Cui Xiaoqing, Yue Ping, Wu Wenchao, Gong Yanming, Li Kaihui, Misselbrook Tom, Goulding Keith, Liu Xuejun
Key Laboratory of Plant-Soil Interactions of the Ministry of Education, Beijing Key Laboratory of Farmland Soil Pollution Prevention and Remediation, College of Resources and Environmental Sciences, China Agricultural University, Beijing, China.
Sino-France Institute of Earth Systems Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing, China.
Front Plant Sci. 2019 Mar 26;10:356. doi: 10.3389/fpls.2019.00356. eCollection 2019.
Nitrogen (N) partitioning between plant and soil pools is closely related to biomass accumulation and allocation, and is of great importance for quantifying the biomass dynamics and N fluxes of ecosystems, especially in low N-availability desert ecosystems. However, partitioning can differ among species even when growing in the same habitat. To better understand the variation of plant biomass allocation and N retention within ephemeral and annual species we studied the responses of (an ephemeral) and (an annual) to N addition, including plant growth, N retention by the plant and soil, and N lost to the environment using N (double-labeled NH NO (5.16% abundance) added at 0, 0.8, 1.6, 3.2, and 6.4 g pot, equivalent to 0, 15, 30, 60, and 120 kg N ha) in a pot experiment. Higher N addition (N120) inhibited plant growth and biomass accumulation of the ephemeral but not the annual. In addition, the aboveground:belowground partitioning of N (the R:S ratio) of the ephemeral decreased with increasing N addition, but that of the annual increased. The N input corresponding to maximum biomass and N retention of the ephemeral was significantly less than that of the annual. The aboveground and belowground retention of N in the ephemeral were significantly less than those of the annual, except at low N rates. The average plant-soil system recovery of added N by the ephemeral was 70%, significantly higher than that of the annual with an average of 50%. Although the whole plant-soil N recovery of this desert ecosystem decreased with increasing N deposition, our results suggested that it may vary with species composition and community change under future climate and elevated N deposition.
植物与土壤库之间的氮(N)分配与生物量积累和分配密切相关,对于量化生态系统的生物量动态和氮通量至关重要,尤其是在低氮有效性的沙漠生态系统中。然而,即使生长在相同的栖息地,不同物种之间的分配也可能不同。为了更好地理解短命植物和一年生植物中植物生物量分配和氮保留的变化,我们研究了短命植物(一种短命植物)和一年生植物(一种一年生植物)对添加氮的响应,包括植物生长、植物和土壤对氮的保留,以及在盆栽实验中使用氮(双标记硝酸铵(丰度为5.16%),以0、0.8、1.6、3.2和6.4克/盆添加,相当于0、15、30、60和120千克氮/公顷)向环境中损失的氮。较高的氮添加量(N120)抑制了短命植物的植物生长和生物量积累,但对一年生植物没有影响。此外,短命植物地上部分:地下部分的氮分配(R:S比)随着氮添加量的增加而降低,但一年生植物的则增加。与短命植物最大生物量和氮保留相对应的氮输入显著低于一年生植物。除了低氮水平外,短命植物地上和地下的氮保留量均显著低于一年生植物。短命植物对添加氮的植物-土壤系统平均回收率为70%,显著高于一年生植物的平均50%。尽管该沙漠生态系统的整个植物-土壤氮回收率随着氮沉降的增加而降低,但我们的结果表明,在未来气候和氮沉降增加的情况下,它可能会因物种组成和群落变化而有所不同。