Shandong Peanut Research Institute, Qingdao, 266100, China.
Dongying Meteorological Bureau of Shandong Province, Dongying, 257091, China.
BMC Plant Biol. 2024 Oct 30;24(1):1029. doi: 10.1186/s12870-024-05745-7.
BACKGROUND: This study clarified the synergistic relationship among annual changes to specify the changes in agro-meteorological factors, soil characteristics and peanut growth in saline-alkali land near the estuary of the Yellow River Delta. We aimed to find the key factors affecting peanut production to optimize and regulate peanut planting mode in saline alkali soil. RESULTS: The daily average temperature from early May to late September in Lijin and Kenli was above 24 °C, with 470-600 mm of precipitation. The sunshine duration was 7.9 h/day and 7.3 h/day and the accumulated temperature was 3742 °C and 3809 °C, in Lijin and Kenli, respectively. Agro-meteorological conditions were suitable for peanut growth and development with the consistent main developmental period in the two experiment regions. The best sowing period was when the soil temperature stabilized above 18 °C in early May, and the best harvest was in mid-September. The soil volumetric water content in Lijin concentrated among 25-40%. Salt was mainly distributed in the 40-60 cm soil layers, and increased rapidly to 2.5 g kg in 0-20 cm cultivation layer in mid-May due to lack of precipitation. In Kenli experiment region, the soil volumetric water content ranged from 10 to 35%. Soil salinity was mainly distributed in the 20 cm soil layer, and the changes in salinity was little affected by precipitation. From mid-July to mid-August, the effective accumulated temperature of 5 cm soil layer was above 520 °C in both regions, which could ensure the normal pod development. The slow dynamic growth of kernel, high unfilled pod rate (26.99%) and low shelling rate (66.0%) might be the main reasons for low peanut yield in Lijin. CONCLUSION: Soil salinity was the main factor affecting pod development and yield. It was also a key point in optimizing the peanut planting mode in the saline alkali land of the Yellow River Delta.
背景:本研究阐明了黄河三角洲河口附近盐碱地农业气象因素、土壤特性和花生生长年际变化的协同关系,旨在找到影响花生产量的关键因素,优化和调控盐碱地花生种植模式。
结果:利津和垦利 5 月下旬至 9 月下旬日平均气温均在 24°C 以上,降雨量 470-600mm,日照时数 7.9h/d、7.3h/d,积温 3742°C、3809°C。两试验区农业气象条件均适宜花生生长发育,主生育期一致。最佳播种期为 5 月初土壤温度稳定在 18°C 以上,最佳收获期为 9 月中旬。利津土壤体积含水量集中在 25-40%之间,5 月中旬由于降水少,盐分主要分布在 40-60cm 土层中,迅速增加到 0-20cm 耕作层 2.5g/kg。垦利试验区土壤体积含水量在 10-35%之间,土壤盐分主要分布在 20cm 土层中,受降水影响较小。7 月中旬至 8 月中旬,两试验区 5cm 土层有效积温均在 520°C 以上,可保证正常荚果发育。利津区花生果仁缓慢动态生长,空秕率高(26.99%),脱壳率低(66.0%),可能是花生产量低的主要原因。
结论:土壤盐分是影响荚果发育和产量的主要因素,也是优化黄河三角洲盐碱地花生种植模式的关键。
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