滨海盐碱地不同土壤-树种系统中盐分离子分布与运移

为揭示滨海盐碱地造林树种对土壤盐分组成变化及树体内盐离子的吸收、运移的影响,采用野外取样与室内分析测试相结合的方法,定量研究了8个盐碱地生态造林树种不同部位(叶、枝、皮、根)及相应林下土壤可溶性盐离子含量,结果表明:对照空地与8个树种及林下土壤中均无CO2-3存在,造林可明显改变土壤中Na+、Cl-、SO2-4、HCO-3等可溶性盐离子的含量,降低土壤全盐含量,不同树种对土壤平均含盐量的降低状况表现为柽柳白蜡杨树桑树刺槐紫穗槐榆树冬枣。不同树种对K+、Na+、Ca2+、Mg2+的吸收选择性系数呈现SK,NaSCa,NaSMg,Na,整体上不同树种对K+具有很强的吸收选择性,Na+被动吸收及在体内的分布表现了树种间的耐盐机制差异,不同树种对Ca2+的吸收选择性都略高于Mg2+。8个树种运输选择性系数RS各不相同,导致树体内各可溶盐离子的分布不同,不同树种各器官中K+、Ca2+、Mg2+的浓度均呈叶部较高。     

运东近滨海地区燕麦秸秆盐分积累与改良盐碱地潜力分析

为探明燕麦在运东滨海盐碱地区秸秆盐分积累特点以及改良盐碱地的潜力,选用"坝莜1号"、"白燕2号"和"花早2号"燕麦,采用单因素随机区组试验,以品种和土壤含盐量作为因素,进行了2组田间试验,测得燕麦的生物量、秸秆离子浓度和积累量及秸秆与土壤离子浓度比值。研究结果显示,"坝莜1号"燕麦开花-灌浆至成熟期整株生物量从2.9 t·hm-2增加至3.8 t·hm-2,延迟20 d收获则减少至2.5 t·hm-2。"白燕2号"在低土壤盐分浓度(1.0 g·kg-1左右)下的生物量(3.1 t·hm-2)显著大于中浓度(2.0 g·kg-1左右,1.7 t·hm-2)和高浓度(3.0 g·kg-1左右,0.4 t·hm-2)下的生物量。中等土壤盐分浓度下"坝莜1号"的生物量(3.8 t·hm-2)显著高于"白燕2号"(3.1t·hm-2)和"花早2号"(2.2 t·hm-2)。"坝莜1号"秸秆中Na+、K+浓度从开花到成熟均显著增加,而Mg2+、Ca2+和Cl-则显著降低。延迟20 d收获,除Ca2+外,其他离子浓度均显著降低。随着土壤盐分的升高,"白燕2号"秸秆Na+、Mg2+、Ca2+和Cl-浓度显著升高,而K+显著下降。3个品种的Na+、K+和Mg2+之间存在显著差异,而Cl-和Ca2+浓度无显著差异。燕麦秸秆中Cl-浓度最高,K+和Na+基本相当,均高于Mg2+和Ca2+。"坝莜1号"秸秆中Na+、K+、Mg2+、Cl-积累量成熟期最高,延迟收获20 d后积累量均显著降低。"白燕2号"秸秆Na+、K+、Mg2+、Ca2+、Cl-积累量随土壤盐分升高显著下降。除Ca2+外,Na+、K+、Mg2+、Cl-积累量品种之间差异显著。"坝莜1号"秸秆与土壤离子浓度比值中,Na++K+最大(46~63),其次是Cl-(30~46)、Mg2+(24~30)和Ca2+(3~15);延迟收获后Na++K+和Cl-秸秆与土壤浓度比值显著下降,Mg2+比值无显著变化,Ca2+比值显著升高。随着土壤盐分升高"白燕2号"秸秆与土壤Na++K+和Cl-浓度比值显著下降,Ca2+无显著变化。秸秆与土壤离子浓度比值在品种之间存在显著差异。燕麦理论上具有改良盐碱地的潜力,但收获时间和土壤盐分均会显著地影响燕麦生物量、离子浓度和积累量,从而影响燕麦改良盐碱地的效果。     

日光温室番茄缺镁与土壤盐分组成及离子活度的关系

研究了石灰性土壤日光温室不同栽培年限及番茄不同程度缺镁的土壤水溶盐分中离子组成、比例及Mg2+、Ca2+、K+离子活度等的变化及关系.结果表明:随着栽培年限的增加,温室土壤水溶盐分中Ca2+、K+、NO3-含量显著增加;水溶性盐分中阳离子以Ca2+为主,栽培5 a后NO3-成为阴离子主要成分;土壤中NO3-含量的增加是导致土壤盐分累积的主要因素.随番茄缺镁程度的加剧,土壤水溶性盐中Ca2+、K+、NO3-、全盐量及Ca2+/Mg2+、K+/Mg2+摩尔比均呈增加趋势,番茄出现缺镁的土壤含盐量达到盐渍化水平.随着土壤盐分含量增加,Ca2+、Mg2+活度均呈指数下降趋势,番茄缺镁的土壤溶液中Mg2+和Ca2+活度显著低于不缺镁土壤,(K+)/(Mg2+)、(Ca2+)/(Mg2+)活度比显著高于不缺镁土壤,(K+)/(Mg2+)活度比随缺镁程度加剧达显著差异,番茄缺镁的土壤溶液(K+)/(Mg2+)活度比大于1.盐分累积使Mg2+活度大幅降低以及K+富集对植物吸收Mg2+的拮抗作用是石灰性土壤上番茄缺镁的主要诱因.     

外源多元醇对盐胁迫下甜瓜幼苗生长和离子平衡的影响

为了探讨外源甘露醇和山梨醇对盐胁迫下甜瓜幼苗生长和离子平衡的影响,以甜瓜‘桂蜜12号’为试验材料,以Hoagland 营养液为培养液进行沙培(CK0),采用100 mmol/L NaCl模拟盐胁迫(CK1),然后添加不同浓度的甘露醇和山梨醇,观察不同处理的甜瓜幼苗生长情况和离子平衡变化。结果表明,在100 mmol/L NaCl盐胁迫(CK1)下,与对照(CK0)相比,甜瓜幼苗根系鲜质量、干质量、根总长度、根表面积以及根体积显著下降,K+/Na+、Ca2+/Na+、Mg2+/Na+显著降低。添加0.4 mmol/L的甘露醇,可显著增加甜瓜幼苗茎叶部Ca2+、Mg2+含量,而不增加Na+含量,不降低K+含量;显著提高Mg2+/Na+,而Ca2+/Na+及K+/Na+则与CK1持平。添加0.4 mmol/L的山梨醇显著提高地上部鲜重、幼苗根长、根表面积和根体积,显著降低盐胁迫甜瓜幼苗的Na+含量,提高Ca2+、Mg2+含量,显著提高Mg2+/Na+、K+/Na+、Ca2+/Na+。上述结果表明,适宜浓度的山梨醇和甘露醇可以缓解盐胁迫对甜瓜幼苗的伤害。在试验条件下,缓解盐胁迫对甜瓜幼苗根系及离子平衡影响的最适处理是添加0.4 mmol/L的山梨醇。     

盐胁迫对小型西瓜幼苗体内离子分布的影响

采用营养液水培法,研究了不同NaCl浓度对耐盐性不同的两个小型西瓜品种（秀雅和秀丽）幼苗体内离子分布的影响。结果表明,NaCl胁迫抑制了西瓜幼苗的生长,秀雅生长受抑制程度明显小于秀丽; 随NaCl浓度的提高,植株体内Na+和Cl－含量增加,K+、 Ca2+和Mg2+含量降低。5种离子在器官间呈区域化分布,Cl－主要积累在茎中而Na+主要积累于茎和根中; K+含量在茎中降低幅度较大,叶中降低幅度较小; Ca2+和Mg2+主要存在于茎和叶中,且在叶中降低幅度较小。NaCl胁迫下,西瓜根向茎选择性运输K+和Ca2+的能力降低,而茎向叶选择性运输的能力提高,有利于减轻NaCl胁迫对叶片的伤害。与秀丽相比,秀雅叶中K+、 Ca2+含量降低幅度较小,Cl－和Na+积累量较少,K+/Na+和Ca2+/Na+比值均较高,茎向叶运输的SK,Na和SCa,Na值也较高。以上结果说明,向叶片运输Na+的选择性较低,是秀雅耐盐性较强的主要原因之一,离子在器官水平上的区域化分布是西瓜植株适应盐胁迫的重要生理机制之一。     

钙对NaCl胁迫下马铃薯脱毒苗离子吸收、分布的影响

【目的】马铃薯是对盐分较敏感的农作物,土壤盐渍化会严重影响马铃薯的生长发育及其产量和品质。有关钙对Na Cl胁迫下马铃薯离子吸收、分布的研究较少。本文通过研究不同浓度Ca Cl2对Na Cl胁迫下马铃薯脱毒苗离子吸收、分布和运输的影响,探讨钙对Na Cl胁迫下马铃薯的调控机制,为盐渍土上马铃薯的生产提供理论依据与技术支持。【方法】以‘克新一号’马铃薯品种为试验材料,采用组织培养方法,将0、5、10、15和20 mmol/L Ca Cl2与0、25、50和75 mmol/L Na Cl分别添加到MS+2mg/L B9+3%蔗糖+0.9%琼脂培养基中,制成不同处理组合的培养基。将继代培养的脱毒苗按单节茎段剪切接种到培养基中进行培养。接种30天时调查脱毒苗生物量和Na+、Cl-、K+、Ca2+、Mg2+、P积累量,并分析Na+/K+、Na+/Ca2+、Na+/Mg2+比值及根系与茎叶的SK、Na、SMg、Na和SCa、Na值,探讨离子吸收、运输及分布情况。【结果】Na Cl胁迫抑制马铃薯脱毒苗的生长,随Na Cl胁迫浓度的增加,马铃薯脱毒苗鲜重、干重显著下降,各器官Na+和Cl-含量极显著增加,K+含量显著下降,Ca2+和Mg2+含量减少,茎、叶中P含量降低而根中P含量增加。Na+/K+、Na+/Ca2+、Na+/Mg2+比值随Na Cl胁迫浓度的增加而升高。随Na Cl胁迫浓度的增加,马铃薯脱毒苗根系与茎叶的SK、Na和SMg、Na值逐渐降低,SCa、Na值呈先升高后降低趋势。0、25和50 mmol/L Na Cl胁迫浓度下,以10 mmol/L Ca Cl2处理的马铃薯脱毒苗根、茎叶鲜重和干重最高,75 mmol/L Na Cl胁迫下以15 mmol/L Ca Cl2处理的马铃薯脱毒苗生物量最高。各Na Cl胁迫浓度下,添加Ca Cl2后,马铃薯脱毒苗各器官Na+含量明显降低,Cl-含量显著增加,K+、Ca2+、Mg2+含量升高,P含量先降低后升高。0、25、50和75 mmol/L Na Cl胁迫浓度下,添加适量Ca Cl2可明显降低马铃薯脱毒苗各器官Na+/K+、Na+/Ca2+、Na+/Mg2+比值,提高SK、Na、SMg、Na和SCa、Na值,增强K+、Ca2+、Mg2+向地上部的选择运输能力,抑制Na+向地上部的选择运输能力,维持细胞内离子平衡,缓解盐胁迫造成的营养亏缺。【结论】Na Cl胁迫下添加外源钙,能够有效改善马铃薯脱毒苗体内的离子平衡,促进营养吸收,Na+向叶片选择运输能力降低,K+、Ca2+、Mg2+向地上部的选择运输能力增强,离子在各器官水平上的区域化分布发生改变是钙缓解盐胁迫的重要生理机制之一。     

盐胁迫下柚实生苗生长、矿质营养及离子吸收特性研究

以坪山柚为材料,对盐胁迫下实生苗生长、矿质营养及离子吸收特性进行了研究。结果表明,沙培30d,80～200mmol/L盐胁迫,随盐浓度提高,坪山柚实生苗株高、叶面积、地上部干重和根部干重明显降低。溶液培养8d,坪山柚实生苗地上部及根Na+、Cl-含量随盐浓度的增加而增加,根及地上部K+、Ca2+、Mg2+以及P和Mn含量下降,Fe、Zn、Cu含量的变化因器官而异。其中,地上部Fe含量对盐胁迫敏感,可作为柚耐盐性鉴定指标。40mmol/L盐胁迫,坪山柚地上部K+/Na+、Ca2+/Na+、Mg2+/Na+值均显著下降,且Mg2+/Na+值+/Na+值>1;浓度≥160mmol/L盐胁迫,K+/Na+值+吸收、运转效率比Cl-高。     

磷钾肥施用对日光温室土壤溶液离子组成的影响

采用土培模拟试验研究了施用磷、钾肥对大田和温室土壤溶液电导率（EC）、离子含量及其比例的影响。结果表明,温室栽培土壤溶液EC、K+、Na+、Ca2+、Mg2+、NO3-含量以及K+ / Ca2+、K+ / Mg2+摩尔比分别为大田土壤的2.5、95.0、16.6、1.9、3.2、4.0、31.0和39.0倍,说明日光温室土壤离子累积及养分比例失调问题突出。施用磷、钾肥对土壤溶液中不同离子含量的影响不同,增加磷肥施用量,显著降低了大田和温室土壤溶液EC和Ca2+、Mg2+离子含量,而对土壤溶液K+、NO3--N和NH4+-N离子浓度均无显著影响;随施钾量增加,大田及温室土壤溶液EC、K+、Na+、Ca2+、Mg2+和K+/Ca2+、K+/Mg2+摩尔比均呈显著增加趋势。温室栽培实践中因过量施用磷、钾肥而造成的阳离子养分比例失调而带来的营养及生态环境问题值得关注。     

盐渍生境下野生琵琶柴盐分分布及泌盐特点

对干旱盐渍环境下野生琵琶柴泌盐结构、泌盐规律及其与土壤盐分、植物盐分分布的关系进行了研究。研究表明 ,生长在硫酸钠盐土上的琵琶柴体内Na 、SO2 -4含量较高 ,其次是Cl-、Mg2 和K ,Ca2 含量最低。在一天之中植物体内含盐量保持稳定 ,叶片盐分离子含量高于枝条。光学显微观察显示 ,琵琶柴叶片具有多细胞盐腺 ,可分泌K 、Na 、Ca2 、Mg2 、Cl-和SO2 -4。其分泌细胞对于离子的分泌作用受到温度及昼夜变化的影响 ,表现为上午的分泌量高于下午 ,白昼高于夜间。盐腺对于不同离子的分泌速率表现为 :对于Cl-的分泌最高 ,其次是Na 和SO2 -4,而对于K 的分泌高于对Ca2 、Mg2 的分泌。但与植物叶片含盐量相比 ,琵琶柴盐腺对于Cl-的相对分泌远高于其他离子 ,分泌的盐分中Na/K比值高于植物体Na/K比值。以上结果表明 ,琵琶柴体内盐分离子含量与土壤盐分离子含量及其自身对于元素的吸收特性有关 ;而盐腺对于盐分的分泌作用在受到温度变化影响的同时 ,对离子分泌具有较高的选择性。琵琶柴对于不同元素的这种选择性吸收及分泌特性对适应盐渍生境有一定意义。     

外源 GSH 对 NaCl 胁迫下番茄幼苗叶片及根系离子微域分布的影响

【目的】盐胁迫是限制新疆番茄生长的重要障碍因子之一,而外源喷施谷胱甘肽 (GSH) 是解决这一问题的有效措施。探讨外源 GSH 缓解番茄盐胁迫的效应和作用机制,可为该措施的有效应用提供理论依据。 【方法】采用营养液栽培法,选用番茄品种‘中蔬四号’为试材。在营养液中加入 NaCl 100 mg/L,使其产生盐胁迫,以不加 NaCl 作为对照 (CK),试验处理包括不喷施 GSH (NaCl)、喷施 GSH (+ GSH)、喷施 GSH 合成酶抑制剂 (+ BSO) 以及喷施 GSH 和 BSO (+ BSO + GSH)。测定番茄幼苗叶片和根系中与耐盐性相关的 K+、Ca2+、Mg2+、Na+ 和 Cl– 的离子微域分布状态和平衡。 【结果】NaCl 胁迫下番茄叶片和根系所有组织细胞中 Na+ 和 Cl– 相对含量显著提高,K+ 相对含量和 K+/Na+、Ca2+/Na+、K+/Cl– 比值降低,说明 NaCl 胁迫使细胞中 Na+ 和 Cl– 有害离子积累及胞内离子稳态严重破坏;外源 BSO 施用进一步加剧了 NaCl 胁迫下番茄叶片和根系细胞的 K+/Na+ 失衡。而外源 GSH 施用抑制了 NaCl 胁迫下番茄叶片和根系对 Na+ 的吸收,降低了 Cl– 的相对含量,提高了 K+/Na+、Ca2+/Na+、K+/Cl– 比值。外源 GSH 亦使 NaCl+BSO 胁迫下番茄叶片各组织及根系中皮层、内皮层和中柱的 Na+ 未检出,根系和叶片各组织中 Cl– 相对含量显著降低,K+ 和 Ca2+ 相对含量及 K+/Na+、Ca2+/Na+、K+/Cl–、Ca2+/Cl– 比值显著提高。 【结论】外源 GSH 通过抑制盐胁迫下番茄叶片和根系对 Na+ 的吸收,降低 Cl– 吸收,改善细胞中离子的微域分布和维持离子平衡, 从而缓解了盐胁迫对番茄的毒害作用,提高了番茄的耐盐性。     

The regulation of accumulation and secretion of several major inorganic cations by Chinese Iris under NaCl stress

Chinese Iris (Iris lactea Pall. var. chinensis (Fisch.) Koidz.) is a monocotyledonous halophyte, which is considered an important salt-tolerant species. In this study, the plant growth, ion absorption and transportation and leaf secretion characteristics of Iris under sodium chloride (NaCl) stress were investigated using nutrient solutions with four NaCl concentrations ranging from 0 to 300 mmol L^?1. The main results indicated that Na⁺ secretion accounted for 5.7–11.5% of the ion distribution pattern of 90% of the ions accumulated in vivo by Iris. The ion transportation ratio was potassium > magnesium > calcium > sodium, (K⁺ > Mg²⁺ > Ca²⁺ > Na⁺), K⁺/Na⁺, Ca²⁺/Na⁺, Mg²⁺/Na⁺ in the shoot were greater than those in the root. K–Na and Ca–Na selectivity ratios showed an increasing trend overall. The contribution of salt secretion to the salt tolerance of Iris was tiny, which will be discussed in further research, achieving ion balance in vivo through selective absorption and transportation under salt stress is undoubtedly a primary salt-tolerance adaptation mechanism of Iris.     

The effects of feeding byOniscus asellus (Isopoda) on nutrient cycling in an incubated hardwood forest soil

Summary Oniscus asellus produced changes in the nutrients leached from Oie and Oa horizons of a hardwood forest soil. Soil with isopods lost more K⁺ (54%) from the Oie horizon and more Ca²⁺ (25%), Mg²⁺ (40%), and water-extractable S (23%) from the Oa horizon than soil without isopods. In contrast, soils with isopods lost less Ca²⁺ (39076) from the Oie horizon and less dissolved C-bonded S (33%) from the Oa horizon than soil without isopods. In addition, the Oia and Oa horizons exhibited different nutrient dynamics. When isopods were present, the Oa horizon leachates accumulated more Na⁺ K⁺, Ca²⁺, Mg²⁺, NO₃ ^– , water-soluble SO₄ ^2–, and dissolved C-bonded S, and the Oie horizon retained more of these nutrients. The type of leaching solution also had a major effect on nutrients. Leaching with a simulated soil solution resulted in smaller nutrient losses for K⁺ and Mg²⁺ in both horizons and for Na⁺, Ca²⁺, and NO₃ ^– in the Oa horizon than leaching with distilled water.     

Sodium‐calcium interactions with growth,water, and photosynthetic parameters in salt‐treated beans

Calcium (Ca²⁺) amelioration of the plant's growth response to salinity depends on genetic factors. In this work, supplemental Ca²⁺ did not improve growth in Phaseolus vulgaris L. cv. Contender under high‐saline conditions and negatively affected several physiological parameters in nonsalinized plants. The response to supplemental Ca²⁺ was examined using plants grown in 25% modified Hoagland solution at different Na⁺ : Ca²⁺ ratios. In control plants (1 mM Ca²⁺; 1 mM Na⁺) surplus Ca²⁺ (4 or 10 mM) was associated with stomatal closure, decrease of hydraulic conductivity, sap flow, leaf specific dry weight, leaf K⁺ and leaf Mg²⁺ concentrations, and inhibition of CO₂ assimilation. Leaf water content was enhanced, while water‐use efficiency and dry matter were unaffected during the 15 d experimental period. The Ca²⁺ effect was not cation‐specific since similar results were found in plants supplied with high external Mg²⁺ or with a combination of Ca²⁺ and Mg²⁺. Relative to control plants, salinization (50 and 100 mM NaCl) caused a decrease in dry matter, hydraulic conductivity, sap flow, leaf Mg²⁺ activity, and inhibition of stomatal opening and CO₂ assimilation. However, NaCl (50 and 100 mM NaCl) enhanced leaf K⁺ concentration and water‐use efficiency. At 100 mM NaCl, leaf water content also significantly increased. Supplemental Ca²⁺ had no amelioration effect on the salt‐stress response of this bean cultivar. In contrast, the 50 mM–NaCl treatment improved stomatal conductance and CO₂‐assimilation rate in plants exposed to the highest Ca²⁺ concentration (10 mM). Phaseolus vulgaris is classified as a very NaCl‐sensitive species. The similarities in the effects caused by supplemental Ca²⁺, supplemental Mg²⁺, and NaCl salinity suggest that P. vulgaris cv. Contender has a high non‐ion‐specific salt sensitivity. On the other hand, the improvement in gas‐exchange parameters in Ca²⁺‐supplemented plants by high NaCl could be the result of specific Na⁺‐triggered responses, such as an increase in the concentration of K⁺ in the leaves.     

外加盐对凉粉草胶溶液的耐盐性和分子链刚性度的影响

在有盐环境下贮藏和加工凉粉草胶必须了解其多糖分子对盐的敏感性，该文绘制了凉粉草胶多糖在不同离子强度NaCl、KCl、MgCl₂和CaCl₂溶液中的Huggins'图，分别计算其分子链在这4种离子溶液中的耐盐度S、链刚性度B等值，结果发现：凉粉草胶多糖在4种离子溶液中，其耐盐性由强到弱的顺序为:K⁺>Na⁺>Mg⁺⁺>Ca⁺⁺，其分子链的构象在4种离子溶液中由柔到刚的顺序为:K⁺>Na⁺>Mg⁺⁺>Ca⁺⁺，这说明凉粉草胶多糖适合在KCl溶液中贮藏和加工。与其他多糖分子链在NaCl溶液中的B值比较后发现，凉粉草胶多糖的分子链构象较海藻酸钠要刚，较黄原胶要柔，这说明凉粉草胶比黄原胶更适合在NaCl溶液中贮藏和加工。     

Edaphic characterization and soil ionic composition influencing plant zonation in a semiarid Mediterranean salt marsh

Soil characteristics and plant zonation were studied in a semiarid Mediterranean salt marsh in SE Spain. According to topographic sequences and plants distribution, two transects were established from the border of La Mata lagoon to the upland vegetation limit and soils were described and analysed. Regularly spaced plots were established in these transects in accordance with the stands of vegetation and surface soil samples were taken every 2 months for 2 years. The following edaphic factors were determined: soil moisture content, pH and concentration of Cl⁻, SO₄²⁻, Ca²⁺, Mg²⁺, Na⁺ and K⁺ in the saturation extract. In addition, the groundwater level was measured and the duration of the flooding periods established in each plot. Soil–plant relationships were studied by means of canonical correspondence analysis. Based on rainfall data for the study period, dry and wet seasons were separated and the habitats of the plant communities were compared for salt quantity and quality independently for each season. Soils were classified, according to FAO (1998), as Hypercalcic, Sodic and Mollic Solonchaks and Hypercalcic Sodic Calcisols. The most important variables which explained plant zonation were: the flooding period, total salinity, minimum Ca²⁺/Na⁺ ratio and the mean sodium adsorption ratio. When the habitats of the main plant communities were compared, differences in salt quantity, quality and seasonal variations were found. Two chenopod shrubs, Arthrocnemum macrostachyum and Sarcocornia fruticosa, predominated in the most saline areas. More pronounced seasonal variations in soil salinity were found in the A. macrostachyum zone than in the Sarcocornia fruticosa zone. The highest value for K⁺/Na⁺ and Ca²⁺/Na⁺ ratios were measured in the Suaeda vera stand. The Lygeum spartum zone was distinguished by the high Ca²⁺/Na⁺ and Ca²⁺/Mg²⁺ ratios in the wet period. Among the rushes, Schoenus nigricans predominated in the less saline areas, where the K⁺/Na⁺ ratio was higher and the Ca²⁺/Na⁺ ratio lower than where Juncus maritimus predominated. Limonium cossonianum communities occupied an intermediate position with respect to soil salinity, between the chenopod shrubs and the other communities.Our results suggest that salt marsh plant zonation is influenced by temporal and spatial edaphic gradients which must be jointly considered if soil–plant relationships in saline soils are to be fully understood.     

基于地理加权回归模型的博斯腾湖湖滨绿洲土壤盐分离子含量高光谱估算

以博斯腾湖湖滨绿洲为研究区,分析HCO_3~–、Cl~–、SO_4~(2–)、Ca~(2+)、Mg~(2+)、Na~++K~+等主要土壤盐分离子含量与土壤高光谱反射率的分数阶微分光谱变换与RSI、DSI、NDSI等二维土壤指数的相关性优选特征波段,构建基于地理加权回归模型的土壤盐分离子含量估算模型。研究结果表明:Na~++K~+的微分变换特征波段集中在468～724 nm与1 182～1 539 nm,二维土壤指数的特征波段集中在1 742～2 395 nm,基于RSI的特征波段优选下地理加权回归模型对Na~++K~+含量的估算效果较好,建模集R~2=0.94,RMSE=0.22,验证集R~2=0.74,RMSE=0.19;SO_4~(2–)含量在1.2阶优选的位于469～636 nm波段估算效果较佳,建模集R~2=0.91,RMSE=0.02,验证集R~2=0.75,RMSE=0.33;Ca~(2+)、Mg~(2+)优选的特征波段主要集中在912～2 340 nm的近红外波段;Cl~–含量在1阶的近红外波段建模效果较好,建模集R~2=0.74,RMSE=0.03,验证集R~2=0.93,RMSE=0.11;含量相对较高的Na~++K~+、SO_4~(2–)、Cl~–的地理加权回归模型精度高于含量较低的Ca~(2+)、Mg~(2+)。     

天津市滨海盐碱地刺槐种植区水盐动态变化规律

[目的]通过对滨海地区盐碱土水盐动态变化规律的研究,为该地区的土壤利用以及植树造林提供科学依据。[方法]以天津大港地区刺槐林土壤为研究对象,研究不同土层的土壤水盐年份变化和盐分离子分布特征。[结果]试验地土壤全年含水量变化范围在11.9%~28.8%;含盐量变化范围在4.2%~18.4%。春(3—5月)秋(9—11月)季节土壤含水量低,含盐量高,土壤盐分含量随土层深度增加逐渐降低;夏季(6—8月),土壤含水量高,含盐量低,土壤盐分含量随土层深度的增加逐渐升高。pH值在7.37~8.39之间,土壤中K+,Na+,Ca2+,Mg2+和Cl-春季表层土壤(0—10cm)含量最高,分别为0.04,4.27,2.69,1.04和10.03g/kg。除SO2-4和HCO-3外,其他盐分离子在春季变异系数(29.99~162.98)明显大于夏秋季节(2.87~88.13)。[结论]不同土层的土壤含水量和含盐量随当地降雨量呈明显的季节性变化;试验地区土壤属于碱性土壤,随季节变化不明显;K+,Na+,Ca2+,Mg2+和Cl-与含盐量变化趋势保持一致,SO2-4和HCO-3随季节变化没有明显的规律性;春季各盐分离子在土壤中分布极为不均。