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柳枝稷生物炭对两种干旱土壤的影响。

Switchgrass biochar affects two aridisols.

机构信息

USDA-ARS, Northwest irrigation and Soils Research Lab., Kimberly, ID, USA.

出版信息

J Environ Qual. 2012 Jul-Aug;41(4):1123-30. doi: 10.2134/jeq2011.0100.

Abstract

The use of biochar has received growing attention because of its ability to improve the physicochemical properties of highly weathered Ultisols and Oxisols, yet very little research has focused on its effects in Aridisols. We investigated the effect of low or high temperature (250 or 500°C) pyrolyzed switchgrass () biochar on two Aridisols. In a pot study, biochar was added at 2% w/w to a Declo loam (Xeric Haplocalcids) or to a Warden very fine sandy loam (Xeric Haplocambids) and incubated at 15% moisture content (by weight) for 127 d; a control (no biochar) was also included. Soils were leached with 1.2 to 1.3 pore volumes of deionized HO on Days 34, 62, 92, and 127, and cumulative leachate Ca, K, Mg, Na, P, Cu, Fe, Mn, Ni, Zn, NO-N, NO-N, and NH-N concentrations were quantified. On termination of the incubation, soils were destructively sampled for extractable Cr, Cu, Fe, K, Mg, Mn, Na, Ni, P, Zn, NO-N, and NH-N, total C, inorganic C, organic C, and pH. Compared with 250°C, the 500°C pyrolysis temperature resulted in greater biochar surface area, elevated pH, higher ash content, and minimal total surface charge. For both soils, leachate Ca and Mg decreased with the 250°C switchgrass biochar, likely due to binding by biochar's functional group sites. Both biochars caused an increase in leachate K, whereas the 500°C biochar increased leachate P. Both biochars reduced leachate NO-N concentrations compared with the control; however, the 250°C biochar reduced NO-N concentrations to the greatest extent. Easily degradable C, associated with the 250°C biochar's structural make-up, likely stimulated microbial growth, which caused NO-N immobilization. Soil-extractable K, P, and NO-N followed a pattern similar to the leachate observations. Total soil C content increases were linked to an increase in organic C from the biochars. Cumulative results suggest that the use of switchgrass biochar prepared at 250°C could improve environmental quality in calcareous soil systems by reducing nutrient leaching potential.

摘要

生物炭的使用因其能够改善高度风化的强风化淋溶土和氧化土的物理化学性质而受到越来越多的关注,但很少有研究关注其在干旱土中的作用。我们研究了低温(250°C)或高温(500°C)热解柳枝稷生物炭对两种干旱土的影响。在盆栽研究中,生物炭以 2%(w/w)的比例添加到 Declo 壤土(干旱弱淋溶土)或 Warden 细砂壤土(干旱弱淋溶土)中,并在 15%(重量)的水分含量下培养 127 天;同时还包括一个对照(无生物炭)。在第 34、62、92 和 127 天,用 1.2 至 1.3 孔隙体积的去离子水对土壤进行淋洗,并定量测定累积淋出液 Ca、K、Mg、Na、P、Cu、Fe、Mn、Ni、Zn、NO-N、NO-N 和 NH-N 的浓度。培养结束时,对土壤进行破坏性采样,以测定可提取的 Cr、Cu、Fe、K、Mg、Mn、Na、Ni、P、Zn、NO-N 和 NH-N、总 C、无机 C、有机 C 和 pH 值。与 250°C 相比,500°C 的热解温度导致生物炭的表面积更大、pH 值更高、灰分含量更高和总表面电荷最小。对于两种土壤,250°C 柳枝稷生物炭的淋出液 Ca 和 Mg 减少,这可能是由于生物炭的官能团位点的结合。两种生物炭都导致淋出液 K 的增加,而 500°C 生物炭增加了淋出液 P。与对照相比,两种生物炭都降低了淋出液 NO-N 浓度;然而,250°C 生物炭将 NO-N 浓度降低到最大程度。与 250°C 生物炭的结构组成相关的易降解 C 可能刺激了微生物的生长,从而导致 NO-N 的固定。土壤可提取的 K、P 和 NO-N 的变化模式与淋出液的观察结果相似。总土壤 C 含量的增加与生物炭中的有机 C 增加有关。累积结果表明,使用 250°C 制备的柳枝稷生物炭可以通过减少养分淋失潜力来改善钙质土壤系统的环境质量。

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