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首页> 外文期刊>Journal of Plant Nutrition >LIMESTONE PARTICLE SIZE AND RESIDUAL LIME CONCENTRATION AFFECT PH BUFFERING IN CONTAINER SUBSTRATES
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LIMESTONE PARTICLE SIZE AND RESIDUAL LIME CONCENTRATION AFFECT PH BUFFERING IN CONTAINER SUBSTRATES

机译:石灰石颗粒大小和残余石灰浓度对容器基质中PH缓冲的影响

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The objective was to quantify how the concentration and particle size of unreacted oresidualo limestone affected pH buffering capacity for ten commercial and nine research container substrates that varied in residual calcium carbonate equivalents (CCE) from 0.3 to 4.9 g CCE center dot L-1. The nine research substrates contained 70% peat:30% perlite (by volume) with dolomitic hydrated lime at 2.1 g center dot L-1, followed by incorporation of one of four particle size fractions [850 to 2000 m (10 to 20 US mesh), 250 to 850 m (20 to 60 US mesh), 150 to 250 m (60 to 100 US mesh), or 75 to 150 m (100 to 200 US mesh)] of a dolomitic carbonate limestone at 0, 1.5 or 3.0 g center dot L-1. Substrate-pH buffering was quantified by measuring the pH change following either (a) mineral acid drenches without plants, or (b) a greenhouse experiment where an ammonium-based (acidic) or nitrate-based (basic) fertilizer was applied to Impatiens wallerana Hook. F. Increasing residual CCE in commercial substrates was correlated with greater pH buffering following either the hydrochloric acid (HCl) drench or impatiens growth with an ammonium-based fertilizer. Research substrates with high applied lime rate (3.0 kg center dot m-3) had greater pH buffering than at 0 or 1.5 g center dot L-1. At 3 g center dot L-1, the intermediate limestone particle size fractions of 250 to 850 m and 150 to 250 (20 to 60 or 60 to 100 US mesh) provided the greatest pH-buffering with impatiens. Particle fractions finer than 150 m reacted quickly over time, whereas buffering by particles coarser than 850 m was limited because of the excessively slow reaction rate during the experimental periods. Addition of acid from either an ammonium-based fertilizer or HCl reduced residual CCE over time. Dosage with 40 meq acid from HCl per liter of substrate or titration with HCl acid to substrate-pH of 4.5 were well-correlated with pH buffering in the greenhouse trials and may be useful laboratory protocols to compare pH buffering of substrates. With nitrate fertilizer application, residual CCE did not affect buffering against increasing pH. Residual limestone is an important substrate property that should be considered for pH management in greenhouse crop production under acidic conditions.
机译:目的是量化未反应的矿石硅灰石的浓度和粒径如何影响10种商用和9种研究容器底物的pH缓冲能力,这些底物的残余碳酸钙当量(CCE)从0.3到4.9 g CCE中心点L-1变化。九种研究基质的泥炭含量为70%:珍珠岩30%(体积),白云母熟石灰在2.1 g中心点L-1处,然后掺入四个粒度级分之一[850至2000 m(10至20美国目) ),250-850 m(20至60 US目),150至250 m(60至100 US目)或75至150 m(100至200 US目)]的白云岩碳酸盐石灰岩,其厚度为0、1.5或3.0 g中心点L-1。通过测量(a)在没有植物的情况下浸透无机酸,或(b)在温室实验中对铵盐(酸性)或硝酸盐(碱性)施肥的温室试验来量化底物的pH缓冲。钩。 F.商业化基质中残留的CCE的增加与盐酸(HCl)浸湿或用铵基肥料使凤仙花生长后的更大pH缓冲液相关。具有高石灰施用量(3.0 kg中心点m-3)的研究基质比0或1.5 g中心点L-1具有更大的pH缓冲。在3 g中心点L-1处,中间的石灰石粒度级分250至850 m和150至250(20至60或60至100 US目)提供了最大的含凤仙花的pH缓冲。随时间推移,小于150 m的颗粒分数会迅速反应,而由于实验期间反应速度过慢,因此限制了大于850 m的颗粒的缓冲作用。从铵基肥料或HCl中添加酸会随着时间的推移减少残留的CCE。在温室试验中,每升底物使用40毫克当量的HCl剂量或用HCl酸滴定至底物pH值为4.5,这与温室试验中的pH缓冲作用密切相关,对于比较底物的pH缓冲作用可能是有用的实验室规程。施用硝酸盐肥料后,残留的CCE不会影响缓冲液以防止pH值升高。残留的石灰石是重要的基质特性,在酸性条件下进行温室作物生产中的pH管理时应考虑该特性。

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