首页> 外文期刊>European Journal of Soil Biology >Nutrient availability, soil respiration and microbial biomass after the second residue addition are influenced by the C/N ratio of the first residue added, but not by drying and rewetting between residue amendments
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Nutrient availability, soil respiration and microbial biomass after the second residue addition are influenced by the C/N ratio of the first residue added, but not by drying and rewetting between residue amendments

机译:第二次添加残留物后的养分利用率,土壤呼吸和微生物生物量受添加的第一个残留物的C / N比的影响,但不受残留物修正之间的干燥和重新润湿影响

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It has been shown that the C/N ratio of the first residue amendment influences soil respiration and nutrient availability after the addition of a second residue, which is referred to as legacy effect. However, little is known about the effect of dry-rewet (DRW) cycles on nutrient availability in soil amended with residues differing in C/N ratio and on the legacy effect. A loamy soil was amended twice (days 0 and 32) with plant residues with either high (H) or low (L) C/N ratio to give the treatments low than high (LH) or high then low C/N residue (HL). Between the first and the second residue addition the soil was maintained at 50% WHC or exposed to one, two or four DRW cycles. After the second residue addition all treatments were kept at 50% WHC until day 64. During the first period, N and P availability and microbial biomass C were higher in LH than HL in all moisture treatments. Cumulative respiration (mg CO2-C g soil(-1)) was higher in LH than HL only in the constantly moist treatment. Available N and P concentration were higher in dry soil than moist soils in 1 DRW and 2 DRW. After the second residue addition, moisture and residue treatments did not differ in available N and P concentration, which confirmed the legacy effect, but indicated that drying only temporarily increased N and P availability and that the previous moisture treatment did not influence the legacy effect. (C) 2016 Elsevier Masson SAS. All rights reserved.
机译:已经表明,添加第二种残留物后,第一种残留物修正的C / N比会影响土壤呼吸和养分的利用率,这被称为遗留效应。但是,关于干再湿(DRW)循环对土壤中养分有效性的影响知之甚少,而残留物的碳氮比(C / N)不同,并且对遗留效应也没有影响。用高(H)或低(L)C / N比的植物残渣对壤土进行两次修正(第0天和第32天),以使处理比高(LH)或高然后低C / N的残渣(HL )。在第一次和第二次添加残留物之间,土壤保持在50%WHC或暴露于一个,两个或四个DRW循环。在第二次添加残留物后,所有处理均保持在50%WHC下直至第64天。在第一阶段中,在所有水分处理中,LH中的N和P利用率以及微生物量C均高于HL。仅在持续湿润的处理中,LH中的累积呼吸(mg CO2-C g土壤(-1))高于HL。在1 DRW和2 DRW中,干土壤中的有效N和P浓度高于潮湿土壤。在第二次添加残留物之后,水分和残留物处理的可用氮和磷浓度没有差异,这确认了遗留效应,但表明干燥只是暂时增加了氮和磷的利用率,并且先前的水分处理不会影响遗留效应。 (C)2016 Elsevier Masson SAS。版权所有。

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