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Temperature limitations in the use of hydrogels on leptosols in a semi-arid region of Brazil
Geoderma Regional ( IF 4.1 ) Pub Date : 2021-06-05 , DOI: 10.1016/j.geodrs.2021.e00407
Carla Danielle Vasconcelos do Nascimento , Jaedson Cláudio Anunciato Mota , Ícaro Vasconcelos do Nascimento , Gustavo Henrique da Silva Albuquerque , Robert William Simmons , Carlos Tadeu dos Santos Dias , Mirian Cristina Gomes Costa

Due to their high-water retention capacity, hydrogels are considered promising soil conditioners to improve soil plant available water content in semi-arid environments; however, little is known about how soil temperature affects the functionality of hydrogels. In this study, the effect of soil temperature on physical attributes of soil amended with a Acrylamide-co-Potassium Acrylate hydrogel was evaluated. A laboratory experiment was installed in a scheme (4 × 4) x 4 - four soil temperatures (30, 45, 65 and 105 °C), four exposure times (40, 70, 100, and 130 days) with four repetitions. The test soil was a Leptsol with sandy loam texture and of the hydrogel was applied at a dose of 0.1% w w−1. Soil moisture at field capacity (θFC) and permanent wilting point (θWP), plant available water (AW), bulk density (BD), and soil porosity were evaluated. The resulting data was subjected to two-way analysis of variance. The hydrogel increased the θFC of the soil, from 0.14 to 0.19 m3 m−3 at 45 °C and 56 days. At 40 days, a minimum θWP (0.05 m3 m−3) was observed at 92 °C. In general, θFC increased, while the θWP decreased, providing improved soil water storage. Plant available water was up to three times higher in soil with hydrogel across a temperature range of 30–105 °C. In all treatments irrespective of temperature and exposure time, the soil BD and porosity were improved in comparison to the un-amended control. This constitutes an advantage in the use of the hydrogel as a soil conditioner. Even with the interaction of abiotic factors acting on the hydrogel, there are beneficial effects on the water storage capacity, soil BD, and soil porosity.



中文翻译:

在巴西半干旱地区使用水凝胶对 leptosols 的温度限制

由于其高保水能力,水凝胶被认为是有前途的土壤调节剂,可改善半干旱环境中土壤植物的可用水分含量;然而,人们对土壤温度如何影响水凝胶的功能知之甚少。在这项研究中,评估了土壤温度对用丙烯酰胺--丙烯酸钾水凝胶改性的土壤物理属性的影响。实验室实验以 (4 × 4) x 4 方案安装 - 四个土壤温度(30、45、65 和 105 °C),四个暴露时间(40、70、100 和 130 天),重复四次。测试土壤是具有砂质壤土质地的 Leptsol,并且以 0.1% ww -1的剂量施用水凝胶。田间持水量土壤水分 (θ FC) 和永久枯萎点 (θ WP )、植物有效水 (AW)、容重 (BD) 和土壤孔隙度。对所得数据进行双向方差分析。水凝胶使土壤的 θ FC在 45°C 和 56 天时从 0.14 增加到 0.19 m 3  m -3。在 40 天时,在 92 °C 时观察到最小 θ WP (0.05 m 3  m -3 )。一般来说,θ FC增加,而 θ WP减少,改善土壤储水量。在 30–105 °C 的温度范围内,使用水凝胶的土壤中植物可用水量高出三倍。在所有处理中,无论温度和暴露时间如何,与未修改的对照相比,土壤 BD 和孔隙率都有所改善。这构成了使用水凝胶作为土壤调节剂的优势。即使非生物因素作用于水凝胶,也会对蓄水能力、土壤 BD 和土壤孔隙度产生有益影响。

更新日期:2021-06-10
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