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新乡市大棚菜田土壤养分及盐分的演变
引用本文:陈碧华,孙 丽,李新峥,王广印,李亚灵.新乡市大棚菜田土壤养分及盐分的演变[J].农业工程学报,2013,29(15):83-90.
作者姓名:陈碧华  孙 丽  李新峥  王广印  李亚灵
作者单位:1. 河南科技学院园艺园林学院,新乡 453003;1. 河南科技学院园艺园林学院,新乡 453003;1. 河南科技学院园艺园林学院,新乡 453003;1. 河南科技学院园艺园林学院,新乡 453003;2. 山西农业大学园艺学院,太谷 030801
基金项目:河南省重大科技攻关项目(092101310300);河南省大宗蔬菜产业技术体系建设专项(112102310378)资金资助。
摘    要:为了研究大棚菜田土壤养分及盐分演变特征,采集了不同种植年限(0、5、10、15、20、25、30a)的大棚菜田0~20、>20~40cm土壤样品,测定了主要土壤养分指标、水溶性盐分以及土壤pH值。结果表明:新乡市大棚菜田土壤的培肥期在0~15a,培肥后(15a)土壤有机质质量分数在30g/kg以上,达到较理想状态,碱解氮和速效磷含量表现为富集,质量分数分别在150、90g/kg以上。但是速效钾却在100g/kg以下,较缺乏,并且15a以后还在继续流失。各养分含量随着土壤深度的增加逐渐下降。土壤碱解氮、速效磷含量与有机质呈极显著相关。新乡市大棚菜田土壤中氮磷钾的比例严重失调,出现磷素过量而钾素供应严重不足。土壤盐渍化从大棚种植15a开始发生,与种植年限呈极显著正相关,并且与土壤pH值下降表现同步性。该研究结论期望给新乡市蔬菜大棚土壤的施肥决策提供参考。

关 键 词:耕种  土壤  pH值  种植年限  大棚菜田  土壤肥力  盐渍化
收稿时间:2012/11/20 0:00:00
修稿时间:2013/7/15 0:00:00

Evolution of soil nutrient and salts in vegetable field ofgreenhouse in Xinxiang
Chen Bihu,Sun Li,Li Xinzheng,Wang Guangyin and Li Yaling.Evolution of soil nutrient and salts in vegetable field ofgreenhouse in Xinxiang[J].Transactions of the Chinese Society of Agricultural Engineering,2013,29(15):83-90.
Authors:Chen Bihu  Sun Li  Li Xinzheng  Wang Guangyin and Li Yaling
Institution:1. College of Horticulture and Landscape, Henan Institute of Science and Technology, Xinxiang 453003, China;1. College of Horticulture and Landscape, Henan Institute of Science and Technology, Xinxiang 453003, China;1. College of Horticulture and Landscape, Henan Institute of Science and Technology, Xinxiang 453003, China;1. College of Horticulture and Landscape, Henan Institute of Science and Technology, Xinxiang 453003, China;2. College of Horticulture, Shanxi Agricultural University, Taigu 030801, China
Abstract:Abstract: The production history of greenhouse was more than 30 years in Muye vegetable production base in Henan Xinxiang. The main planting pattern of this region was wheat and maize rotation before building a greenhouse, but now it is the production of cucumbers and tomatoes in a greenhouse in spring and autumn. In order to study the evolution characteristics of soil fertility and salt of the vegetable field in the greenhouse, the soil sample of the vegetable field in the greenhouse (0-20, >20-40 cm) in different cultivating years (0, 5, 10, 15, 20, 25, and 30) were collected and the main soil fertility index and soluble salt and soil pH values were measured. The results showed that the fertilization period of plastic house soil in Xinxiang is usually around 15 age of cultivating where the content of organic matter therein is ideal, exceeding 30 g/kg. However, at the 15th cultivating years, the contents of alkali-hydrolyzable nitrogen and rapidly available phosphorus are slightly high, exceeding 150 and 90 mg·kg-1 respectively. Regarding the quantity of rapidly available potassium, the soil is in serious shortage of rapidly available potassium whose content is lower than 100 mg/kg, and this continues to decline after 15 cultivating years. The contents of nutrients decline as the depth of soil rises. The contents of organic matter, alkali-hydrolyzable nitrogen, and rapidly available phosphorus in soil of 0-20 cm in depth are 33%, 39.79%, and 18% higher than their contents in soil of 20-40 cm in depth. Judging from the contents of nitrogen phosphorus potassium in soil, plastic houses of different cultivating years are all in serious shortage of potassium, having an oversupply of phosphorus. Hence, great attention should be paid to the fertilization management of plastic house soil in Xinxiang city. The salinization speed of plastic house vegetable field soil slows down within the first 15 years of plantation, and it reaches 0.3% and exceeds the critical value of 0.296% at the 15th cultivating year. Then the salinization speed rises at an annual speed of 0.05%/a during the cultivating period from 15 to 30 years. Changes of contents of SO42-, NO3-, Cl-, K+, and Na+ agree with the change of content of water soluble salt, comprising of the main element of salt ions. The content of SO42- goes up stably at an annual speed of 33 mg/kg after cultivating of vegetables, and it always exceeds 43% of the total content of salt ions, becoming the ion leading to salinization of soil by the largest margin. pH value of the soil declines by approximately 0.03 each year after cultivating, but stays above 7.0 all the time without any occurrence of soil acidification. The analysis indicates that soil salinization tends to synchronize with a decline of pH value of soil, which directly resulted from the application of a large amount of fertilizer. The research conclusions tend to provide a theoretical basis for fertilization decisions of the vegetable greenhouse soil of Xinxiang.
Keywords:cultivation  soils  pH  cultivating years  vegetable field  soil fertility  salinization
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