Effect of different types of soil tillage for sunflower on some soil physical characteristics. Part I: soil moisture

Q3 Agricultural and Biological Sciences
Helia Pub Date : 2021-05-03 DOI:10.1515/helia-2020-0012
P. Yankov, M. Drumeva
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引用次数: 1

Abstract

Abstract The investigation was carried out during 2014–2016 in the land of General Toshevo town in the South Dobrudzha region on slightly leached chernozem soil type. The effect of the types of soil tillage for sunflower given bellow was followed: ploughing at 24–26 cm, chisel-plough at 24–26 cm, disking with disk harrow at 10–12 cm and direct sowing (no-tillage) on the soil moisture content. Based on bulk density, wilting point and the determined soil moisture content the plant-available water was calculated. The additional soil tilths of the areas subjected to ploughing, chisel-ploughing and disking with disc harrow included double spring pre-sowing cultivation with harrowing. To destroy the emerging weeds in the variant with direct sowing, a total herbicide was applied. The soil moisture content was evaluated during three main stages of sunflower development: emergence, flowering and technical maturity. The investigated parameter was determined for each of the studied layers – 0–10, 10–20, 20–30, 30–40 and 40–60 cm. In years with normal amounts of rainfalls, no significant differences in the soil moisture under the different ways of soil tillage were observed. Conventional ploughing and tillage without turning of the soil layer contributed to accumulation of more moisture and to higher moisture storage down the soil profile under heavy and intensive rainfalls. Tillage without turning of the soil layer, minimal and no tillage maintained more and better soil moisture in years with limited precipitation and in periods of drought.
向日葵不同耕作方式对土壤某些物理特性的影响。第一部分:土壤湿度
2014-2016年在南多勃鲁扎地区托舍沃将军镇土地上进行了轻度淋溶黑钙土类型调查。土壤耕作方式对向日葵土壤含水量的影响为:24 ~ 26 cm翻耕、24 ~ 26 cm凿犁、10 ~ 12 cm盘耙和免耕直播。根据容重、凋萎点和测定的土壤含水量计算植物有效水分。犁耕、凿耕和盘耙耕区的额外土壤耕度包括双春播前耙耕。采用全除草剂直接播种的方法,对异种杂草进行灭除。对向日葵出苗期、开花期和技术成熟期三个主要发育阶段土壤水分含量进行了评价。每个研究层(0-10、10-20、20-30、30-40和40-60 cm)的研究参数都被确定。在降雨量正常的年份,不同耕作方式下的土壤湿度无显著差异。在强降雨条件下,不翻土的常规耕作和耕作有助于积累更多的水分,并提高土壤剖面的水分储存。免翻耕、少耕和免耕在降水有限的年份和干旱时期保持了更多、更好的土壤水分。
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
Helia
Helia Agricultural and Biological Sciences-Agronomy and Crop Science
CiteScore
1.00
自引率
0.00%
发文量
9
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