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Biochar increases plant-available water in a sandy loam soil under an aerobic rice crop system.

机译:在有氧水稻作物系统下,生物炭增加了砂壤土中植物的水分利用率。

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摘要

The main objective of this study was to assess the impact of biochar rate (0, 8, 16 and 32 Mg ha-1) on the water retention capacity (WRC) of a sandy loam Dystric Plinthosol. The applied biochar was a by-product of slow pyrolysis (~450 °C) of eucalyptus wood, milled to pass through a 2000 micrometers sieve that resulted in a material with an intrinsic porosity less than or equal to 10 micrometers and a specific surface area of ~3.2 m2 g-1. The biochar was incorporated into the top 15 cm of the soil under an aerobic rice system. Our study focused on both the effects on WRC and rice yields 2 and 3 years after its application. Undisturbed soil samples were collected from 16 plots in two soil layers (5-10 and 15-20 cm). Soil water retention curves were modelled using a nonlinear mixed model which appropriately accounts for uncertainties inherent of spatial variability and repeated measurements taken within a specific soil sample. We found an increase in plant-available water in the upper soil layer proportional to the rate of biochar, with about 0.8% for each Mg ha-1 biochar amendment 2 and 3 years after its application. The impact of biochar on soil WRC was most likely related to an effect in overall porosity of the sandy loam soil, which was evident from an increase in saturated soil moisture and macro porosity with 0.5 and 1.6% for each Mg ha-1 of biochar applied, respectively. The increment in soil WRC did not translate into an increase in rice yield, essentially because in both seasons the amount of rainfall during the critical period for rice production exceeded 650 mm. The use of biochar as a soil amendment can be a worthy strategy to guarantee yield stability under short-term water-limited conditions. Our findings raise the importance of assessing the feasibility of very high application rates of biochar and the inclusion of a detailed analysis of its physical and chemical properties as part of future investigations.
机译:这项研究的主要目的是评估生物炭速率(0、8、16和32 Mg ha-1)对砂壤土Dystric Plinthosol的保水能力(WRC)的影响。施加的生物炭是桉木缓慢热解(〜450°C)的副产品,经过研磨可通过2000微米的筛子,产生的材料的固有孔隙率小于或等于10微米,比表面积约3.2平方米g-1。在有氧水稻系统下,将生物炭掺入土壤的顶部15厘米。应用后的2年和3年,我们的研究集中于对WRC和水稻产量的影响。从两个土壤层(5-10和15-20 cm)的16个样地中收集未受干扰的土壤样品。使用非线性混合模型对土壤保水曲线建模,该模型适当考虑了空间变异性固有的不确定性以及在特定土壤样品中进行的重复测量。我们发现,上层土壤中植物可用水的增加与生物炭的比例成正比,应用后2年和3年,每Mg ha-1生物炭改良剂的利用率约为0.8%。生物炭对土壤WRC的影响最有可能与沙壤土的整体孔隙率有关,这可以从饱和土壤水分和大孔隙率的增加中看出,每施用1 Mg ha-1的生物炭,其饱和度分别为0.5%和1.6% , 分别。土壤WRC的增加并未转化为水稻产量的增加,这主要是因为在两个季节中,水稻生产关键时期的降雨量均超过650 mm。使用生物炭作为土壤改良剂可以是一种在短期缺水条件下保证产量稳定的有价值的策略。我们的发现提高了评估非常高的生物炭施用量的可行性的重要性,并提出了对其物理和化学特性的详细分析作为未来研究的一部分。

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