Neugschwandtner Reinhard W, Száková Jiřina, Pachtrog Vera, Tlustoš Pavel, Kulhánek Martin, Černý Jindřich, Kaul Hans-Peter, Wagentristl Helmut, Moitzi Gerhard, Euteneuer Pia
Institute of Agronomy, Department of Crop Sciences, University of Natural Resources and Life Sciences Vienna (BOKU), Konrad-Lorenz-Straße 24, 3430 Tulln, Austria.
Department of Agro-Environmental Chemistry and Plant Nutrition, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Kamýcká 129, 165 21 Prague, Czech Republic.
Plants (Basel). 2022 Feb 21;11(4):565. doi: 10.3390/plants11040565.
The status of macronutrients phosphorus (P), potassium (K), sulphur (S), calcium (Ca) and magnesium (Mg) was assessed 15 years after the establishment of a long-term crop rotation and soil tillage trial with mouldboard ploughing (MP), no-till (NT), deep conservation tillage (CTd) and shallow conservation tillage (CTs). The mobile proportions of macronutrients in an Austrian Chernozem soil were determined to a depth of 50 cm with the single reagent extractant acetic acid (AA) and Mehlich 3 (M3), which uses several reagents as extractants. AA revealed less P and K, but more Ca and Mg compared to M3. Both extractants could capture the distribution pattern of the nutrients in the soil profile, but M3 showed higher differences among the soil layers. In the first 5 cm in NT, the P concentration was higher than in MP, CTd and CTs. The concentration of K was higher in NT, CTd and CTs than in MP in the first 10 cm of the soil. Phosphorus and K concentrations did not differ between tillage treatments below these soil layers, and S, Ca and Mg were similar in all soil layers. As none of the analysed elements except for Ca were fertilized and no accumulation of S, Ca and Mg was observed in the upper soil layer, the higher concentrations are attributed to accumulation through crop residues and then less leaching of P and K. Crop rotation did not affect the distribution of the analysed macronutrients in the soil but affected the nutrient uptake by winter wheat mostly due to the yield differences of winter wheat in the two crop rotations.
在一项长期作物轮作和土壤耕作试验开展15年后,对大量元素磷(P)、钾(K)、硫(S)、钙(Ca)和镁(Mg)的状况进行了评估。该试验采用了铧式犁翻耕(MP)、免耕(NT)、深松保墒耕作(CTd)和浅松保墒耕作(CTs)。使用单一试剂提取剂乙酸(AA)和使用多种试剂作为提取剂的Mehlich 3(M3),测定了奥地利黑钙土中大量元素在50厘米深度内的移动比例。与M3相比,AA显示出更少的P和K,但更多的Ca和Mg。两种提取剂都能捕捉到土壤剖面中养分的分布模式,但M3在各土层间显示出更大的差异。在免耕的前5厘米,P浓度高于铧式犁翻耕、深松保墒耕作和浅松保墒耕作。在土壤的前10厘米,免耕、深松保墒耕作和浅松保墒耕作中的K浓度高于铧式犁翻耕。在这些土层以下,不同耕作处理的P和K浓度没有差异,所有土层中的S、Ca和Mg含量相似。由于除Ca外的所有分析元素均未施肥,且在上层土壤中未观察到S、Ca和Mg的积累,较高的浓度归因于作物残茬的积累以及随后P和K较少的淋溶。作物轮作并未影响所分析的大量元素在土壤中的分布,但主要由于两种作物轮作中冬小麦产量的差异,影响了冬小麦对养分的吸收。