型之间的通用性。为了构建陕西省土壤有机质含量估算的最优模型,以陕西省9种主要土壤类型的216个土样的光谱反射曲线和土壤有机质含量为数据基础,将光谱反射曲线进行一阶微分d(R)、倒数对数log(1/R)、倒数对数一阶微分d[log(1/R)]和包络线去除N(R)4种变换,结合一元线性回归(SLR)、偏最小二乘回归(PLSR)和支持向量机回归(SVR)3种建模方法构建了不同的土壤有机质含量估算模型。结果显示:不同类型土壤的反射光谱曲线总体态势基本一致,吸收特征位置基本相同,且土壤有机质含量与光谱反射率呈负相关态势;基于d [log(1/R)]光谱变换构建的SVR估算模型精度最高,建模集和验证集的判断系数(R~2)分别为0.9210、0.8874,验证均方根误差(RMSE)为2.18,相对分析误差(RPD)达到2.8751,是估算陕西省土壤有机质含量的最优模型,PLSR次之,SLR最差。  相似文献   

Gross nitrogen transformations and N_2O emission sources in sandy loam and silt loam soils     

LANG Man 《干旱区科学》2021,13(5):487-499

The soil type is a key factor influencing N(nitrogen) cycling in soil; however, gross N transformations and N_2O emission sources are still poorly understood. In this study, a laboratory ~(15)N tracing experiment was carried out at 60% WHC(water holding capacity) and 25℃ to evaluate the gross N transformation rates and N_2O emission pathways in sandy loam and silt loam soils in a semi-arid region of Heilongjiang Province, China. The results showed that the gross rates of N mineralization, immobilization, and nitrification were 3.60, 1.90, and 5.63 mg N/(kg·d) in silt loam soil, respectively, which were 3.62, 4.26, and 3.13 times those in sandy loam soil, respectively. The ratios of the gross nitrification rate to the ammonium immobilization rate(n/ia) in sandy loam soil and silt loam soil were all higher than 1.00, whereas the n/ia in sandy loam soil(4.36) was significantly higher than that in silt loam soil(3.08). This result indicated that the ability of sandy loam soil to release and conserve the available N was relatively poor in comparison with silt loam soil, and the relatively strong nitrification rate compared to the immobilization rate may lead to N loss through NO_3~– leaching. Under aerobic conditions, both nitrification and denitrification made contributions to N_2O emissions. Nitrification was the dominant pathway leading to N_2O production in soils and was responsible for 82.0% of the total emitted N_2O in sandy loam soil, which was significantly higher than that in silt loam soil(71.7%). However, the average contribution of denitrification to total N_2O production in sandy loam soil was 17.9%, which was significantly lower than that in silt loam soil(28.3%). These results are valuable for developing reasonable fertilization management and proposing effective greenhouse gas mitigation strategies in different soil types in semiarid regions.  相似文献   

基于大学学术生产力提升的图书馆创新服务     

朱玉珍 《农业图书情报学刊》2014,(6):184-186

大学是科技成果的发源地,提升大学学术生产力是促进科技发展的重要途径。大学图书馆为促进大学学术生产力的提升,可在大学教学工作中的知识转移、科研工作中的知识创造和科研成果的知识转化三个环节提供信息服务。  相似文献   

提高农杆菌介导转化水稻效率的因素   总被引：11，自引：0，他引：11  

李双成  王世全  尹福强  邹良平  起登风  江洪  李平 《中国水稻科学》2005,19(3):231-237

 以3个籼稻品种和2个粳稻品种为对象，对农杆菌转化水稻过程中影响转化效率的因素进行了研究。结果表明，菌株AGL1和EHA105按一定比例混合共转化和转化前菌体重悬对抗性愈伤率有显著影响；琼脂粉加倍和超净工作台上风干4 h的方法因能明显提高抗性愈伤率和分化率而被认为是最适合的干燥培养方式；分化培养基中加入二甲基亚砜（DMSO）或脯氨酸（Pro）可以提高分化率；壮苗时加入适量的NAA有利于壮根并提高移栽成活率。应用此农杆菌转化系统，获得了一批经PCR和点杂交鉴定的转基因植株。  相似文献   

Factors Affecting Agrobacterium-Mediated Transformation Efficiency in Rice     

CHEN En-hui ZHANG Ping ZUO Shi-min LI Ai-hong ZHANG Ya-fang CHEN Zong-xiang PAN Xue-biao 《水稻科学》2004,11(2)

Several important factors affecting the efficiency of Agrobacterium-mediated rice transformation were studied with several predominant commercial indica and japonica rice cultivars. As far as indica rice callus was concerned, CC medium was the best and the quality of callus was improved with the addition of 1.0 to 2.0 mg/L ABA. It decreased the percentage of browning calli and improved the callus growing state by addition of a certain amount of sorbitol to the subculture medium. NB medium was the best for callus initiation of japonica rice, but the improvement in the quality of callus of japonica subspecies was not obvious by adding ABA. During the period of subculture, to a certain degree, increasing the sucrose concentration could improve the proportion of hygromycin resistant calli. Furthermore, the transformation efficiency would be higher by applying selection pressure in the selection stage, removing selection pressure during the plantlet differentiation period and applying selection pressure again during seedling hardening period. Besides, suitable combination of plant hormones was beneficial for callus differentiation. An efficient Agrobacterium-mediated rice transformation system had been established for several rice cultivars and a lot of transgenic rice plants had been obtained.  相似文献