{"title":"地面蛇纹石和地面镁灰岩作为油棕苗木镁源的评价","authors":"M. J., NG J Y, M. S, K. O J","doi":"10.56333/tp.2022.006","DOIUrl":null,"url":null,"abstract":"Treatment of ground magnesium limestone and ground serpentine by boiling in 5 ml of concentrated nitric (HNO3) acid and 10 ml of concentrated hydrochloric (HCl) acid for 1, 2, 4, 8 and 16 hours in the laboratory showed mean magnesium oxide (MgO) content of 18.2 and 29.20 per cent, respectively. The experiment for the two sources of magnesium (Mg) was carried out on oil palm nursery seedlings grown in large polybags with coarse river sand as the medium of growth. The rates were 5, 10, 20 and 30 g of MgO, applied in planting holes at the time of transplanting of three-month-old pre-nursery seedlings. Initially, up to four months, the leaf 3 Mg levels were slightly higher in ground serpentine treatment, although the difference in values was statistically not significant when compared to the rest of the treatments. As the age of the seedlings increased, there was a continuous decline in leaf Mg levels for all treatments. At the eighth month, the Mg levels of oil palm leaves grown with ground magnesium limestone were significantly higher than the control treatment with no Mg. The source of Mg had no influence on the vegetative growth of seedlings, as all the treatments including control showed no significant differences for the measured growth parameters. In conclusion, ground serpentinite rock is comparable to ground magnesium limestone as a source of Mg. The rate of 30 g MgO per plant, when placed in the planting hole, is insufficient to meet the oil palm needs after the fourth month of application. Higher rates or different methods of application may be needed and to be studied in subsequent trials.","PeriodicalId":22956,"journal":{"name":"The Planter","volume":"26 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-05-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"EVALUATION OF GROUND SERPENTINE ROCK AND GROUND MAGNESIUM LIMESTONE AS MAGNESIUM SOURCES FOR OIL PALM NURSERY SEEDLINGS\",\"authors\":\"M. J., NG J Y, M. S, K. O J\",\"doi\":\"10.56333/tp.2022.006\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Treatment of ground magnesium limestone and ground serpentine by boiling in 5 ml of concentrated nitric (HNO3) acid and 10 ml of concentrated hydrochloric (HCl) acid for 1, 2, 4, 8 and 16 hours in the laboratory showed mean magnesium oxide (MgO) content of 18.2 and 29.20 per cent, respectively. The experiment for the two sources of magnesium (Mg) was carried out on oil palm nursery seedlings grown in large polybags with coarse river sand as the medium of growth. The rates were 5, 10, 20 and 30 g of MgO, applied in planting holes at the time of transplanting of three-month-old pre-nursery seedlings. Initially, up to four months, the leaf 3 Mg levels were slightly higher in ground serpentine treatment, although the difference in values was statistically not significant when compared to the rest of the treatments. As the age of the seedlings increased, there was a continuous decline in leaf Mg levels for all treatments. At the eighth month, the Mg levels of oil palm leaves grown with ground magnesium limestone were significantly higher than the control treatment with no Mg. The source of Mg had no influence on the vegetative growth of seedlings, as all the treatments including control showed no significant differences for the measured growth parameters. In conclusion, ground serpentinite rock is comparable to ground magnesium limestone as a source of Mg. The rate of 30 g MgO per plant, when placed in the planting hole, is insufficient to meet the oil palm needs after the fourth month of application. Higher rates or different methods of application may be needed and to be studied in subsequent trials.\",\"PeriodicalId\":22956,\"journal\":{\"name\":\"The Planter\",\"volume\":\"26 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-05-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The Planter\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.56333/tp.2022.006\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Planter","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.56333/tp.2022.006","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
磨碎的镁石灰石和磨碎的蛇纹石在实验室中分别用5毫升浓硝酸和10毫升浓盐酸煮沸1、2、4、8和16小时,平均氧化镁含量分别为18.2%和29.20%。以油棕苗木为研究对象,以粗河砂为生长介质,在大塑料袋中进行两种镁源的育苗试验。在3月龄苗木移栽时,分别施用5、10、20和30 g MgO。最初,在4个月时,地面蛇纹石处理的叶片3mg水平略高,尽管与其他处理相比,差异在统计学上不显著。随着幼苗年龄的增长,各处理的叶片Mg含量均呈持续下降趋势。在第8个月,磨镁石灰处理油棕叶片的镁含量显著高于不加镁的对照处理。Mg的来源对幼苗的营养生长没有影响,包括对照在内的所有处理对测量的生长参数没有显著差异。综上所述,地面蛇纹岩与地面镁灰岩作为镁的来源是相当的。在种植孔中,每株30克MgO的用量不足以满足油棕在施用第四个月后的需求。可能需要更高的速率或不同的施用方法,并在随后的试验中进行研究。
EVALUATION OF GROUND SERPENTINE ROCK AND GROUND MAGNESIUM LIMESTONE AS MAGNESIUM SOURCES FOR OIL PALM NURSERY SEEDLINGS
Treatment of ground magnesium limestone and ground serpentine by boiling in 5 ml of concentrated nitric (HNO3) acid and 10 ml of concentrated hydrochloric (HCl) acid for 1, 2, 4, 8 and 16 hours in the laboratory showed mean magnesium oxide (MgO) content of 18.2 and 29.20 per cent, respectively. The experiment for the two sources of magnesium (Mg) was carried out on oil palm nursery seedlings grown in large polybags with coarse river sand as the medium of growth. The rates were 5, 10, 20 and 30 g of MgO, applied in planting holes at the time of transplanting of three-month-old pre-nursery seedlings. Initially, up to four months, the leaf 3 Mg levels were slightly higher in ground serpentine treatment, although the difference in values was statistically not significant when compared to the rest of the treatments. As the age of the seedlings increased, there was a continuous decline in leaf Mg levels for all treatments. At the eighth month, the Mg levels of oil palm leaves grown with ground magnesium limestone were significantly higher than the control treatment with no Mg. The source of Mg had no influence on the vegetative growth of seedlings, as all the treatments including control showed no significant differences for the measured growth parameters. In conclusion, ground serpentinite rock is comparable to ground magnesium limestone as a source of Mg. The rate of 30 g MgO per plant, when placed in the planting hole, is insufficient to meet the oil palm needs after the fourth month of application. Higher rates or different methods of application may be needed and to be studied in subsequent trials.