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Nitrogen deposition alters nitrogen cycling and exotic annual grass litter decomposition in southern California.

机译:氮的沉积改变了南加州的氮循环和每年异国草丛分解。

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This study demonstrated that nitrogen (N) deposition alters litter decomposition and N cycling in exotic annual grasslands that exist in former coastal sage scrub ecosystems of southern California. N deposition resulted in altered tissue chemistry of the exotic annual grass Bromus diandrus by increasing tissue N and decreasing lignin content. Altered B. diandrus tissue chemistry and elevated soil N associated with N deposition resulted in accelerated rates of N movement from litter to soil and litter decomposition during the early stages of decomposition. Microbial enzyme activities were used as indicators of microbial response to litter quality and soil N. Faster mass loss rates of high N/low lignin litter compared to low N/high lignin litter corresponded to higher activity levels of the C acquiring enzyme, beta-1,4 glucosidase. Faster N mineralization from high N/low lignin litter is probably due to greater activity of the proteolytic enzyme leucine aminopeptidase. As litter decomposition progressed, changes in microbial enzyme activity from decomposing B. diandrus litter reflected changes in tissue carbon (C) and N. By the later stages of decomposition, there was no longer a difference in mass loss between litter types. N deposition resulted in faster rates of gross and net soil N mineralization during the beginning of the rainy season, which could make N available for plant uptake earlier than without N deposition. Long-term N deposition resulted in N accumulation in the soil profile to at least 1 m, which could allow N to persist in the ecosystem. By altering ecosystem processes in exotic annual grasslands of southern California, N deposition may facilitate the invasion of nitrophilous exotic annual grasses into native coastal sage scrub.
机译:这项研究表明,氮(N)的沉积改变了南加州前沿海鼠尾草灌木丛生态系统中存在的异国一年生草地的凋落物分解和氮循环。 N的沉积通过增加组织N并降低木质素含量而导致异域一年生无芒一年生布鲁姆草的组织化学改变。 B. diandrus组织化学的变化和与N沉积相关的土壤N的升高导致了氮在分解初期从垫料向土壤移动的速率加快以及垫料分解。微生物酶活性被用作微生物对垫料质量和土壤氮素反应的指标。与低氮/高木质素垫料相比,高氮/低木质素垫料的质量损失速度更快,对应于碳获取酶β-1的较高活性水平,4葡糖苷酶。高氮/低木质素垫料中更快的氮矿化可能是由于蛋白水解酶亮氨酸氨基肽酶的活性更高。随着垃圾分解的进行,分解双歧双歧杆菌垃圾的微生物酶活性变化反映了组织碳(C)和氮的变化。在分解的后期,垃圾类型之间的质量损失不再存在差异。在雨季开始时,氮的沉积导致土壤总氮和净氮矿化的速率加快,这可能使氮比没有氮沉积的植物更早被植物吸收。长期的氮沉降导致土壤剖面中的氮积累至少达到1 m,这可能使氮在生态系统中持续存在。通过改变加利福尼亚南部外来一年生草地的生态系统过程,氮的沉积可促进含氮外来一年生草入侵本地沿海鼠尾草灌木丛。

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