磷肥和硒施用对稻米硒、钙、锌等营养累积的影响

研究了施用不同水平磷肥和硒对稻米中硒、钙、锌、镁、硫等人体必需营养吸收累积的影响。结果表明，适量施磷，降低米中硒含量；大量施磷，又促进硒在米中累积。施磷肥一般不利于钙和锌在稻米中累积，适量施磷增加稻米中镁、硫含量，而过量施用磷肥显著降低钙、锌、镁、硫等矿质营养的含量，影响稻米营养品质。适量施硒，一般提高稻米的矿质营养含量；过量施硒，特别在高磷水平下则降低矿质营养含量。     

磷肥中有效磷的示波滴定

根据Ｐｂ２＋能与ＰＯ＿４￣（３－）定量形成沉淀，过量的Ｐｂ２＋在ＮａＣｌＯ３－六次甲基四胺底液示波图上有敏锐切口的性质，报告了磷肥中有效磷含量测定的示波滴定新方法。该法与通用方法相比较，具有操作简便、测定快速、终点直观的优点。     

微量元素叶面肥料中硼的测定

研究了在 pH 6 .5乙酸铵缓冲溶液中 ,硼与 3 甲氧基 甲亚胺H的显色反应条件 ,最大吸收在 4 2 0nm处 ,摩尔吸光系数为 8.1× 10 3,硼含量在 0～ 10 μg/ 10ml范围内符合比耳定律。用于微量元素叶面肥料中硼的测定 ,获得了与国标法一致的结果     

Efficient production of nanoporous silicon carbide from rice husk at relatively low temperature

Nanoporous silicon carbide with a specific surface area of up to 186.45 m² g⁻¹ has been efficiently synthesized from waste rice husk using a magnesiothermic reduction at 950 °C as a key step. Throughout the entire process, the recovery rates of silicon, potassium and phosphorus from rice husk can reach 88.46, 91.5 and 65.5%, respectively. Turning rice husk waste into a real treasure, this promising method for producing porous SiC protects the environment and brings economic benefits.     

The impact of nitrogen fertilizers on degradation and leaching of chlorotoluron in soil

Abstract

This study presents the developed and applied methods for the determination of carbendazim in environmental samples originating from several field studies.

For water samples sample pretreatment consisted of a solid phase extraction (SPE) on cartridges packed with 200 mg SDB-1. In case of solid samples the performance of microwave assisted solvent extraction (MASE) and classical ultrasonic extraction with acetone-ethyl acetate were studied. The latter technique was selected because of the reduced time of manual operations. Instrumental analysis of extracts of water samples was performed on-line with coupled column reversed phase liquid chromatography (LC/LC) and UV detection (280 nm) allowing to assay carbendazim to a level of at least 0.1 μg/l. Improved column life time was obtained by performing the favorable LC separation of carbendazim at high pH on newly developed 5 μm Extend-pH bidentate C18 material.

The combination of a short column packed with 5 μm Inertsil ODS-5 and a mobile phase at low pH material was most adequate as the regards the robust and fast processing of extracts of solid samples and allowed in most cases the screening of carbendazim in soils and sediments to a level of 10μg/kg.

The developed procedures yield overall recoveries for carbendazim of 101, 80 and 71 % in water (levels, 0.1—1.2 μg/l: n=12), soil (levels, 10 and 100 μg/kg; n=22) and sediments (levels, 10 and 100 μg/kg; n=11), respectively, with a repeatability and reproducibility below 7 % for all method/matrix combinations. Soil samples with aged residues (level, 100 μg/kg; n=10) provided an overall recovery of 71% and no significant decrease of carbendazim was observed during nine weeks of storage in the refrigerator.     

New green process to increase the solubility of soil fertilizer based on Potassium Nitrate (KNO3)

Fertilization is the set of operations that consists of fertilizing the soil so that the plant finds all these mineral nutrition needs, among these nutrients is found potassium nitrate (KNO₃), as an important source of two elements which are nitrogen (N) and potassium (K). The need for potassium nitrate for plants will increase dramatically as its demand for nutrition growing up. However, the application of this potassium in fertilization is limited by a physicochemical parameter which is solubility. The availability of potassium and nitrogen in ionic form, which can be assimilated by the plant, is closely related to its solubility in irrigation water. Herein, we have chosen three experimental parameters such as the KNO₃ content, the magnetization time, and the type of water, to optimize the factors which have the maximum effect on KNO₃ solubility.We adopted a model from nine experiments performed with Minitab software, which informed us that the solubility of KNO₃ in irrigation water is strongly influenced by water type, magnetization time and KNO₃ content. The best conditions which allow the best solubility of potassium nitrate are 24% KNO₃, 30 ​min of water magnetization, and salt water (SW).     

基于傅里叶变换红外光声光谱的包膜控释肥料聚合物膜疏水性的表征

以不饱和有机硅改性的丙烯酸酯为基材,在不同条件下制备了30种水基聚合物包膜控释肥料模型膜,测定了模型膜的溶胀度及模型膜的傅里叶变换红外光声光谱.分别以红外光声光谱和溶胀度为自变量和因变量进行简单相关分析,同时也构建了偏最小二乘模型,并利用该模型对模型膜的疏水性进行预测.结果表明,聚合物模型膜具有明显不同的疏水性,其红外光声光谱具有相似的吸收特征,但不同吸收带的相对强度发生明显改变;常用的简单相关分析无法实现模型膜疏水性的预测,表明模型膜的疏水性与谱区更多的特征峰相关;基于偏最小二乘法的多元校正分析具有很好的预测能力,模型的校正系数(R2)为0.9864,校正标准误差为0.70%,验证标准误差为1.92%.此模型可用于模型膜疏水性的预测.本方法样品用量少,测定快速,操作简便且可实现原位测定,为控释肥料包膜材料的研制提供新的手段.     

中微肥的生产及其应用

综述了中量和微量元素肥料生产的必要性、生产工艺的改进和在不同土壤条件、作物品种、肥料形式和栽培条件下的应用方法.解决好这一重要问题的关键在于:中微肥的生产,只有综合利用矿产资源和工业废弃资源,才能有效地降低生产成本;只有采取有机螯合的方法,才能保持中微肥的活性;以大量元素肥料为载体,可方便农民使用.     

基于荧光光谱技术研究增效肥料对土壤富里酸荧光特性的影响

为探讨施用增效肥料后对土壤富里酸(FA)荧光特性及腐殖化程度的影响,在黑龙江省黑河市嫩江县和爱辉区两个试验区采取相同施肥处理,设置5个处理组：平衡施肥(NE)、平衡施肥减量25%(CK) 、平衡施肥减量25%+纳米碳增效剂(T1)、平衡施肥减量25%+沸石增效剂(T2)、平衡施肥减量25%+生物炭增效剂(T3),分析土壤中FA荧光光谱特性的变化情况。三维荧光区域积分（FRI）方法不同肥料处理区域F_max相对含量的变化表明,施用增效肥料可以提高土壤腐殖化程度,其中T2＞T1＞T3＞NE＞CK,沸石增效处理对于提高土壤腐殖化程度、提高土壤的供肥水平表现最为显著,其在嫩江试验区的可见荧光FA区域Ⅴ与紫外荧光FA区域Ⅲ所对应的物质相对含量的比值（P_Ⅴ,n/P_Ⅲ,n）较CK处理提高了5.81%,根据平行因子分析方法将土壤FA分为C1组分和C2组分,其中C2组分与C1组分F_max的比值（C2/C1）较CK处理提高了22.09%;在爱辉试验区的P_Ⅴ,n/P_Ⅲ,n较CK处理提高了4.65%,C2/C1较CK处理提高了20.93%;根据平行因子分析（PARAFAC）结果,各处理土壤FA可分为C1和C2两个组分,C1组分为类富里酸(Ex/Em=230 nm, 320/410 nm),C2组分为类胡敏酸(Ex/Em=265/465 nm),施用三种增效肥料均可以提高土壤的供肥能力,其中NE＞T2＞T1＞T3＞CK。与CK处理相比,T1,T2和T3三个增效处理中,T2增效处理的提升作用最为明显,采用沸石作为肥料增效剂对于土壤FA的积极作用要优于纳米碳和生物炭,因此长期施用沸石增效肥料可有效提高土壤供肥能力,能够改善土壤生态环境。     

Oxygen and nitrogen isotopic composition of nitrate in commercial fertilizers,nitric acid,and reagent salts

Nitrate is a key component of synthetic fertilizers that can be beneficial to crop production in agro-ecosystems, but can also cause damage to natural ecosystems if it is exported in large amounts. Stable isotopes, both oxygen and nitrogen, have been used to trace the sources and fate of nitrate in various ecosystems. However, the oxygen isotope composition of synthetic and organic nitrates is poorly constrained. Here, we present a study on the N and O isotope composition of nitrate-based fertilizers. The δ¹⁵N values of synthetic and natural nitrates were 0?±?2?‰ similar to the air N₂ from which they are derived. The δ¹⁸O values of synthetic nitrates were 23?±?3?‰, similar to air O₂, and natural nitrate fertilizer δ¹⁸O values (55?±?5?‰) were similar to those observed in atmospheric nitrate. The Δ¹⁷O values of synthetic fertilizer nitrate were approximately zero following a mass-dependent isotope relationship, while natural nitrate fertilizers had Δ¹⁷O values of 18?±?2?‰ similar to nitrate produced photochemically in the atmosphere. These narrow ranges of values can be used to assess the amount of nitrate arising from fertilizers in mixed systems where more than one nitrate source exists (soil, rivers, and lakes) using simple isotope mixing models.