
石灰性土壤微生物量碳_氮与土壤颗粒组成和氮矿化势的关系_金发会.pdf
8页石灰性土壤微生物量碳、 氮与土壤颗粒组成 和氮矿化势的关系 3 金发会 1,2 李世清 1,23 3 卢红玲 1 李生秀 2 (1西北农林科技大学/中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌712100; 2西北农林科技大学资源环境学院 ,陕西杨凌712100) 摘 要 以黄土高原土壤类型和土壤肥力差异较大的25个农田石灰性耕层土壤为供试土 样,研究了土壤微生物量碳 (B C)、 微生物量氮 (B N)与土壤氮素矿化势 (N 0)、 全氮 (TN)、 有机 碳(OC)及土壤颗粒组成的关系.结果表明: BC、BN与TN、OC呈极显著正相关(P0101 mm颗粒的吸水性、 保肥性、 粘结性、 粘着 性和可塑性较差;而粒径0101 mm)相比,进一步说明小粒级颗 粒 ( 0 101 mm)对土壤有机质的吸附和保持能力更 强.这一方面与小粒级颗粒中有机质含量较高有关, 另一方面与小粒级颗粒和有机质复合形成更加稳定 的有机无机复合体有关.有研究表明,粗质土BC占 OC的比例较细质土低,但粗质土中的C、N转化较 快 [34 ] ,这与本研究土壤微生物量碳与各土样物理性 粘粒 ( 0101 mm)呈负相关性的结 论相一致. 5 结 论 1) 土壤BC与TN、OC之间呈极显著正相关,相 关系数分别为01846和01 683 ( P 0101) ,土壤BN 与TN、OC之间也呈极显著正相关,相关系数分别为 01661和01 519 ( P0101) ,表明BC、BN与土壤肥力 关系密切,可作为评价土壤质量的生物学指标.土壤 微生物量碳氮比 (B C/BN)在018~816之间,较土壤 有机碳与全氮比值 (5 121~111 89) 低,说明BN是植 物有效氮的重要储备库和源. 2)BC、BN与土壤氮素矿化势 (N 0)高度相关,相 关系数分别为01741和01665 (P 0101) ,表明BN 是表征土壤供氮能力的另一指标. 3) 土壤物理性粘粒 ( 0101 mm)与各指标呈显著或极显著负相关,物理性 粘粒和砂粒比值与各指标呈显著或极显著正相关. 参考文献 [1] AdamsMA, Attewill PM. 1986. 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