首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Vertical distribution of soil total nitrogen and soil total phosphorus in the critical zone on the Loess Plateau, China
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Vertical distribution of soil total nitrogen and soil total phosphorus in the critical zone on the Loess Plateau, China

机译:中国黄土高原临界区土壤总氮和土壤总磷的垂直分布

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摘要

It is important to determine the vertical distributions of soil total nitrogen (SIN) and soil total phosphorus (STP) as well as the factors that influence them in the Earth's critical zone (CZ) in order to understand the N/P cycle in the CZ. However, few data are available regarding the vertical distributions of STN and STP in deep soil profiles in the CZ. Thus, this study investigated the vertical distributions of the STN and STP as well as related factors in a deep soil profile on the Loess Plateau, China. Soil drilling was used to collect 703 soil samples throughout the soil profile from five sites. The STN decreased initially at all of the sampling sites (except at Shenmu), before fluctuating with increasing depth throughout the profile, whereas the STP exhibited a fluctuating trend at all sites. The mean STN and STP concentrations ranged from 0.12 g kg(-1) to 0.25 g kg(-1) and from 0.45 g kg(-1) to 0.58 g kg(-1), respectively. The adjusted r(2) values based on stepwise multiple linear regressions for STN and SIP ranged from 35% to 83% and from 4% to 17%, respectively, and thus, SIN was explained better by the measured soil variables compared with STP. The mean STN and STP stocks ranged from 1.87 to 3.90 mg ha(-1) and from 6.75 to 9.09 mg ha(-1), respectively. The results of this study facilitate evaluations of STN and STP stocks and studies of the N/P cycle in the CZ on the Loess Plateau.
机译:确定土壤总氮(SIN)和土壤总磷(STP)的垂直分布以及影响其在地球临界区(CZ)中的因素,以便理解CZ中的N / P周期。然而,在CZ中的深层土壤分布中的STN和STP的垂直分布很少有数据。因此,本研究研究了STN和STP的垂直分布以及黄土高原的深层土壤剖面中的相关因素。土壤钻井用于从五个地点的土壤剖面中收集703种土壤样品。 STN最初在所有采样点(神木除外)下降,然后在整个轮廓上越来越多的深度波动,而STP在所有网站上表现出波动的趋势。平均STN和STP浓度范围为0.12g kg(-1)至0.25g kg(-1),分别为0.45g kg(-1)至0.58g kg(-1)。基于STN和SIP的逐步多线性回归的调节的R(2)值分别为35%至83%,分别为4%至17%,因此通过测量的土壤变量与STP相比,SIN更好地解释。平均STN和STP股票分别为1.87至​​3.90 mg HA(-1),分别为6.75至9.09 mg(-1)。本研究的结果促进了黄土高原CZ中的STN和STP股票的评估和研究CZ中的N / P循环。

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