Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China.
College of Urban and Environmental Sciences, Peking University, Peking 100871, China.
Sci Total Environ. 2019 Mar 20;657:811-818. doi: 10.1016/j.scitotenv.2018.12.101. Epub 2018 Dec 8.
Grassland ecosystems play an important role in the global terrestrial silicon (Si) cycle, and Si is a beneficial element and structural constituent for the growth of grasses. In previous decades, grasslands have been degraded to different degrees because of the drying climate and intense human disturbance. However, the impact of grassland degradation on the distribution and bioavailability of soil Si is largely unknown. Here, we investigated vegetation and soil conditions of 30 sites to characterize different degrees of degradation for grasslands in the agro-pastoral ecotone of northern China. We then explored the impact of grassland degradation on the distribution and bioavailability of soil Si, including total Si and four forms of noncrystalline Si in three horizons (0-10, 10-20 and 20-40 cm) of different soil profiles. The concentrations of noncrystalline Si in soil profiles significantly decreased with increasing degrees of degradation, being 7.35 ± 0.88 mg g, 5.36 ± 0.39 mg g, 3.81 ± 0.37 mg g and 3.60 ± 0.26 mg g in non-degraded, lightly degraded, moderately degraded and seriously degraded grasslands, respectively. Moreover, the storage of noncrystalline Si decreased from higher than 40 t ha to lower than 23 t ha. The corresponding bioavailability of soil Si also generally decreased with grassland degradation. These processes may not only affect the Si pools and fluxes in soils but also influence the Si uptake in plants. We suggest that grassland degradation can significantly affect the global grassland Si cycle. Grassland management methods such as fertilizing and avoiding overgrazing can potentially double the content and storage of noncrystalline Si in soils, thereby enhancing the soil Si bioavailability by >17%.
草原生态系统在全球陆地硅(Si)循环中发挥着重要作用,Si 是草类生长的有益元素和结构组成部分。在过去几十年中,由于气候干燥和人类活动的强烈干扰,草原已经退化到不同程度。然而,草原退化对土壤 Si 分布和生物有效性的影响在很大程度上尚不清楚。在这里,我们调查了 30 个地点的植被和土壤条件,以描述中国北方农牧交错带不同程度退化的草原。然后,我们探讨了草原退化对土壤 Si 分布和生物有效性的影响,包括总 Si 和三种土壤剖面三个层次(0-10、10-20 和 20-40 cm)中四种非晶态 Si 的分布和生物有效性。土壤剖面中非晶态 Si 的浓度随退化程度的增加而显著降低,在未退化、轻度退化、中度退化和严重退化的草原中分别为 7.35±0.88、5.36±0.39、3.81±0.37 和 3.60±0.26mg g。此外,非晶态 Si 的储量从高于 40 t ha减少到低于 23 t ha。土壤 Si 的相应生物有效性也普遍随草原退化而降低。这些过程不仅可能影响土壤中的 Si 库和通量,还可能影响植物对 Si 的吸收。我们认为,草原退化会显著影响全球草原 Si 循环。草原管理方法,如施肥和避免过度放牧,可能会使土壤中非晶态 Si 的含量和储量增加一倍,从而使土壤 Si 生物有效性提高超过 17%。