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干旱区农田灌溉前后土壤水盐时空变异性研究 被引量:12
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作者 李宝富 熊黑钢 +1 位作者 张建兵 龙桃 《中国生态农业学报》 CAS CSCD 北大核心 2011年第3期491-499,共9页
通过田间土壤剖面取样,测定了新疆奇台县干旱区农田灌溉前、灌溉后1周和3周土壤水盐的时空变异特征。结果表明:灌溉前,剖面各层土壤含水量较低(15.25%~16.70%),且呈中等(偏弱)变异性;剖面上部(40 cm以上)土壤盐分呈强变异性,而下部为中... 通过田间土壤剖面取样,测定了新疆奇台县干旱区农田灌溉前、灌溉后1周和3周土壤水盐的时空变异特征。结果表明:灌溉前,剖面各层土壤含水量较低(15.25%~16.70%),且呈中等(偏弱)变异性;剖面上部(40 cm以上)土壤盐分呈强变异性,而下部为中等(偏强)变异性。灌溉后1周,除0~20 cm(弱变异性)外,其他土层水分及剖面下部盐分变异性未变,但变异系数均减小,上部土壤盐分转为中等(偏强)变异性;剖面平均土壤含水量升高10.51%,脱盐率达8.94%,其中,表层(0~20 cm)土壤水分增加率(118.48%)及脱盐率(20.86%)最大,底层(100~120 cm)水分增加率(40.54%)及脱盐率(-6.93%)最小。灌溉后3周与1周相比,各层(除80~100 cm土层)水分及盐分的变异性保持不变,但水分的变异系数增大,而盐分的变异系数减小;剖面平均含水量减少5.20%,表层(0~20 cm)失水率(36.47%)最大,80~100 cm失水率(7.31%)最小;表层土壤积盐率(4.55%)约为20~40 cm土层的12倍;而40 cm土层以下仍处于脱盐阶段,40~80 cm土壤脱盐率减小,80~120 cm土层脱盐率(9.03%)增大。 展开更多
关键词 干旱区农田 灌溉 土壤剖面 含量 时空变异 失水 积盐率
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膜下微润带埋深对温室番茄土壤水盐运移的影响 被引量:10
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作者 张子卓 牛文全 +1 位作者 许健 张珂萌 《中国生态农业学报》 CAS CSCD 北大核心 2015年第9期1112-1121,共10页
为探讨微润灌溉对温室轻度盐碱地番茄土壤水盐的影响,通过设置3种不同埋深(10 cm、15 cm、20 cm),探究了不同微润带埋设深度下,膜内(番茄种植行)、膜间(番茄行间)土壤含水量和含盐量的变化特征。结果表明,膜内、膜间土壤水盐的变... 为探讨微润灌溉对温室轻度盐碱地番茄土壤水盐的影响,通过设置3种不同埋深(10 cm、15 cm、20 cm),探究了不同微润带埋设深度下,膜内(番茄种植行)、膜间(番茄行间)土壤含水量和含盐量的变化特征。结果表明,膜内、膜间土壤水盐的变化规律在不同埋深下保持一致,膜内土壤水分随时间推移先增大后减小,盐分随时间推移逐渐减小;膜间土壤水分、盐分均随时间推移逐渐增大。膜间土壤含水量始终小于膜内,随着土层深度增加,膜内、膜间土壤含水量差距减小;表层土壤膜内、膜间土壤含水量差距最大,50-60 cm土层膜间与膜内土壤含水量基本趋于一致。微润带埋深大时,土壤含水量较高,开花结果期,20 cm、15 cm、10 cm埋深的土壤含水量分别为23.31%、24.46%及22.42%;且微润带埋深为10 cm时,膜内、膜间土壤含水量差值小于埋深为15 cm和20 cm。膜内土壤含盐量始终小于膜间,微润带埋深越小,膜内、膜间土壤含盐量差异也越小;全生育期内,膜内0-40 cm土层处于脱盐状态,脱盐率随深度增加逐渐降低,离微润带越近,脱盐效果越明显;40-60 cm土层土壤含水量少,盐分含量也较小,为轻微积盐状态。10-20 cm土层水分含量最大、盐分含量最小、脱盐率最高。膜间0-60 cm土层始终处于积盐状态,积盐率随深度增加逐渐降低,0-20 cm土层积盐率最高。开花结果期,20 cm、15 cm和10 cm埋深下,膜内10-20 cm土层平均最大脱盐率分别为24.66%、32.28%和14.71%,15 cm埋深下脱盐率最高;苗期和结果末期15 cm埋深处理脱盐率也达最高,平均最大脱盐率分别为27.42%、24.67%。研究结果充分说明微润带埋深对不同土层深度的洗盐效果具有显著影响。综合来看,微润带埋深15 cm时土层平均脱盐率和土壤平均含水率均最高,分别达到26.05%和25.1%,为番茄生长创造了一个良好的水盐环境,最有利于番茄生长发育,为最佳埋深。 展开更多
关键词 膜下微润灌溉 埋深 运移 膜内 膜间 积盐率 温室番茄
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微咸水混灌对土壤理化性质及冬小麦产量的影响 被引量:24
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作者 吴忠东 王全九 《农业工程学报》 EI CAS CSCD 北大核心 2008年第6期69-73,共5页
根据中科院南皮生态农业试验站2002~2005年的冬小麦微咸水混灌田间试验资料,以淡水为对照研究了矿化度分别为3、4、5g/L的微咸水混灌对土壤积盐率、土壤饱和浸提液钠吸附比(SAR)、冬小麦产量和产量构成因素以及水分利用效率的影响,从... 根据中科院南皮生态农业试验站2002~2005年的冬小麦微咸水混灌田间试验资料,以淡水为对照研究了矿化度分别为3、4、5g/L的微咸水混灌对土壤积盐率、土壤饱和浸提液钠吸附比(SAR)、冬小麦产量和产量构成因素以及水分利用效率的影响,从而确定适宜的灌溉水矿化度上限。结果表明,微咸水灌溉后土壤积盐程度与灌溉水矿化度呈正相关;微咸水灌溉会使土壤饱和浸提液的SAR升高,且影响深度因灌溉水矿化度而异。通过对冬小麦产量和产量构成因素的分析可得,在非偏旱年利用微咸水灌溉的矿化度不宜超过3g/L,偏旱年不宜采用微咸水进行灌溉,或灌溉后应采取措施缓解盐分胁迫,水分利用效率与灌溉水矿化度呈负相关,综合各种因素可以认为3g/L是当地微咸水灌溉的矿化度的上限。 展开更多
关键词 微咸水混灌 土壤积盐率 钠吸附比 冬小麦产量 水分利用效
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Experimental study of the electrical conductivity of hydrous minerals in the crust and the mantle under high pressure and high temperature 被引量:5
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作者 GUO XinZhuan 《Science China Earth Sciences》 SCIE EI CAS CSCD 2016年第4期696-706,共11页
Hydrous minerals are important water carriers in the crust and the mantle, especially in the subduction zone. With the recent development of the experimental technique, studies of the electrical conductivity of hydrou... Hydrous minerals are important water carriers in the crust and the mantle, especially in the subduction zone. With the recent development of the experimental technique, studies of the electrical conductivity of hydrous silicate minerals under controlled temperature, pressure and oxygen fugacity, have helped to constrain the water distribution in the Earth's interior. This paper introduces high pressure and temperature experimental study of electrical conductivity measurement of hydrous minerals such as serpentine, talc, brucite, phase A, super hydrous phase B and phase D, and assesses the data quality of the above minerals. The dehydration effect and the pressure effect on the bulk conductivity of the hydrous minerals are specifically emphasized. The conduction mechanism of hydrous minerals and the electrical structure of the subduction zone are discussed based on the available conductivity data. Finally, the potential research fields of the electrical conductivity of hydrous minerals is presented. 展开更多
关键词 Electrical conductivity High pressure and temperature experiment Hydrous minerals Conduction mechanism Subduction zone High conductivity anomalies
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Music stimuli lead to increased levels of nitrite in unstimulated mixed saliva
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作者 Luyuan Jin Mengbi Zhang +4 位作者 Junji Xu Dengsheng Xia Chunmei Zhang Jingsong Wang Songlin Wang 《Science China(Life Sciences)》 SCIE CAS CSCD 2018年第9期1099-1106,共8页
Concentration of salivary nitrate is approximately 10-fold to that of serum. Many circumstances such as acute stress could promote salivary nitrate secretion and nitrite formation. However, whether other conditions ca... Concentration of salivary nitrate is approximately 10-fold to that of serum. Many circumstances such as acute stress could promote salivary nitrate secretion and nitrite formation. However, whether other conditions can also be used as regulators of salivary nitrate/nitrite has not yet been explored. The present study was designed to determine the influence of exposure to different music on the salivary flow rate and nitrate secretion and nitrite formation. Twenty-four undergraduate students(12 females and 12 males) were exposed to silence, rock music, classical music or white noise respectively on four consecutive mornings. The unstimulated salivary flow rate and stimulated salivary flow rate were measured. Salivary ionic(Na+, Ca2+Cl-,and PO3-4) content and nitrate/nitrite levels were detected. The unstimulated salivary flow rate was significantly increased after classical music exposure compared to that after silence. Salivary nitrite levels were significantly higher upon classical music and white noise stimulation than those under silence in females. However, males were more sensitive only to white noise with regard to the nitrite increase. In conclusion, this study demonstrated that classical music stimulation promotes salivary nitrite formation and an increase in saliva volume was observed. These observations may play an important role in regulating oral function. 展开更多
关键词 classic music salivary flow rate salivary nitrite salivary nitrate
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