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Effect of substrate quality on the N uptake routes of soil microorganisms in different soil depths

机译:基质质量对不同土壤深度土壤微生物氮吸收途径的影响

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A few studies have indicated that substrate quality is an important factor affecting the N uptake route of soil microorganisms, but less is known about the effect of soil depth on the N uptake route under different nutrient conditions. Objectives were to investigate (i) the effects of corn residues with different C to N ratios in the presence and absence of mineral N and (ii) the effects of soil depth on the N uptake route of soil microorganisms. An incubation experiment with surface soils (0-5 cm, C/N = 10) and subsoils (30-40 cm, C/N = 9) from three German loess sites was carried out for 21 days at 20 degrees C and 60% of their water-holding capacity. The following treatments were used: no addition (control), addition of corn residues with a C/N ratio of 20, 40, and 40 + (NH4)(2)SO4. To distinguish between the N uptake routes, the mineralization rate of amino acids was determined using N-15-labeled amino acids. In the control surface soil and subsoil the direct uptake of organic N was favored with no significant (p < 0.05) differences between depths despite significantly higher microbial activity, protease activity, gross N mineralization rate and availability of inorganic N in the surface soil, suggesting that N availability relative to C was similar at both depths. Substrate additions resulted in significantly increased protease activities at both depths after 3-7 days. Addition of corn residue with a high C/N ratio resulted in an increased direct uptake (97% and 94% in the surface soil and subsoil, respectively), compared with addition of corn residue with a low C/N ratio or addition of corn residue and inorganic N (79 to 91% direct uptake). This suggests that the enzyme system involved in the direct uptake was slightly repressed under conditions of sufficient mineralizable N (C/N of 20) or increased concentrations of NH4+. Substrate additions resulted in an initial significantly higher increase in the direct uptake in the surface soil than in the subsoil. (C) 2015 Elsevier GmbH. All rights reserved.
机译:一些研究表明,基质质量​​是影响土壤微生物氮吸收途径的重要因素,但对于不同养分条件下土壤深度对氮吸收途径的影响知之甚少。目的是研究(i)在存在和不存在矿质氮的情况下,不同碳氮比的玉米残留物的影响,以及(ii)土壤深度对土壤微生物氮吸收途径的影响。在20摄氏度和60%的温度下,对来自德国三个黄土站点的表层土壤(0-5 cm,C / N = 10)和地下土壤(30-40 cm,C / N = 9)进行了为期21天的孵化实验他们的持水能力。使用以下处理:不添加(对照),添加C / N为20、40和40 +(NH4)(2)SO4的玉米残渣。为了区分N吸收途径,使用N-15标记的氨基酸确定氨基酸的矿化率。在对照表层土壤和下层土壤中,尽管土壤微生物活性,蛋白酶活性,总氮矿化率和无机氮的利用率明显提高,但在深度之间无明显差异(p <0.05)的情况下,有机氮的直接吸收受到了支持,这表明N在两个深度上相对于C的可用性都相似。加入底物会导致3-7天后两个深度的蛋白酶活性显着增加。与添加低C / N比例的玉米残渣或添加玉米相比,添加高C / N比例的玉米残渣导致增加的直接吸收(分别在表层土壤和地下土壤中增加97%和94%)残留物和无机氮(直接吸收79%至91%)。这表明在足够矿化的氮(C / N为20)或增加的NH4 +浓度的条件下,直接吸收所涉及的酶系统受到轻微抑制。底物的添加导致表层土壤的直接吸收最初的增加明显高于底土。 (C)2015 Elsevier GmbH。版权所有。

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