Steps toward an integrated soil water tension and osmotic tension sensor

IF 2.4 3区 农林科学 Q2 SOIL SCIENCE Soil Science Society of America Journal Pub Date : 2024-08-30 DOI:10.1002/saj2.20749
Martin S. Goodchild
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Abstract

The two most important abiotic plant stressors that impact plant development and crop yields are water stress and salinity stress. These issues are particularly important in arid and semi‐arid regions. According to a 2019 research paper, “thirty crop species provide 90% of our food, most of which display severe yield losses under moderate salinity.” Moderate salinity is defined as extracted pore‐water salinity in the range of 4–8 dS m−1. Currently, commercially available soil moisture and bulk soil electrical conductivity sensors can estimate in situ soil pore‐water electrical conductivity with suitably calibrated soil moisture and electrical conductivity models for a wide range of soil types and growing media. With knowledge of the pore‐water electrical conductivity it is possible to estimate osmotic tension. Furthermore, there are commercially available dielectric tensiometers that provide soil water tension measurements from the water content of a porous matrix component that is in equilibrium with the water capillary forces in the surrounding soil or growing media. Combining soil moisture and soil water tension measurements enables water retention curves and the hydraulic properties of a soil to be determined. However, the overall ability of a plant to extract water from a soil or substrate is typically dominated by water tension and osmotic tension. Currently, while the technology blocks exist in different commercial offerings, the combination of a water tension and osmotic tension in an integrated sensor does not exist. A key benefit of the porous matrix in a dielectric tensiometer is that electrical measurements include a component of extracted water from the soil or growing media. With the appropriate dielectric characterization of the porous matrix, there should be no need for soil‐specific calibrations. The aim of the paper is to outline the measurement processing that could be implemented into an integrated water tension and osmotic tension sensor.
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向集成式土壤水分张力和渗透张力传感器迈进
影响植物生长和作物产量的两个最重要的非生物植物胁迫因素是水分胁迫和盐分胁迫。这些问题在干旱和半干旱地区尤为重要。根据 2019 年的一份研究论文,"30 种作物提供了我们 90% 的食物,其中大多数在中度盐度条件下会出现严重的产量损失"。中度盐度的定义是提取的孔隙水盐度在 4-8 dS m-1 之间。目前,市场上销售的土壤水分和大体积土壤电导率传感器可以利用经过适当校准的土壤水分和电导率模型来估算原位土壤孔隙水电导率,适用于多种土壤类型和生长介质。有了孔隙水导电率的知识,就可以估算渗透张力。此外,市场上还有介电张力仪,可通过多孔基质成分的含水量测量土壤水张力,该基质成分与周围土壤或生长介质中的毛细水力处于平衡状态。结合土壤水分和土壤水张力测量结果,可以确定土壤的保水曲线和水力特性。不过,植物从土壤或基质中汲取水分的整体能力通常由水张力和渗透张力主导。目前,虽然不同的商业产品中都有这些技术模块,但还没有将水张力和渗透张力结合在一起的集成传感器。介电张力仪中多孔基质的一个主要优点是,电测量包括从土壤或生长介质中提取的水分。只要对多孔基体进行适当的介电特性分析,就不需要针对特定土壤进行校准。本文旨在概述可在集成式水张力和渗透张力传感器中采用的测量处理方法。
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来源期刊
Soil Science Society of America Journal
Soil Science Society of America Journal 农林科学-土壤科学
CiteScore
5.40
自引率
3.40%
发文量
130
审稿时长
3.6 months
期刊介绍: SSSA Journal publishes content on soil physics; hydrology; soil chemistry; soil biology; soil biochemistry; soil fertility; plant nutrition; pedology; soil and water conservation and management; forest, range, and wildland soils; soil and plant analysis; soil mineralogy, wetland soils. The audience is researchers, students, soil scientists, hydrologists, pedologist, geologists, agronomists, arborists, ecologists, engineers, certified practitioners, soil microbiologists, and environmentalists. The journal publishes original research, issue papers, reviews, notes, comments and letters to the editor, and book reviews. Invitational papers may be published in the journal if accepted by the editorial board.
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