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Nitrogen transformations and nitrate leaching in mine soils reclaimed with sewage sludge and coal combustion residues.

机译:用污水污泥和煤燃烧残渣回收的矿质土壤中的氮转化和硝态氮淋失。

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Nitrogen mineralization and nitrate leaching were investigated in an acid mine soil reclaimed with sewage sludge (SS) and coal combustion residues (CCR). In the field experiments mine soil was amended with three rates of SS (0, 1200, and 2400 kg N ha{dollar}sp{lcub}-1{rcub}){dollar} and two types of CCR, i.e. fly ash (FA) and fluidized bed waste (FBW) applied at rates equivalent to once and twice the lime requirement of the soil. Laboratory incubation experiments using two procedures (leached and nonleached) were also conducted for 46 weeks to investigate N mineralization in an acid mine soil with or without liming agents (agricultural lime and FBW), and in two fly ashes (one alkaline and the other near neutral) used as top soil substitutes. Sewage sludge was added to supply 0, 600, 1200, and 2400 kg N ha{dollar}sp{lcub}-1{rcub}.{dollar} Application of SS alone or along with CCR resulted in a soil solution NO{dollar}sb3sp{lcub}-{rcub}{dollar}-N concentration in excess of drinking water standard limit of 10 mg L{dollar}sp{lcub}-1{rcub}{dollar} for the initial six to seven months of the experiment. Both mineral N and NO{dollar}sb3sp{lcub}-{rcub}{dollar}-N in soil solution decreased with time and remained below 10 mg L{dollar}sp{lcub}-1{rcub}{dollar} after seven months. Laboratory incubation studies demonstrated that cumulative N mineralized after 46 weeks expressed as percentage of organic N added was inversely related to the rate of SS applied in both leached and nonleached procedures. Less N was mineralized when SS was added to fly ashes than to the topsoil. Addition of SS resulted in gaseous losses of nitrogen. The losses were mainly due to NH{dollar}sb3{dollar} volatilization in alkaline FA and by denitrification in the mine soil and neutral FA. The results of the field study showed that FA amended with SS can serve as an acceptable growth media for revegetation.
机译:在用污水污泥(SS)和燃煤残渣(CCR)回收的酸性矿山土壤中研究了氮矿化和硝酸盐淋失。在田间试验中,用三种比率的SS(0、1200和2400 kg N ha {dol} sp {lcub} -1 {rcub}){dollar}和两种CCR类型,即粉煤灰(FA )和流化床废料(FBW)的施用量相当于土壤石灰需求量的一倍和两倍。还使用两种方法(淋滤和非淋滤)进行了实验室培养实验,历时46周,以研究在有或没有石灰剂(酸性石灰和FBW)的酸性矿山土壤中以及在两种粉煤灰(一种碱性粉煤灰和另一种接近碱性粉煤灰的土壤)中的氮矿化作用。中性)用作土壤替代品。添加了污水污泥,以供应0、600、1200和2400 kg N ha {dol}} {lcub} -1 {rcub}。{dollar}单独施用SS或与CCR一起使用会产生土壤溶液NO {dollar}在实验的最初6到7个月,sb3sp {lcub}-{rcub} {dollar} -N浓度超过饮用水标准限值10 mg L {dollar} sp {lcub} -1 {rcub} {dollar} 。土壤溶液中的矿质氮和NO {dollar} sb3sp {lcub}-{rcub} {dollar} -N随时间减少,并在七点后仍低于10 mg L {dollar} sp {lcub} -1 {rcub} {dollar}个月。实验室培养研究表明,在46周后矿化的累积N(以添加的有机N的百分比表示)与淋滤和非淋滤程序中SS的施用率成反比。当添加SS到飞灰中时,矿化的N少于表层土壤中的N。 SS的添加导致氮气的气态损失。损失主要是由于碱性FA中的NH {dolb} sb3 {dollar}挥发以及矿山土壤和中性FA中的反硝化作用所致。田间研究的结果表明,用SS改良的FA可以作为可接受的植被再生培养基。

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