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Effects of nitrogen deposition and plant litter alteration on soil respiration in a semiarid grassland

机译:氮沉积及植物凋落物改变对半干旱草原土壤呼吸的影响

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Nitrogen (N) deposition and the input of litter to soils are expected to significantly affect soil respiration (R_s). However, the responses of R_s to N deposition and litter input alteration in semiarid grassland are still unclear. We investigated the effects of N addition, litter input alteration, and their interactions on R_s throughout the growing season from May to September in 2017, in Horqin grassland, Northern China. N deposition included N addition (10 g N m~(-2) year~(-1)) and N control (0 g N m~(-2) year~(-1)), and litter alteration consisting of litter removal, litter doubling and litter control were conducted. We found that N addition significantly improved vegetation coverage (P < 0.01) and thus increased root respiration (R_t) by 30% (P < 0.05), but did not significantly enhance R_s (P> 0.05) due to the negative effect of microbial respiration (R_m). Litter removal significantly decreased soil mi-crobial biomass and thus reduced Rm (13%) and Rs (14%), but litter doubling did not significantly alter R_m, R_t and R_s. N addition slightly weakened the inhibition of litter removal and led to soil respiration was not significantly decreased, whereas N addition and litter doubling did not significantly interact with R_s. Furthermore, R_s and its components were mainly mediated by soil temperature, moisture, soil microbial biomass carbon (SMBC) and vegetation coverage, but the structural equation model found that soil temperature, SMBC and coverage were the key controlling factor of R_s, R_m and R_t, respectively. Different influences of N deposition and litter input on R_s, as well as the contributions of R_m and R_t to R_s identified could facilitate the evaluation and prediction of R_s and belowground C storage in grassland ecosystems in the context of future global changes.
机译:氮(N)沉积和垃圾的输入预期对土壤呼吸(R_S)显着影响。然而,R_S在半干旱草原上的沉积和垃圾输入改变的响应仍然不清楚。我们调查了N添加,垃圾投入改变的影响,以及2017年5月至9月在2017年9月在2017年9月在中国北方Horqin Grassland的整个生长季节的互动。 n沉积包括n加(10 g n m〜(-2)年〜(-1))和n控制(0 g n m〜(-2)年〜(-1)),并乱丢垃圾清除组成,进行了垃圾倍增和垃圾控制。我们发现N添加显着改善了植被覆盖率(P <0.01),从而增加了根呼吸(R_T)的30%(P <0.05),但由于微生物呼吸的负面影响,没有显着增强R_S(p> 0.05) (R M)。凋落物去除显着降低了土壤颅骨生物量,从而降低了RM(13%)和卢比(14%),但垃圾倍增没有显着改变R_M,R_T和R_S。 N添加略微削弱抑制凋落物去除并导致土壤呼吸没有显着降低,而另外并加倍加倍没有显着与R_S相互作用。此外,R_S及其组分主要由土壤温度,水分,土壤微生物碳(SMBC)和植被覆盖介导,但结构方程模型发现土壤温度,SMBC和覆盖率是R_S,R_M和R_T的关键控制因子, 分别。 N沉积和垃圾输入对R_S的不同影响以及所识别的R_M和R_T对R_S的贡献可以促进在未来的全球变化的背景下的草原生态系统中R_S和地下C存储的评估和预测。

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