Puppe Daniel, Busse Jacqueline, Stein Mathias, Kaczorek Danuta, Buhtz Christian, Schaller Jörg
Leibniz Centre for Agricultural Landscape Research (ZALF), 15374 Müncheberg, Germany.
Soil Science and Soil Protection, Martin Luther University Halle-Wittenberg, 06120 Halle (Saale), Germany.
Biology (Basel). 2024 Oct 16;13(10):828. doi: 10.3390/biology13100828.
The potato is the most important non-cereal food crop, and thus improving potato growth and yield is the focus of agricultural researchers and practitioners worldwide. Several studies reported beneficial effects of silicon (Si) fertilization on potato performance, although plant species from the family Solanaceae are generally considered to be non-Si-accumulating. We used results from two field experiments in the temperate zone to gain insight into silica accumulation in potato plants, as well as corresponding long-term potato yield performance. We found relatively low Si contents in potato leaves and roots (up to 0.08% and 0.3% in the dry mass, respectively) and negligible Si contents in potato tuber skin and tuber flesh for plants grown in soils with different concentrations of plant-available Si (field experiment 1). Moreover, potato yield was not correlated to plant-available Si concentrations in soils in the long term (1965-2015, field experiment 2). Based on our results, we ascribe the beneficial effects of Si fertilization on potato growth and yield performance reported in previous studies mainly to antifungal/osmotic effects of foliar-applied Si fertilizers and to changes in physicochemical soil properties (e.g., enhanced phosphorus availability and water-holding capacity) caused by soil-applied Si fertilizers.
马铃薯是最重要的非谷类粮食作物,因此提高马铃薯的生长和产量是全球农业研究人员和从业者关注的焦点。多项研究报告了硅(Si)肥对马铃薯生长表现的有益影响,尽管茄科植物通常被认为是非硅积累植物。我们利用温带地区两个田间试验的结果,来深入了解马铃薯植株中的硅积累情况以及相应的马铃薯长期产量表现。对于在不同有效硅浓度土壤中生长的植株,我们发现马铃薯叶片和根系中的硅含量相对较低(干重中分别高达0.08%和0.3%),马铃薯块茎表皮和块茎肉中的硅含量可忽略不计(田间试验1)。此外,从长期来看(1965 - 2015年,田间试验2),马铃薯产量与土壤中有效硅浓度无关。基于我们的研究结果,我们认为先前研究中报道的硅肥对马铃薯生长和产量表现的有益影响,主要归因于叶面施用硅肥的抗真菌/渗透效应以及土壤施用硅肥引起的土壤理化性质变化(例如,提高了磷的有效性和持水能力)。