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141.
Bravo Carlo Millo Christian Covelli Stefano Contin Marco De Nobili Maria 《Journal of Soils and Sediments》2020,20(2):1074-1086
Journal of Soils and Sediments - Humic acids (HA) have several environmental roles, but are particularly important in aquatic environments, being recognized as redox active natural organic matter... 相似文献
142.
基于随机森林算法和气象因子的砀山酥梨始花期预报 总被引:5,自引:4,他引:1
准确预报始花期是制定砀山酥梨花期管理措施和赏花活动方案的重要基础。该文利用1983-2018年砀山酥梨始花期的定位观测物候数据和平行观测的气象资料,采用线性趋势法,揭示始花期演变趋势;采用相关分析,筛选影响始花期的关键气象因子,依据不同预报日期构成特征变量集;采用随机森林算法(Random Forest, RF),自3月11日开始预报到3月25日终止预报,每日训练1个预报模型。结果表明,1)1983-2018年始花期呈极显著提早发生趋势,每10a约提前2.750 d(P<0.001)。2)16个逐日气象预报模型中,共计有200个气象因子与始花期早迟密切相关,相关系数在0.469~0.789之间;各气象预报模型的训练集与测试集的平均正确率(Nd)分别为92.9%和75.5%、平均均方根误差(RMSE)分别为1.693~2.870和2.240~7.237、平均决定系数(R2)分别为0.891和0.701。3)2019年试验预报中,提前15日准确预报出当年始花期。该文研究表明RF在梨树始花期逐日气象预报中有一定业务应用潜力,预报准确率基本满足气象服务需求。 相似文献
143.
浙江省商品有机肥中重金属含量变化趋势及风险管控对策 总被引:3,自引:1,他引:2
144.
D. P. De Vries 《Euphytica》1965,14(1):78-82
In 9–13 year old cherry seedling populations, totalling 1,033 individuals, a preliminary selection was made in 1963, for field resistance to bacterial canker (Pseudomonas syringae
van Hall).The field resistance of the three cherry species used, P. avium, P. cerasus and P. avium × P. cerasus, has shown to be low, high and very high, respectively. 相似文献
145.
H H Chang J W De Vries W E Hobbs 《Journal of the Association of Official Analytical Chemists》1979,62(6):1281-1284
The difference between the CB and Best Foods methods in extracting aflatoxins from peanut products has been studied. The CB method yields 60, 121, 35, and 22% higher results for aflatoxins B1, B2, G1, and G2, respectively for 4 samples of peanut meal and 6 samples of peanut butter studied. Both reverse phase liquid chromatography and thin layer chromatography were used to quantitate the extracted aflatoxins. 相似文献
146.
The chemistry of humic and fulvic acids extracted from argentine soils—I. Analytical characteristics
Five humic and three fulvic acids were extracted from Argentine Chestnut, Brunizem, Solod and Solonetz soils and analysed by electrometric, spectroscopic and spectrometric methods. There were great similarities in elementary analysis, functional group content, absorption characteristics in the visible region and in the IR, and in the ESR measurements between the humic acids and, similarly, between the fulvic acids. There were distinct differences between the humic and fulvic acids in C, H, N and O content, distribution of oxygen in functional groups, E4/E6 ratios and free radical content. 相似文献
147.
F. De Coninck 《Geoderma》1980,24(2):101-128
Current explanations of the formation of spodic horizons do not accomodate all features of the horizons in their natural state. In this paper, a more complete explanation of major mechanisms is proposed, using two principles of colloid chemistry: (1) organic substances may form hydrophylic colloids with surface charges, and (2) the hydrophylic character and negative surface charges determine the dispersibility of the colloids. The hydrophylic character is due to the presence of hydrophylic radicals as parts of the organic compounds in soils. The surface charges are the result of dissociation of -COOH and possibly phenol-OH radicals.The neutralization of the surface charge can in principle occur: (1) through electrostatic or physical adsorption and (2) through chemisorption. The first case is typical for monovalent alkali cations. The adsorbed cations are distributed in a double layer, which favours dispersion. Chemisorption occurs mostly with polyvalent cations. This process corresponds in reality to the formation of organo-metallic compounds. It results in a relatively complete disappearance of the double layer and in the formation of large immobile “polymerized” organo-metallic compounds. Because these compounds contain much hydrophylic water, they form a gel. Transition into the solid state is accompanied by the loss of most of the hydration water. The dehydration may be induced by a decrease in thickness of the double layer. At a certain stage of the dehydration process, Van der Waals bonds and protonic bridges can form and bring about a certain degree of hydrophoby.In soils, mobile organic substances are formed during breakdown of plant remains. If at the top of the mineral soil enough polyvalent cations, especially Al and Fe, are available, the mobile organic substances formed are immobilized immediately and no migration occurs. In case insufficient amounts of Al and/or Fe are available to completely immobilize the mobile compounds, these cations are complexed by the mobile compounds and transported downward. Immobilization may occur at some depth through supplementary fixation of cations, through dessication or on arrival at a level with different ionic concentration.In nature, spodic horizons range from loose, with many roots, to very cemented with few roots. These differences can be related to changes in microstructure. Loose spodic horizons have a predominance of polymorphic pellets and aggregates, whereas organans or monomorphic coatings prevail in cemented horizons. The former horizons have many features suggesting major biological influences during their formation, viz., high numbers of roots, thorough mixing of the organic units with clay and silt, the presence of pedotubules and relatively young mean residence times. The latter horizons have features consistent with organo-metallic compounds immobilized in a gel-state, viz., the coatings are strongly cracked, indicating the transition of a gel into a solid; they contain much Al or Al plus Fe but very little or no Si, and the mean residence time is considerably higher than in loose horizons.The two processes seem to operate simultaneously during the formation of spodic horizons and their relative intensities determine the composition of each spodic horizon at any moment in its evolution. As long as the biological activity predominates, the horizon remains loose; if the accumulation of mobile organo-metallic compounds starts to prevail, the horizon is gradually cemented and fossilized. 相似文献
148.
149.
盐碱胁迫下绒毛白蜡种子的萌发特性 总被引:5,自引:0,他引:5
将中性盐NaC l,Na2SO4和2种碱性盐NaHCO3,Na2CO3按不同比例混合,模拟出20种盐度、碱度各不相同的复杂盐碱逆境条件,进行绒毛白蜡种子发芽试验。测定其发芽率等6项指标,结果表明:在混合盐碱的胁迫作用下,绒毛白蜡种子的发芽受到明显的抑制,发芽率、发芽势、发芽指数、活力指数等指标呈下降趋势,并随盐碱度递增,下降趋势变大,高盐高碱的共同作用结果远远大于单纯的高盐或高碱,SOD的活性总体上有不同程度的增加,CAT在不同处理组间均呈现上升的趋势,在50,100mmol/L的组内呈上升趋势,但在200,300mmol/L组内则是先升后降。可见盐胁迫与碱胁迫是2种完全不同的胁迫,应将碱性盐胁迫称为碱胁迫,而通常所说的盐胁迫应仅指中性盐胁迫,而且两者具有明显的协同作用。 相似文献
150.