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BASIC CATION SATURATION RATIO THEORY APPLIED TO SAND-BASED PUTTING GREENS

机译:应用于沙质果岭的基本阳离子饱和比理论

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The basic cation saturation ratio theory of soil test interpretation states that calcium (Ca),magnesium (Mg),and potassium (K) should be present on the cation exchange sites of the soil in the following percentages,65 – 85%,6 – 12% and 1 – 5%,respectively.Golf course putting greens are often constructed utilizing a sand-based rootzone.Since sands generally have a low cation exchange capacity (CEC),it is possible that the Ca,Mg,and K cations can occupy the correct ratios within the rootzone yet fail to support optimal growth.Also,the validity of these cation ratios has not been thoroughly evaluated for creeping bentgrass on low CEC soil media.The objective of this research was to evaluate the BCSR theory for sand-based greens.Twenty-eight cation treatments of widely varying cation ratios were applied to 'Penncross' creeping bentgrass (Agrostis stolonifera L.) established on either calcareous or silica sand.Creeping bentgrass tolerated a wide range of applied cation ratios,as no differences in quality or growth rate were observed among the 28 treatments.Samples from the silica sand pots had high K saturation percentages,>28%,but leaf and soil extractable K concentrations were very low,<21 g?kg-1 and <1.6 mg?kg-1,respectively.The Ca:K ratios of silica sand ranged from 1:1 to 2:1,whereas; according to the BCSR theory,they should be 13:1 and a Ca application would be recommended to correct the ratio.However,leaf Ca concentrations from grass grown on silica sand were high (12 g?kg-1) and leaf K concentrations were low (8.7 g?kg-1).Dissolution of CaCO3 from calcareous sand samples resulted in Ca saturations percentages greater than 95%.Additionally,the silica sand samples had such low CEC that calculated cation saturation percentages and ratios gave misleading results.Using the BCSR theory on low CEC sands results in widely varying cation saturation ratios that may lead to erroneous interpretations of soil test results.It is recommended that the results of BCSR interpretation not be used as the final determining factor in developing fertility systems for sand-based golf course greens.
机译:土壤测试解释的基本阳离子饱和比理论指出,钙(Ca),镁(Mg)和钾(K)应以以下百分比出现在土壤的阳离子交换部位:65 – 85%,6 –高尔夫球推杆果岭通常使用基于沙子的根部区域建造。分别为12%和1 – 5%。由于沙子通常具有较低的阳离子交换容量(CEC),因此Ca,Mg和K阳离子可能阳离子比率在根区中占据正确的比例,却不能支持最佳的生长。此外,对于阳离子交换比率低的CEC土壤介质上蠕动的草根,这些阳离子比率的有效性尚未得到充分评估。对在钙质或硅砂上建立的'Penncross'爬行草(Agrostis stolonifera L.)进行了二十种阳离子比例的阳离子处理。在28种处理中观察到质量或生长速率的降低。来自硅砂罐的样品的钾饱和度百分比高,> 28%,但叶和土壤中可提取的钾浓度非常低,<21 g?kg-1和<1.6。硅砂的Ca:K比范围为1:1至2:1。根据BCSR理论,该比例应为13:1,建议使用Ca来校正该比例。但是,在硅砂上生长的草叶中的Ca含量较高(12 g?kg-1),叶中的K含量较高。低(8.7 g?kg-1)。从钙质砂样品中溶解CaCO3导致Ca饱和度百分比大于95%。此外,硅砂样品的CEC非常低,因此计算出的阳离子饱和度百分比和比例产生了误导性的结果。低CEC砂的BCSR理论导致阳离子饱和比变化很大,可能会导致对土壤测试结果的错误解释。建议不要将BCSR解释的结果作为开发砂基高尔夫球肥力系统的最终决定因素当然是果岭。

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