Estimation of water consumption as affected by measurement locations of soil water content in drip irrigated tomato in solar greenhouses

Q3 Agricultural and Biological Sciences
Zhao Weixi
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引用次数: 2

Abstract

Placements of soil moisture sensor have been key considerations in obtaining representative soil water content in crop root zones for irrigation schedules. In this article, the distribution of soil water content in the wetted volume from a line source was studied in drip irrigated tomato in solar greenhouse condition. Through comparison of tomato water consumption determined from measured water content by moisture sensors at different locations, suitable placements of sensors were discussed. The results indicated that irrigation quota range of 14 25 mm increased soil water content in the 0 40 cm soil layer, and daily mean soil water content in wetted soil volume was 75% 100% field capacity throughout tomato growth season. Wetted soil volumes generated by adjacent emitters along the drip lines fully overlapped after several sequential irrigation events, forming lateral zones with approximately uniform distribution of water content around the drip lines. There was no significant difference between mean soil water content along the depth of 0 40 cm layer. The variation tendency of soil water content with time at different horizontal locations from drip lines was synchronous in character, without any obvious hysteresis quality. Assuming that the 0 40 cm layer was the root zone with 80% root concentrated, an irrigation quota range of 14 25 mm caused deep percolation from the bottom of the root zone with a certain spatial variability. Seasonal deep percolation accounted for 13% of irrigation amount during tomato growth season. The differences in tomato water consumption at different locations from drip lines were within 10%, except for the seedling and blossom fruiting stages. The experimental results suggested that high frequency drip irrigation sustained suitable soil water condition in the root zone. One profile of soil water content measured in the proximity of drip lines was adequate for the proper estimation of water consumption of drip irrigated tomato in solar greenhouse conditions.
日光温室滴灌番茄土壤含水量测定位置对耗水量的影响
土壤水分传感器的放置是获得作物根区代表性土壤含水量的关键考虑因素。本文研究了日光温室条件下滴灌番茄线源湿润体积土壤含水量的分布规律。通过对不同位置水分传感器测得的番茄耗水量进行比较,探讨了传感器的适宜放置位置。结果表明:14 ~ 25 mm灌水定额范围可提高0 ~ 40 cm土层土壤含水量,整个番茄生长期湿润土壤体积日平均含水量为75% ~ 100%大田容量;在连续几次灌溉后,沿滴灌管道相邻的发射器产生的湿土体积完全重叠,在滴灌管道周围形成了含水量分布近似均匀的横向区域。在0 ~ 40 cm土层,土壤平均含水量差异不显著。不同水平位置土壤含水量随时间的变化趋势具有同步性,不存在明显的滞后性。假设0 ~ 40 cm层为根区,根系集中80%,14 ~ 25 mm的灌溉定额范围内,从根区底部深层渗透,具有一定的空间变异性。季节性深渗占番茄生长期灌水量的13%。除苗期和开花结实期外,不同地点番茄耗水量差异在10%以内。试验结果表明,高频滴灌维持了根区适宜的土壤水分条件。在滴灌管道附近测量的土壤含水量剖面足以正确估计日光温室条件下滴灌番茄的耗水量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Chinese Journal of Eco-agriculture
Chinese Journal of Eco-agriculture Environmental Science-Ecology
CiteScore
2.70
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0.00%
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