McGilloway R L, Weaver R W, Ming D W, Gruener J E
Soil and Crop Sciences Department, Texas A&M University, College Station, TX, 77843-2474, USA.
Plant Soil. 2003 Oct;256(2):371-8. doi: 10.1023/a:1026174026995.
Clinoptilolite is a zeolite mineral with high cation exchange capacity used in zeoponic substrates that have been proposed as a solid medium for growing plants or as a fertilizer material. The kinetics of nitrification has not been measured for NH4+ saturated zeoponic substrate. Experiments were conducted to evaluate the production of NO2- and NO3-, and nitrifier populations in zeoponic substrates. Small columns were filled with zeoponic substrate inoculated with a commercial inoculum or soil enrichment culture of nitrifying bacteria. In addition to column studies, a growth chamber study was conducted to evaluate the kinetics of nitrification in zeoponic substrates used to grow radishes (Raphanus sativus L.). The zeoponic substrate provided a readily available source of NH4+, and nitrifying bacteria were active in the substrate. Ammonium oxidation rates in column studies ranged from 5 to 10 micrograms N g-1 substrate h-1, and NO2- oxidation rates were 2 to 9.5 micrograms N g-1 substrate h-1. Rates determined from the growth chamber study were approximately 1.2 micrograms N g-1 substrate h-1. Quantities of NH4+ oxidized to NO2- and NO3- in inoculated zeoponic substrate were in excess of plant up-take. Acidification as a result of NH4+ oxidation resulted in a pH decline, and the zeoponic substrate showed limited buffering capacity.
斜发沸石是一种具有高阳离子交换容量的沸石矿物,用于沸石栽培基质中,这种基质已被提议作为种植植物的固体介质或肥料材料。对于铵离子饱和的沸石栽培基质,尚未测定其硝化动力学。开展了实验以评估沸石栽培基质中二氧化氮和硝酸根的产生以及硝化细菌种群数量。小柱中填充有接种了商业接种物或硝化细菌土壤富集培养物的沸石栽培基质。除了柱实验外,还进行了生长室实验,以评估用于种植萝卜(Raphanus sativus L.)的沸石栽培基质中的硝化动力学。沸石栽培基质提供了易于利用的铵离子来源,硝化细菌在该基质中具有活性。柱实验中的铵氧化速率为5至10微克氮每克基质每小时,二氧化氮氧化速率为2至9.5微克氮每克基质每小时。从生长室实验确定的速率约为1.2微克氮每克基质每小时。接种的沸石栽培基质中氧化为二氧化氮和硝酸根的铵离子量超过了植物的吸收量。铵氧化导致的酸化使pH值下降,且沸石栽培基质显示出有限的缓冲能力。