土壤含水量和土壤质地对使用两种坚固离子选择电极进行原位 pH 值快速测量的影响

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2024-05-17 DOI:10.5194/soil-10-321-2024
Sebastian Vogel, Katja Emmerich, Ingmar Schröter, Eric Bönecke, Wolfgang Schwanghart, Jörg Rühlmann, Eckart Kramer, Robin Gebbers
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引用次数: 0

摘要

摘要使用离子选择电极(ISE)进行原位土壤 pH 值测量可避免耗时的采样和异地实验室工作,因此在精准农业的土壤制图中受到越来越多的关注。然而,与标准实验室方案不同的是,原位 pH 测量是在较低和不同的土壤含水量(SMC)下进行的,这会对传感器读数产生明显影响。此外,由于原位测量时与土壤的接触时间相对较短,土壤质地可能会产生影响,因为质地会控制质子向电极界面的迁移。与标准玻璃电极相比,用于原位测量的电极由灵敏度较低但更坚固的材料制成,这可能会加剧上述影响。因此,本研究旨在研究土壤湿度和土壤质地对使用直接压入土壤 30 秒的坚固锑和环氧树脂体 ISE 测量 pH 值的影响。SMC 从干燥条件逐渐增加到田间容量。土壤质地等级范围很广,沙子、粉土和粘土的含量分别为 16% 至 91%、5% 至 44% 和 4% 至 65%。对数据进行了指数模型拟合,以量化 SMC 与 pH 值之间的关系。结果表明,无论使用哪种 pH 值 ISE,SMC 的增加都会导致 pH 值最大增加约 1.5 个 pH 单位。此外,对于砂质土壤质地,pH 值与 SMC 之间呈相当线性的关系,而随着平均颗粒直径(MPD)的减小,该模型呈明显的指数形状,即低 SMC 时 pH 值增加较大,高 SMC 时呈高原效应。随着 SMC 的增加,pH 值逐渐接近在 0.01 M CaCl2(土壤与溶液的比例为 1:2.5)中用玻璃电极测量的标准 pH 值。因此,在高 SMC 条件下,传感器 pH 值与标准 pH 值的后续校准可以忽略不计,这可能与使用传感器 pH 数据估算石灰需求量有关。pH 测量误差随着土壤湿度的增加呈指数下降,随着 MPD 的降低而增加。使用膝点检测,无论使用哪种 pH ISE,当 SMC > 11 % 时都能获得可靠的 pH 值。对拟合指数模型回归系数的分析表明,pH 值的最大增幅也取决于土壤质地;也就是说,土壤湿度变化对 pH 值的影响随着 MPD 的减小而增大。此外,指数曲线的凹度也随着 MPD 的降低而增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effect of soil moisture content and soil texture on fast in situ pH measurements with two types of robust ion-selective electrodes
Abstract. In situ soil pH measurements with ion-selective electrodes (ISEs) are receiving increasing attention in soil mapping for precision agriculture as they can avoid time-consuming sampling and off-site laboratory work. However, unlike the standard laboratory protocol, in situ pH measurements are carried out at lower and varying soil moisture contents (SMCs), which can have a pronounced effect on the sensor readings. In addition, as the contact with the soil during in situ measurements should be relatively short, effects of soil texture could be expected because texture controls the migration of protons to the electrode interface. This may be exacerbated by the fact that the electrodes used for in situ measurements are made of less sensitive but more robust materials as compared to the standard glass electrode. Therefore, the aim of the present study was to investigate the effect of soil moisture and soil texture on pH measurements using robust antimony and epoxy-body ISEs pressed directly into the soil for 30 s. The SMC was gradually increased from dry conditions to field capacity. A wide range of soil texture classes were included, with sand, silt, and clay contents ranging from 16 % to 91 %, 5 % to 44 %, and 4 % to 65 %, respectively. An exponential model was fitted to the data to quantify the relationship between SMC and pH. The results show that an increase in SMC causes a maximum increase in pH of approximately 1.5 pH units, regardless of the type of pH ISE used. Furthermore, for sandy soil textures, a rather linear relationship between pH and SMC was observed, whereas, with decreasing mean particle diameter (MPD), the model had a pronounced exponential shape, i.e., a greater pH increase at low SMC and a plateau effect at high SMC. With increasing SMC, the pH values asymptotically approached the standard pH measured with a glass electrode in 0.01 M CaCl2 (soil : solution ratio of 1:2.5). Thus, at high SMC, subsequent calibration of the sensor pH values to the standard pH value is negligible, which may be relevant for using the sensor pH data for lime requirement estimates. The pH measurement error decreases exponentially with increasing soil moisture and increases with decreasing MPD. Using a knee point detection, reliable pH values were obtained for SMC > 11 %, irrespective of the pH ISE used. An analysis of the regression coefficients of the fitted exponential model showed that the maximum pH increase also depends on soil texture; i.e., the influence of soil moisture variation on the pH value increases with decreasing MPD. Moreover, the concavity of the exponential curve increases with decreasing MPD.
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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