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滴灌施肥条件下减量施肥对马铃薯田土壤养分积累及产量的影响 被引量:11
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作者 冯志文 万书勤 +2 位作者 康跃虎 孙清华 张若芳 《节水灌溉》 北大核心 2019年第8期28-33,38,共7页
为了进一步确定合理施肥量并有效指导滴灌条件下的肥料管理,以马铃薯“夏波蒂”为试材,基于推荐施肥量(N、P2O5、K2O施用量分别为420、105、495kg/hm^2),布置了5个施肥量比例的滴灌施肥灌溉处理,分别为推荐施肥量的10%(F1)、30%(F2)、50... 为了进一步确定合理施肥量并有效指导滴灌条件下的肥料管理,以马铃薯“夏波蒂”为试材,基于推荐施肥量(N、P2O5、K2O施用量分别为420、105、495kg/hm^2),布置了5个施肥量比例的滴灌施肥灌溉处理,分别为推荐施肥量的10%(F1)、30%(F2)、50%(F3)、70%(F4)和90%(F5),研究了其对收获时农田土壤养分积累与产量的影响。结果表明,经过整个生育期的滴灌施肥灌溉后,随着施肥量的增加,0~60cm土层的硝态氮浓度增加,且向土壤下层的移动增加;0~40cm土层的铵态氮浓度和0~30cm土层的速效磷浓度呈先增加后下降的趋势;0~60cm土层的速效钾浓度在垂直分布减弱,而水平分布增加。当施肥量比例在70%左右(F4)时,土壤养分主要在积累0~40cm土层,且向下层土壤淋失较少。马铃薯产量随着施肥量的增加呈先增加后下降的趋势,以F3处理最高,为25.3t/hm^2,除显著高于F1处理外,与其他处理间差异不显著。因此,滴灌施肥灌溉时,当施肥量比例为推荐施肥量的70%左右时,马铃薯田的土壤养分主要积累在0~40cm土层,并降低了施肥量、减少了养分从根区的淋失,且产量较高。 展开更多
关键词 滴灌施肥 马铃薯 施肥量比例 土壤养分积累
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Effect of Sprinkler and Border Irrigation on Topsoil Structure in Winter Wheat Field 被引量:25
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作者 SUN Ze-Qiang kang yao-hu JIANG Shu-Fang 《Pedosphere》 SCIE CAS CSCD 2010年第4期419-426,共8页
A two-year experiment was carried out on the effect of sprinkler irrigation on the topsoil structure in a winter wheat field. A border-irrigated field was used as the control group. The total soil porosity, pore size ... A two-year experiment was carried out on the effect of sprinkler irrigation on the topsoil structure in a winter wheat field. A border-irrigated field was used as the control group. The total soil porosity, pore size distribution, pore shape distribution, soil cracks and soil compaction were measured. The sprinkler irrigation brought significant changes to the total soil porosity, capillary porosity, air-filled porosity and pore shape of topsoil layers in comparison with the border irrigation. The total porosity and air-filled porosity of the topsoil in the sprinkler irrigation were higher than those in the border irrigation. The changes in the air-filled and elongated pores were the main reasons for the changes in total porosity. The porosities of round and irregular pores in topsoil under sprinkler irrigation were lower than those under border irrigation. Sprinkler irrigation produced smaller soil cracks than border irrigation did, so sprinkler irrigation may restrain the development of macropore flow in comparison with border irrigation. The topsoil was looser under sprinkler irrigation than under border irrigation. According to the conditions of topsoil structure, it is preferable for crops to grow under sprinkler irrigation than under border irrigation. 展开更多
关键词 表层结构 土壤结构 麦田土壤 喷灌 畦灌 土壤总孔隙度 冬小麦 土壤孔隙度
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Effects of different irrigation methods on micro-environments and root distribution in winter wheat fields 被引量:7
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作者 Lü Guo-hua SONG Ji-qing +3 位作者 BAI Wen-bo WU Yong-feng LIU Yuan kang yao-hu 《Journal of Integrative Agriculture》 SCIE CAS CSCD 2015年第8期1658-1672,共15页
The irrigation method used in winter wheat fields affects micro-environment factors, such as relative humidity(RH) within canopy, soil temperature, topsoil bulk density, soil matric potential, and soil nutrients, and ... The irrigation method used in winter wheat fields affects micro-environment factors, such as relative humidity(RH) within canopy, soil temperature, topsoil bulk density, soil matric potential, and soil nutrients, and these changes may affect plant root growth.An experiment was carried out to explore the effects of irrigation method on micro-environments and root distribution in a winter wheat field in the 2007–2008 and 2008–2009 growing seasons.The results showed that border irrigation(BI), sprinkler irrigation(SI), and surface drip irrigation(SDI) had no significant effects on soil temperature.Topsoil bulk density, RH within the canopy, soil available N distribution, and soil matric potential were significantly affected by the three treatments.The change in soil matric potential was the key reason for the altered root profile distribution patterns.Additionally, more fine roots were produced in the BI treatment when soil water content was low and topsoil bulk density was high.Root growth was most stimulated in the top soil layers and inhibited in the deep layers in the SDI treatment, followed by SI and BI, which was due to the different water application frequencies.As a result, the root profile distribution differed, depending on the irrigation method used.The root distribution pattern changes could be described by the power level variation in the exponential function.A good knowledge of root distribution patterns is important when attempting to model water and nutrient movements and when studying soil-plant interactions. 展开更多
关键词 根系分布 冬小麦田 灌溉方式 微环境 土壤-植物 土壤温度 土壤容重 土壤水势
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Effects of water application intensity of microsprinkler irrigation on water and salt environment and crop growth in coastal saline soils 被引量:4
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作者 CHU Lin-lin kang yao-hu WAN Shu-qin 《Journal of Integrative Agriculture》 SCIE CAS CSCD 2015年第10期2077-2089,共13页
Laboratory and field experiments were conducted to investigate the effects of water application intensity(WAI) on soil salinity management and the growth of Festuca arundinacea(festuca) under three stages of water and... Laboratory and field experiments were conducted to investigate the effects of water application intensity(WAI) on soil salinity management and the growth of Festuca arundinacea(festuca) under three stages of water and salt management strategies using microsprinkler irrigation in Hebei Province, North China. The soil water content(è) and salinity of homogeneous coastal saline soils were evaluated under different water application intensities in the laboratory experiment. The results indicated that the WAI of microsprinkler irrigation influenced the è, electrical conductivity(ECe) and p H of saline soils. As the WAI increased, the average values of è and ECe in the 0–40 cm profile also increased, while their average values in the 40–60 cm profile decreased. The p H value also slightly decreased as depth increased, but no significant differences were observed between the different treatments. The time periods of the water redistribution treatments had no obvious effects. Based on the results for è, ECe and p H, a smaller WAI was more desirable. The field experiment was conducted after being considered the results of the technical parameter experiment and evaporation, wind and leaching duration. The field experiment included three stages of water and salt regulation, based on three soil matric potentials(SMP), in which the SMP at a 20-cm depth below the surface was used to trigger irrigation. The results showed that the microsprinkler irrigation created an appropriate environment for festuca growth through the three stages of water and salt regulation. The low-salinity conditions that occurred at 0–10 cm depth during the first stage(-5 k Pa) continued to expand through the next two stages. The average p H value was less than 8.5. The tiller number of festuca increased as SMP decreased from the first stage to the third stage. After the three stages of water and salt regulation, the highly saline soil gradually changed to a low-saline soil. Overall, based on the salt desalinization, the microsprinkler irrigation and three stages of water and salt regulation could be successfully used to cultivate plants for the reclamation of coastal saline land in North China. 展开更多
关键词 滨海盐土 作物生长 灌溉水 微喷头 盐环境 强度 应用 土壤盐分
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Effect of different water application intensity and irrigation amount treatments of microirrigation on soil-leaching coastal saline soils of North China 被引量:2
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作者 CHU Lin-lin kang yao-hu WAN Shu-qin 《Journal of Integrative Agriculture》 SCIE CAS CSCD 2016年第9期2123-2131,共9页
In coastal regions, Bohai Gulf is one of the most affected areas by salinization. To study the effects of mocrosprinkler irrigation on the characteristics of highly saline sandy loam soil(ECe(saturated paste extract)=... In coastal regions, Bohai Gulf is one of the most affected areas by salinization. To study the effects of mocrosprinkler irrigation on the characteristics of highly saline sandy loam soil(ECe(saturated paste extract)=22.3 d S m^(–1); SAR(sodium adsorption ratio)=49.0) of North China, a laboratory experiment was conducted. Five water application intensity(WAI) treatments(1.7, 3.1, 5.3, 8.8, and 10.1 mm h^(–1)), five irrigation amount(IA) treatments(148, 168, 184, 201, and 223 mm) and three time periods of water redistribution(0, 24 and 48 h) were employed in the study. A compounding microsprinkler system was used for the WAI treatments, and a single microsprinkler was used for the IA treatments. The results indicated that, as soil depth increased, soil water content(θ) increased and then slightly decreased; with WAI and IA consistently increasing, the relatively moist region expanded and the average θ increased. Meanwhile, soil ECe increased as soil depth increased, and the zone with low soil salinity expanded as WAI and IA increased. Although the reduction of the average SAR was smaller than that of the average electrical conductivity of the ECe, these variables decreased in similar fashion as WAI and IA increased under microsprinkler irrigation. The average p H decreased as soil depth increased. Longer time periods of water redistribution led to lower salinity and slight expansion of the SAR zone. Considering the effects of leached salts in coastal saline soils, greater WAI and IA values are more advantageous under unsaturated flow conditions, as they cause better water movement in the soil. After leaching due to microsprinkler irrigation, highly saline soil gradually changes to moderately saline soil. The results provide theoretical and technological guidance for the salt leaching and landscaping of highly saline coastal environments. 展开更多
关键词 滨海盐渍土 土壤特性 华北地区 喷灌强度 灌溉量 土壤水分含量 浸出 微灌
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散水介质滴灌龟裂碱土水盐运移规律
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作者 黄鹏飞 康跃虎 +3 位作者 万书勤 李晓彬 黄艳丽 刘春成 《土壤通报》 CAS CSCD 北大核心 2023年第5期1041-1049,共9页
【目的】探究散水介质滴灌条件下龟裂碱土水盐运移规律。【方法】室内设置土柱试验研究散水介质滴灌条件下龟裂碱土水分、电导率和pH的变化规律。【结果】一维垂直入渗条件下散水介质滴灌较定水头入渗水分扩散速率更快,稳定入渗阶段散... 【目的】探究散水介质滴灌条件下龟裂碱土水盐运移规律。【方法】室内设置土柱试验研究散水介质滴灌条件下龟裂碱土水分、电导率和pH的变化规律。【结果】一维垂直入渗条件下散水介质滴灌较定水头入渗水分扩散速率更快,稳定入渗阶段散水介质滴灌垂直湿润峰扩散速率提高了50.3%,两种灌溉方式水盐分布规律基本一致。二维条件下垂直方向湿润峰扩散速率高于水平方向,水分再分布过程中以散水介质和龟裂碱土界面处碱土表层土壤为中心向外扩散;散水介质水平距离10 cm时,相邻灌水器形成的湿润体在96 h逐渐搭接整体向外淋洗盐分;电导率<2 dS m^(-1)的脱盐区pH<9,电导率介于2~4 dS m^(-1)的脱盐区土壤pH值较原土逐渐降低,脱盐区边缘电导率介于4~10 dS m^(-1),pH值显著高于原土,积盐区边缘pH值较原土略下降。【结论】散水介质滴灌能够显著增加龟裂碱土的水分入渗速率,并在灌水器下方快速形成脱盐区,脱盐初期土壤碱化现象明显且与脱盐程度密切相关,生产实践中应采取相应的措施避免pH值过高影响植物生长。 展开更多
关键词 盐碱地改良 龟裂碱土 滴灌 散水介质 水盐运移
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Soil Salinity Changes Under Cropping with Lycium barbarum L.and Irrigation with Saline-Sodic Water 被引量:11
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作者 DOU Chao-Yin kang yao-hu +1 位作者 WAN Shu-Qin HU Wei 《Pedosphere》 SCIE CAS CSCD 2011年第4期539-548,共10页
In order to utilize the wasted saline-sodic soils under shallow groundwater condition,a 3-year field study was carried in a field cropped with Lycium barbarum L.and irrigated by drip irrigation with saline groundwater... In order to utilize the wasted saline-sodic soils under shallow groundwater condition,a 3-year field study was carried in a field cropped with Lycium barbarum L.and irrigated by drip irrigation with saline groundwater under the water table depth of 30-40 cm in the northern Yinchuan Plain,China.Effects of cropping duration (one,two,and three years) on soil salinity,soil solution composition,and pH in three adjacent plots were investigated in 2008.Results showed that a high irrigation frequency maintained high soil water potential and subsequently facilitated infiltration and downward movement of water and salt in the crop root zone.Salt accumulated on the edges of the ridges,and soil saturated-paste electrical conductivity (ECe) was higher in the edge.Concentrations of Na+,Ca2+,Mg2+,Cl-,and SO42- in the soil increased with the soil depth as did the ECe,while HCO3- and pH had a relative uniform distribution in soil profile.As planting year increased,the ECe and soil salts in the field had a decreasing tendency,while in the root zone they decreased immediately after irrigation and then remained relatively stable in the following growing seasons.HCO3- and pH had little change with the planting year.Results suggested that the application of drip irrigation with saline water could ameliorate saline-sodic soil and provide a relatively feasible soil environment for the growth of salt-tolerant plant Lycium barbarum L.under the saline-sodic soils with shallow groundwater. 展开更多
关键词 土壤盐碱化 地下水灌溉 生理盐水 盐度变化 枸杞 PH值变化 浅层地下水
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