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国家重点基础研究发展计划(2009CB825101)

作品数:47 被引量:532H指数:13
相关作者:王绍明张霞熊友才朱宏伟曹国栋更多>>
相关机构:石河子大学中国科学院新疆生态与地理研究所兰州大学更多>>
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Spatial distribution of soil moisture,salinity and organic matter in Manas River watershed,Xinjiang,China被引量:9
2012年
With the classical statistical and geostatistical methods,the study of the spatial distribution and its influence factors of soil water,salinity and organic matter was carried out for 0-70 cm soil layers in Manas River watershed.The results showed that the soil moisture data from all soil layers exhibited a normal distribution,with average values of 14.08%-21.55%.Geostatistical analysis revealed that the content of soil moisture had a moderate spatial autocorrelation with the ratios of nugget/sill ranging from 0.500 to 0.718,which implies that the spatial pattern of soil moisture is influenced by the combined effects of structural factors and random factors.Remarkable spatial distributions with stripped and mottled features were found for soil moisture in all different soil layers.The landform and crop planting had a relatively big influence on the spatial distribution of soil moisture;total soil salinity was high in east but low in west,and non-salinized soil and lightly salinized soil appeared at the northwest and southwest of the study area.Under the effect of reservoir leakage,the heavily salinized soils are widely distributed in the middle of the study area.The areas of the non-salinized and lightly salinized soils decreased gradually with soil depth increment,which is contrary to the case for saline soils that reached a maximum of 245.67 km2 at the layer of 50-70 cm.The types of soil salinization in Manas River watershed were classified into four classes:the sulfate,chloride-sulfate,sulfate-chloride and chloride.The sulfate salinized soil is most widely distributed in the surface layer.The areas of chloride-sulfate,sulfate-chloride,and chloride salinized soils increased gradually along with the increment of soil depth;the variation range of the average values of soil organic matter content was between 7.48%-11.33%.The ratios of nugget/sill reduced gradually from 0.698 to 0.299 with soil depth increment,which shows that the content of soil organic matter has a moderate spatial autocorrelation.The soil organi
Jilili ABUDUWAILIYang TANGMireban ABULIMITIDongWei LIULong MA
关键词:玛纳斯河流域盐渍化土壤
Water adaptive traits of deep-rooted C_3 halophyte(Karelinia caspica(Pall.) Less.) and shallow-rooted C_4 halophyte(Atriplex tatarica L.) in an arid region,Northwest China
2012年
This paper focused on the water relations of two halophytes differing in photosynthetic pathway,phenotype,and life cycle:Karelinia caspica(Pall.) Less.(C3,deep-rooted perennial Asteraceae grass) and Atriplex tatarica L.(C4,shallow-rooted annual Chenopodiaceae grass).Gas exchange,leaf water potential,and growth characteristics were investigated in two growing seasons in an arid area of Xinjiang to explore the physiological adaptability of the two halophytes.Both K.caspica and A.tatarica showed midday depression of transpiration,indicating that they were strong xerophytes and weak midday depression types.The roots of A.tatarica were concentrated mainly in the 0-60 cm soil layer,and the leaf water potential(ΨL) increased sharply in the 0-20 cm layer due to high soil water content,suggesting that the upper soil was the main water source.On the other hand,K.caspica had a rooting depth of about 1.5 m and a larger root/shoot ratio,which confirmed that this species uptakes water mainly from deeper soil layer.Although A.tatarica had lower transpiration water consumption,higher water use efficiency(WUE),and less water demand at the same leaf water potential,it showed larger water stress impact than K.caspica,indicating that the growth of A.tatarica was restricted more than that of K.caspica when there was no rainfall recharge.As a shallow-rooted C4 species,A.tatarica displayed lower stomatal conductance,which could to some extent reduce transpiration water loss and maintain leaf water potential steadily.In contrast,the deep-rooted C3 species K.caspica had a larger root/shoot ratio that was in favor of exploiting groundwater.We concluded that C3 species(K.caspica) tapes water and C4 species(A.tatarica) reduces water loss to survive in the arid and saline conditions.The results provided a case for the phenotype theory of Schwinning and Ehleringer on halophytic plants.
Yuan FANPinFang LIZhenAn HOUTuSheng RENChunLian XIONGBiao ZHANG
关键词:四翅滨藜叶水势花花柴
准噶尔盆地荒漠-绿洲过渡区土壤呼吸特征
2011年
【目的】研究干旱区典型山盆结构下不同土地利用方式的土壤呼吸特征,为干旱区碳过程阐明提供数据支持。【方法】通过LI-8100碳通量测定系统对西北干旱区典型荒漠-绿洲过渡带的自然植被和人工作物覆盖下的土壤呼吸进行两个植物生长时期的监测。【结果】不同植被覆盖条件的土壤呼吸日变化均呈单峰曲线,且日呼吸速率最高值出现在14:00~16:00,最低值出现在02:00~04:00;植物花期的土壤呼吸速率平均值明显高于凋败期;土壤0~5、5~10、10~20 cm温度日变化与土壤呼吸速率变化趋势极为接近。【结论】不同土地利用/覆盖下土壤呼吸特征差异性明显,土壤温度是影响土壤呼吸的关键因子。
朱宏伟夏军曹国栋王绍明张霞杨瑞阳
关键词:土壤呼吸土壤温度环境因子
灌溉水矿化度对玛纳斯流域棉花生长影响的试验研究被引量:13
2012年
合理利用咸水资源对缓解干旱区绿洲农业用水矛盾有重要意义。本文于2010年和2011年在石河子大学节水灌溉试验站研究了矿化度为0.87、2、3、4、6、8g/L的咸水对土壤水盐动态和棉花生长及产量的影响。结果表明,咸水灌溉导致土壤剖面持续积盐,棉花叶面积指数减小,干物质积累减少、产量下降;灌溉水矿化度每提高1g/L,产量降低约391kg/hm2;土壤根系层(0~60cm)可溶性盐浓度每升高1g/L,产量降低约861kg/hm2。在灌溉水矿化度2g/L情况下,100cm土层盐分最大累积率2010年为113%,2011年为26%,呈下降趋势,棉花生长、干物质积累及产量受影响较小,可作为该区咸水利用调控参考阈值,指导农业生产。
杨传杰罗毅孙林甘容吴娜张艳阿布都外力.吉力力
关键词:滴灌咸水土壤盐分土壤水分棉花
干旱区滴灌棉田灌水量与灌溉周期关系被引量:7
2012年
由于其节水增产的优势,近年来,膜下滴灌在我国西北干旱区绿洲农田得到了迅速推广。由于轮灌仍是目前农田用水分配的主要方式,并且还需要考虑滴灌产生的土壤盐分积累问题,因此,对滴灌灌水量(Q)、灌水周期(T)以及相应的深层下渗(L)关系研究,不仅是农田用水分配的要求,也是盐分控制的需要。本文利用田间试验数据校验HYDRUS-2D模型,进行数值模拟试验,并结合马尔可夫链模型分析,分析不确定蒸散下的Q-T-L关系,结果显示:①总体上,随着灌水量的增加,可支持的灌溉周期增加,同时深层下渗增加,Q-T-L关系曲线表现为非线性关系;②其中存在3个关键Q-T阈值点:深层下渗出现点(Q为35mm,T为5d)、灌溉周期增加减缓点(Q为65mm,T为10d)、最大灌溉周期点(T为11d,Q为120mm)。因此,①在以水分利用为优先的模式下,最大灌水量不应超出35mm,最大灌溉周期为5d;②在灌溉间隔时间优先的模式下,有最大灌水周期11d,所需灌水量为120mm,适宜的灌水周期为10d,所需灌水量为65mm;③在有盐分淋洗需求模式下,适宜的灌水周期为10d,所需灌水量为65mm,产生下渗量约占灌水量17%,可用于根区盐分淋洗;④潜水位对灌溉产生作用的阈值深度是-300cm,高于时潜水可以补给根区土壤水分,从而增加灌溉周期。利用本文数值模拟与方法,可以为不同气候与土壤情形区域农田滴灌灌溉设计提供指导。
孙林罗毅杨传杰张艳来剑斌吉力力·阿不都外力
关键词:滴灌灌溉量
玛纳斯河流域近30年气候要素变化研究被引量:1
2013年
为了探索和揭示玛纳斯河流域各气候要素之间的关系,通过对该流域1983年以来逐月平均气温、平均最低气温、平均最高气温以及降水量等数据的分析,结果表明:玛纳斯河流域近30年平均气温、日最高气温、日最低气温随时间呈增加态势;1月最低气温的线性增加率为8.21℃/100a,7月最高气温的线性增加率为13℃/100a,其结果导致日较差减少;20世纪90年代末期年平均气温、日最高气温、日最低气温显著升高;年平均降水量与冬季降水量变化较为相似,夏季降雨变化波动较大;降水量与气温变化呈显著正相关。
侯丽娜刘慧明王绍明
关键词:最高气温最低气温降水量气候变化玛纳斯河流域
滴灌棉田土壤水盐氮的分布和运移规律
2013年
选取典型绿洲滴灌条件下中度和轻度盐渍化棉田,研究不同盐分含量棉田土壤水、盐、氮的分布特征和运移规律。结果表明:整个生育期土壤(0-80cm)水分含量呈现增加-减少-增加-减少的趋势,中度盐渍化棉田土壤水分含量要显著高于轻度盐渍化棉田,并且在0-20cm、60-0cm土层含水量都较高。随着棉田土壤水分含量的增加,土壤盐分含量迅速降低,水分含量减少,盐分有所增加;棉田土壤表层硝态氮含量较高,60cm土层最低,80cm土层略有增加,轻度盐渍化棉田土壤硝态氮含量显著高于中度盐渍化棉田,其0-80cm土体硝态氮含量分别为30.3mg/kg和28.4mg/kg,主要是由于高盐分含量土壤水分残留较多,容易造成硝态氮的深层淋洗。
王海江李冬冬侯振安吕新
关键词:滴灌滴灌棉花
新疆橙黄疣柄牛肝菌分离培养研究被引量:3
2010年
研究以橙黄疣柄牛肝菌的子实体作为分离材料,采用组织分离方法,在不同配方的培养基上培养,筛选出适合橙黄疣柄牛肝菌菌丝生长的基础培养基,其中菌盖和菌柄两者交接处的分离成功率达60%以上。以菌丝生长速度、生长状况为参照标准,对橙黄疣柄牛肝菌的生物学特性进行研究,确定其最适生长温度、pH值、葡萄糖含量以及氮源。结果表明,橙黄疣柄牛肝菌为中温型菌根真菌,在25℃下长势良好,最佳pH值为6,最佳葡萄糖含量为0.5%,最佳氮源为蛋白胨。
贺亚玲刘红玲陆爽李邦张霞王绍明
Arbuscular mycorrhizal fungal colonization of Glycyrrhiza glabra roots enhances plant biomass,phosphorus uptake and concentration of root secondary metabolites被引量:13
2014年
Arbuscular mycorrhizal(AM)fungi penetrate the cortical cells of the roots of vascular plants,and are widely distributed in soil.The formation of these symbiotic bodies accelerates the absorption and utilization of mineral elements,enhances plant resistance to stress,boosts the growth of plants,and increases the survival rate of transplanted seedlings.We studied the effects of various arbuscular mycorrhizae fungi on the growth and development of licorice(Glycyrrhiza glabra).Several species of AM,such as Glomus mosseae,Glomus intraradices,and a mixture of fungi(G.mosseae,G.intraradices,G.cladoideum,G.microagregatum,G.caledonium and G.etunicatum)were used in our study.Licorice growth rates were determined by measuring the colonization rate of the plants by the fungi,plant dry biomass,phosphorus concentration and concentration of secondary metabolites.We established two cloned strains of licorice,clone 3(C3)and clone 6(C6)to exclude the effect of genotypic variations.Our results showed that the AM fungi could in fact increase the leaf and root biomass,as well as the phosphorus concentration in each clone.Furthermore,AM fungi significantly increased the yield of certain secondary metabolites in clone 3.Our study clearly demonstrated that AM fungi play an important role in the enhancement of growth and development of licorice plants.There was also a significant improvement in the secondary metabolite content and yield of medicinal compounds from the roots.
HongLing LIUYong TANMonika NELLKarin ZITTER-EGLSEERChris WAWSCRAHBrigitte KOPPShaoMing WANGJohannes NOVAK
关键词:植物生物量磷浓度摩西球囊霉定殖
季节性冻融对盐荒地水盐运移的影响及调控被引量:20
2013年
季节性冻融是干旱区土壤盐碱化形成的主要驱动因子,但冻融过程中土壤水盐耦合关系及热量调控机理仍不清楚。通过分析2009年11月~2010年5月新疆玛纳斯河流域典型盐荒地季节性冻融过程中土壤剖面160cm以内的水分、盐分和温度动态变化,探讨了不同土层冻融过程中水热盐的耦合关系。结果表明:土壤最大冻结深度为150cm左右,表土层(0~40cm)温度与气温关系密切;土壤剖面水分呈现“C”型垂直分布,表土层和底土层(100~160cm)含水量较大,而心土层(40~100em)含水量不足10%,土层平均含水率在冻融前期增加了12.91%,而在初蒸期减少了10.01%;土壤剖面盐分在冻结期和初蒸期表聚作用明显,心土层和底土层含盐量稳定,土壤剖面含盐量表现为“积盐-脱盐-再积盐”的变化过程。水热盐之间具有高度协同性,心土层和底土层表现为水盐相随、而表土层为水去盐留的耦合特征,热量传输是调控水盐运移的关键因素。
富广强李志华王建永王绍明王慧莉Asfa Batool熊友才
关键词:季节性冻融水盐运移积盐玛纳斯河流域
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