咸水沟灌对棉田土壤水稳性团聚体稳定性的影响

探明咸水沟灌对土壤水稳性团聚体的影响对实现咸水资源安全高效利用具有重要意义。本研究在棉花长期定位咸水沟灌试验(始于2006年)的基础上,分析了不同矿化度(1、2、4、6、8、10 g·L^-1)咸水连续灌溉第10年和第15年棉田土壤盐分和水稳性团聚体稳定性的变化特征。结果表明: 沟底0~30 cm土层土壤盐分随灌溉水矿化度的升高而增加,其中6、8、10 g·L^-1灌水处理与1 g·L^-1处理间差异达显著水平;随着土层深度的增加,各处理土壤盐分逐渐增大。咸水沟灌有降低沟底土壤水稳性团聚体稳定性的趋势,当灌溉水矿化度≥6 g·L^-1时,水稳性大团聚体(>0.25 mm)质量分数、团聚体平均重量直径和几何平均直径显著降低,分形维数和平均重量比表面积显著增大;随着土层深度的增加,各处理土壤水稳性团聚体稳定性下降。连续多年咸水沟灌条件下,各处理棉田沟底0~30 cm土层土壤盐分和水稳性团聚体稳定性未随灌水年限的增加而逐年积累与恶化。在本研究灌溉制度下,采用≤4 g·L^-1咸水沟灌对试验区棉田土壤盐分和水稳性团聚体稳定性指标无显著影响。     

咸水灌溉对冬小麦籽粒品质特性和产量的影响

为缓解农业用水供需矛盾,解决井灌区地下水超采问题,探究华北平原广泛分布的地下咸水灌溉对冬小麦品质和产量的影响,实现农业可持续发展,本研究在始于2006年的长期定位试验基础上,设置1、2、4、6、8 g·L^-1共5个灌溉水矿化度处理,其中1 g·L^-1灌溉水(取自当地地下水)为对照,研究咸水灌溉对冬小麦籽粒品质特性和产量性状的影响。结果表明: 与对照相比,当灌溉水矿化度≥4 g·L^-1时可显著增加籽粒吸水量、面团形成时间、沉淀值、湿面筋和粗蛋白含量,但显著降低出粉率、面团稳定时间和面筋指数;长期灌溉高矿化度咸水(4～8 g·L^-1)显著降低了冬小麦穗数(44.0%～60.7%)和籽粒产量(35.6%～64.7%)。在连续多年咸水灌溉条件下,与对照相比,2 g·L^-1灌水处理对籽粒产量及产量构成因素无显著影响,且能提高吸水量、面团形成时间、沉淀值、湿面筋和粗蛋白含量等籽粒品质。采用主成分分析法对冬小麦产量性状和品质特性进行综合性评价,得出2 g·L^-1灌水处理综合效果最优。本研究可为华北平原咸水资源高效利用提供理论支撑。     

咸水灌溉条件下土壤水盐分布特征

通过设置3种灌水量水平（100%ET_c、80%ET_c、60%ET_c）和3种灌水水质水平（0.7、3和6 g·L^-1）,研究了咸水灌溉条件下春小麦120 cm土层内水分动态和盐分累积特征.结果表明：水分在农田土壤中的分布主要受灌水量和土壤质地的影响,充分灌溉使水分存贮在较深土层中,而非充分灌溉则使水分存贮在表层;在相同灌水量的条件下,土体内的盐分积累程度随着灌溉水矿化度的增大而加剧;在相同矿化度条件下,土体内的盐分含量及积盐深度随着灌水量的增加而增大.在作物整个生育期内,连续使用咸水灌溉将导致土壤积盐,且非充分灌溉较充分灌溉更易使土壤表层积盐.     

高水位区暗管埋设下土壤盐分适时立体调控的生态效应

高水位地区作物生长关键期采用微咸水或咸水灌溉被证明在一定条件下可以起到增产正效应,但同时却存在着土体盐分积累及其对下茬或次年种植影响的生态负效应.为探讨消除或抑制微咸水或咸水灌溉对土壤盐分积累的生态负效应,保证作物种植增产的正效应,本文在河北近滨海高水位盐碱区开展了为期2年的试验研究,探讨了旱季微咸水或咸水灌溉带来的盐分异位积累与离子分布变化特征,分析了雨季关键期暗管适时排盐对土壤盐分的立体调控生态效应.结果表明：旱季咸水灌溉后土壤经历“积盐-脱盐-二次积盐”3个阶段;灌溉初期,1 g·L^-1咸水灌溉处理下0～50 cm土体脱盐,土壤含盐量随土壤深度增加而增加,HCO₃^-含量增加,其他离子含量降低;6与13 g·L^-1咸水灌溉处理下0～50 cm土体积盐,土壤含盐量随土壤深度增加而降低,HCO₃^-含量降低,其他离子含量增加;雨季暗管适时立体调控脱盐效果显著,土壤脱盐率达16.0%～45.7%,同降雨量下,降水分布越集中,脱盐效果越好;周年时间尺度上,咸水灌溉小区土壤积盐量小于对照区;咸水灌溉处理小区冬小麦产量显著高于对照处理,1 g·L^-1 处理高于6与13 g·L^-1处理.     

外源甜菜碱对水分胁迫下桃树生理响应的影响

以4年生盆栽“庆丰”桃树为试材,研究了水分胁迫下桃树叶片中甜菜碱含量的变化规律及叶面喷施甜菜碱对水分胁迫下桃树生理响应的影响.结果表明：正常供水情况下,桃树叶片中甜菜碱含量为75.9～80.5 μg·g^-1FM , 随着水分胁迫程度的加深,甜菜碱含量逐渐增加,停水第16 天时达278.9 μg·g^-1FM ;正常供水时桃叶片细胞质膜透性为8.06%～8.61%,水分胁迫下增至28.62%,叶面喷施100和500 mg·L^-1甜菜碱16d后分别为26.25%和21.79%;过氧化氢(H₂O₂)含量由正常情况下的27.2～32.5 μmol·g^-1FM 增至胁迫后的76.4 μmol·g^-1FM,叶面喷施100和500 mg·L^-1甜菜碱后分别为73.2和68.5 μmol·g^-1 FM;水分胁迫下,抗坏血酸过氧化物酶(AsA-POD)活性峰值为0.435 mg·g^-1 FM,甜菜碱处理后峰值达到0.490 mg·g^-1 FM;游离脯氨酸与可溶性糖在干旱胁迫下逐渐累积, 500 mg·L^-1甜菜碱处理分别为2.878 mg·g^-1 FM和37.6 mg·g^-1 FM,均低于单纯胁迫及100 mg·L^-1甜菜碱处理;可溶性蛋白质含量在水分胁迫下呈下降趋势,甜菜碱处理后最小值为4.03 mg·g^-1 FM,较单纯胁迫下的最低值（3.14 mg·g^-1 FM）高20.3%.表明叶面喷施甜菜碱能在一定程度上减轻桃树的受害程度,提高其抗旱性.     

化学诱抗剂诱导黄瓜抗盐性及其机理

在200 mmol·L^-1 NaCl胁迫条件下,采用根际注射结合叶面喷洒的诱导方法探讨了不同浓度水杨酸、油菜素内酯、壳聚糖、亚精胺4种化学诱抗剂对黄瓜幼苗生长及其生理生化特性的影响.结果表明,4种化学诱抗剂在适宜浓度范围内,显著地降低了黄瓜幼苗的盐害指数和死苗率,以油菜素内酯0.01 mg·L^-1降低幅度最大,比对照分别降低了63.0%和75.0%;显著地促进了超氧化物歧化酶、过氧化物酶、过氧化氢酶等保护酶活性,从而显著降低了丙二醛含量和电解质渗出率,干重含水量显著升高;促进了幼苗的形态建成,植株茎粗、展开叶数及壮苗指数显著提高,壮苗指数以壳聚糖150 mg·L^-1最大,比对照提高了30.9%.说明施用适宜浓度的化学诱抗剂可以诱导黄瓜幼苗的抗盐能力,减缓盐害症状.综合作用效果依次为：油菜素内酯0.005～0.05 mg·L^-1、亚精胺150～200 mg·L^-1、壳聚糖100～200 mg·L^-1和水杨酸50～150 mg·L^-1.     

凋落物添加条件下咸水灌溉对风沙土CO2排放及化学性质的影响

沙拐枣作为塔克拉玛干沙漠公路防护林主要优势物种之一,其凋落物在该区域的碳循环过程中具有重要作用。采用室内培养试验测定了沙拐枣凋落物添加后,在25%、50%、75%、100%田间持水量的咸水(SW)和淡水(FW)灌溉条件下,风沙土CO₂排放、土壤有机碳(SOC)、可溶性有机碳(DOC)、pH和电导率(EC)的动态变化。结果表明: 咸水灌溉对土壤CO₂排放具有抑制作用,在4种土壤含水量处理下,淡水灌溉比咸水灌溉的CO₂累积排放量增加1.9%～29.1%;土壤CO₂累积排放量随土壤含水量的增加而升高;在沙拐枣凋落物添加条件下,SOC在前期迅速下降,但后期所有处理SOC均逐渐升高后趋于稳定;培养结束时,各处理DOC含量比培养前提高了41.3%～92.4%;在培养结束时各处理与培养前相比pH升高了0.20～0.35;EC随土壤含水量的增加而升高,培养结束时在4种含水量条件下,咸水灌溉下EC比培养前增加了0.11～0.79 mS·cm^-1,而淡水灌溉下EC比培养前有增有减。土壤CO₂累积排放量与SOC、DOC、pH呈显著正相关,但与土壤含水量相关性不显著。凋落物添加条件下咸水灌溉以及较低的含水量条件均能抑制风沙土CO₂的排放,EC受灌溉水质和土壤含水量的影响较大。     

微咸水滴灌对土壤酶活性、CO2通量及有机碳降解的影响

利用微咸水灌溉是解决干旱区水资源短缺的重要途径.通过田间小区滴灌试验,研究了不同矿化度微咸水(0.31、3.0、5.0 g·L^-1,NaCl浓度)对土壤过氧化氢酶、蔗糖酶、多酚氧化酶、β-葡萄糖苷酶和纤维素酶活性的影响,采用土壤碳通量和物料袋法研究了土壤CO₂通量和有机碳降解对微咸水滴灌的响应.结果表明: 微咸水(3.0 g·L^-1)处理下蔗糖酶、β-葡萄糖苷酶、纤维素酶的活性分别比淡水处理降低31.7%～32.4%、29.7%～31.6%、20.8%～24.3%,而土壤多酚氧化酶活性则随灌溉水矿化度提高而显著升高,在膜下微咸水、咸水处理多酚氧化酶较淡水处理提高2.4%、20.5%.土壤微生物生物量碳和微生物熵均随灌溉水矿化度提高呈降低趋势,而代谢熵则呈升高趋势.不同处理对土壤CO₂通量影响表现为淡水＞微咸水≥咸水,且膜下CO₂通量显著高于膜间(P<0.05),棉花吐絮期(9月20日)膜下淡水处理较咸水和微咸水处理的CO₂通量分别升高29.8%、28.2%,微咸水滴灌显著降低了土壤CO₂通量.不同矿化度微咸水滴灌对有机物(棉花和苜蓿秸秆)的降解率表现为淡水＞微咸水＞咸水,膜下有机物降解显著高于膜间.在培养第125天时,咸水、微咸水、淡水处理的膜间棉花秸秆回收率分别为39.7%、36.3%、30.5%,膜间苜蓿秸秆回收率分别为46.5%、36.5%、35.4%.微咸水灌溉明显抑制了北疆滴灌棉田土壤酶活性,造成土壤微生物量和CO₂通量下降,土壤有机物降解率降低,使绿洲农田土壤生物性状变差.     

龙须菜对重金属铜胁迫的生理响应

研究了大型海藻龙须菜(Gracilaria lemaneiformis)对不同浓度重金属铜(0、25、50、100、250和500 μg·L^-1)胁迫的生理响应.结果表明:当Cu²⁺浓度≥50 μg·L^-1时,龙须菜藻体的相对生长速率显著下降,最大光化学量子产量、最大相对电子传递速率和相对电子传递效率呈相同的变化趋势.随着Cu²⁺浓度的升高,龙须菜藻体最大净光合速率和光饱和点显著降低,而光补偿点显著升高,叶绿素a、类胡萝卜素和藻胆蛋白含量则呈先升高后下降的趋势;当Cu²⁺浓度达到500 μg·L^-1时,叶绿素a、类胡萝卜素和藻胆蛋白含量显著下降.说明龙须菜在低浓度Cu²⁺胁迫下具有一定的抵抗能力,而当Cu²⁺浓度≥50 μg·L^-1时,会对藻体生理活动造成显著的抑制作用.     

微咸水滴灌对土壤酶活性、CO2通量及有机碳降解的影响

利用微咸水灌溉是解决干旱区水资源短缺的重要途径.通过田间小区滴灌试验,研究了不同矿化度微咸水(0.31、3.0、5.0 g·L^-1,NaCl浓度)对土壤过氧化氢酶、蔗糖酶、多酚氧化酶、β-葡萄糖苷酶和纤维素酶活性的影响,采用土壤碳通量和物料袋法研究了土壤CO₂通量和有机碳降解对微咸水滴灌的响应.结果表明: 微咸水(3.0 g·L^-1)处理下蔗糖酶、β-葡萄糖苷酶、纤维素酶的活性分别比淡水处理降低31.7%～32.4%、29.7%～31.6%、20.8%～24.3%,而土壤多酚氧化酶活性则随灌溉水矿化度提高而显著升高,在膜下微咸水、咸水处理多酚氧化酶较淡水处理提高2.4%、20.5%.土壤微生物生物量碳和微生物熵均随灌溉水矿化度提高呈降低趋势,而代谢熵则呈升高趋势.不同处理对土壤CO₂通量影响表现为淡水＞微咸水≥咸水,且膜下CO₂通量显著高于膜间(P<0.05),棉花吐絮期(9月20日)膜下淡水处理较咸水和微咸水处理的CO₂通量分别升高29.8%、28.2%,微咸水滴灌显著降低了土壤CO₂通量.不同矿化度微咸水滴灌对有机物(棉花和苜蓿秸秆)的降解率表现为淡水＞微咸水＞咸水,膜下有机物降解显著高于膜间.在培养第125天时,咸水、微咸水、淡水处理的膜间棉花秸秆回收率分别为39.7%、36.3%、30.5%,膜间苜蓿秸秆回收率分别为46.5%、36.5%、35.4%.微咸水灌溉明显抑制了北疆滴灌棉田土壤酶活性,造成土壤微生物量和CO₂通量下降,土壤有机物降解率降低,使绿洲农田土壤生物性状变差.     

壳聚糖包衣对油菜种子萌发及幼苗耐盐性影响

以不同浓度的壳聚糖对油菜种子进行包衣处理,考察其对油菜种子萌发及幼苗耐盐性的影响,并在不同盐浓度胁迫条件下对种子萌发时的发芽势、发芽率、生物量（鲜重、干重、根长、芽长）等指标进行测定,同时分析油菜幼苗叶绿素含量、可溶性蛋白及可溶性糖含量的变化。结果表明,一定浓度的壳聚糖包衣处理可提高油菜种子发芽率、发芽势、生物量、幼苗的耐盐指数、叶绿素含量、可溶性蛋白及可溶性糖的含量,其中浓度为0.25 g·L^-1壳聚糖包衣处理对油菜种子萌发的促进效果较好,而浓度为0.50 g·L^-1壳聚糖包衣处理对提高油菜幼苗耐盐性具有较好的促进作用。     

Crop production and management under saline conditions

Summary This review evaluates management practices that may minimize yield reduction under saline conditions according to three strategies: (I) control of root-zone salinity; (II) reduced damage to the crop; (III) reduced damage to individual plants. Plant response to salinity is described by an unchanged yield up to a threshold soil salinity (a), then a linear reduction in relative yield (b), to a maximum soil salinity that corresponds to zero yield (Y_o). Strategies I and II do not take into consideration any change in the parameters of the response curve, while strategy III is aimed at modifying them.Control of root zone salinity is obtained by irrigation and leaching. From the review of existing data it is concluded that the effective soil salinity parameter should be taken as the mean electrical conductivity of the saturated paste extract or of the soil solution over time and space. Several irrigation and leaching practices are discussed. It is shown that intermittent leaching is more advantageous than leaching at each irrigation. Specific cultivation and irrigation practices that result in soil salinity reduction adjacent to young seedlings and the use of water of low salinity at specifically sensitive growth stages may be highly beneficial. Recent data do not show that reduced irrigation intervals improve crop response more under saline than under nonsaline irrigation. Alternate use of water of different salt concentrations results in mixing in the soil and the crop responds to the mean water salinity.Reduced damage at the fiel level when soil or irrigation water salinity is too high to maintain full yield of single plants requires a larger crop stand. For row crops reduced inter-row spacing is more effective than reduced intra-row spacing.Reduced damage at the plant level while the salinity tolerance of the plants remains constant shows up in the response curve parameters as larger threshold and slope and constant salinity at zero yield. This is the effect of a reduced atmospheric water demand that results in reduced stress in the plant under given salinity. Management can also change the salt tolerance of the crop. This will show up as higher salinity at zero yield, as well as changes in threshold and slope. Such changes in the response curve were found at different growth stages, under different atmospheric CO₂, under different fertilization, and when sprinkler irrigation was compared with drip irrigation.Contribution from the Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel. No. 1111-E 1984 series.     

濒危植物珙桐的组织培养与植株再生

以珙桐冬芽为材料进行组织培养和植株再生研究,结果表明：珙桐冬芽直接诱导丛生芽的最适培养基为WPM+NAA 0.2 mg·L^-1+6-BA 3.0 mg·L^-1+AC 2.0 g·L^-1;珙桐带芽茎段增殖的适宜培养基为WPM+NAA 0.05 mg·L^-1+6-BA 1.0 mg·L^-1+GA₃ 2.0 mg·L^-1+AC 2.0 g·L^-1;生根最佳培养基为White+IBA3.0 mg·L^-1+6-BA 1.0 mg·L^-1+AC 2.0 g·L^-1,在此条件下,根发育良好,植株健壮;组培苗炼苗后移栽,成活率可达80%。     

Soil Salt Distribution and Tomato Response to Saline Water Irrigation under Straw Mulching

To investigate better saline water irrigation scheme for tomatoes that scheduling with the compromise among yield (Y_t), quality, irrigation water use efficiency (IWUE) and soil salt residual, an experiment with three irrigation quotas and three salinities of irrigation water was conducted under straw mulching in northern China. The irrigation quota levels were 280 mm (W1), 320 mm (W2) and 360 mm (W3), and the salinity levels were 1.0 dS/m (F), 3.0 dS/m (S1) and 5.0 dS/m (S2). Compared to freshwater, saline water irrigations decreased the maximum leaf area index (LAI_m) of tomatoes, and the LAI_m presented a decline tendency with higher salinity and lower irrigation quota. The best overall quality of tomato was obtained by S2W1, with the comprehensive quality index of 3.61. A higher salinity and lower irrigation quota resulted in a decrease of individual fruit weight and an increase of the blossom-end rot incidence, finally led to a reduction in the tomato Y_t and marketable yield (Y_m). After one growth season of tomato, the mass fraction of soil salt in plough layer under S2W1 treatment was the highest, and which presented a decline trend with an increasing irrigation quota. Moreover, compared to W1, soil salts had a tendency to move to the deeper soil layer when using W2 and W3 irrigation quota. According to the calculation results of projection pursuit model, S1W3 was the optimal treatment that possessed the best comprehensive benefit (tomato overall quality, Y_t, Y_m, IWUE and soil salt residual), and was recommended as the saline water irrigation scheme for tomatoes in northern China.     

咸水灌溉对沙土土壤盐分和胡杨生理生长的影响

通过咸水灌溉沙土土质生长的幼龄胡杨,分析了咸水灌溉沙土土壤盐分分布累积特点、盐分胁迫对胡杨的耗水生长关系、叶绿素、Pro、MDA的影响,结果表明:(1)在1.2—3 g/L范围内,微咸水灌溉沙土处于脱盐状态,6—12 g/L咸水灌溉使沙土积盐大增。在整个生长周期内,微咸水和咸水灌溉,0—200 cm内土体的总盐都呈累积趋势。(2)咸水灌溉胡杨,不同盐分处理的生长耗水关系可以用对数模型描述。(3)盐分胁迫下,胡杨叶片内叶绿素含量呈抛物线递减,Pro和MDA含量则呈现抛物线递增趋势。说明短期内咸水灌溉对土壤安全和胡杨的生长影响有限,可用咸水解决生态缺水现状,3种生理指标可用来衡量胡杨的盐胁迫程度,以此为指导提高人工造林的成活率。     

基于比较优势分析法的冬小麦产量差异

在农户调查基础上,采用比较优势分析法对曲周县2003—2004年度冬小麦产量差异进行分析.调查数据表明,地块间小麦产量差异较大,产量范围为在4.2～7.9 t·hm-²,变异系数为0.14.通过逐步回归建立的由土壤盐碱度、土壤肥力、是否咸水灌溉、品种选择、返青期追施氮肥类型、播种时间、病虫害防治和返青期是否水分胁迫8个因子构成的产量差模型可以解释63%的产量差异.其中土壤盐碱度、土壤肥力和是否咸水灌溉是冬小麦的主要产量限制因子,其引起的产量差为727 kg·hm^-2,占总模拟产量差的52%.小麦品种引起的产量差为202.1 kg·hm^-2,占总模拟产量差的14%.播种时间、返青期追施氮肥类型、病虫害防治和返青期是否水分胁迫4个因子引起的产量差分别占总模拟产量差的7%、14%、10%和3%.因此,除土壤和气候状况外,管理措施也是造成产量差异的重要因素,通过优化管理措施可以大大减小产量差异.     

Oxygation Enhances Growth, Gas Exchange and Salt Tolerance of Vegetable Soybean and Cotton in a Saline Vertisol

Impacts of salinity become severe when the soil is deficient in oxygen. Oxygation (using aerated water for subsurface drip irrigation of crop) could minimize the impact of salinity on plants under oxygen-limiting soil environments. Pot experiments were conducted to evaluate the effects of oxygation (12% air volume/volume of water) on vegetable soybean (moderately salt tolerant) and cotton (salt tolerant) in a salinized vertisol at 2, 8, 14, 20 dS/m ECe. In vegetable soybean, oxygation increased above ground biomass yield and water use efficiency (WUE) by 13% and 22%, respectively, compared with the control. Higher yield with oxygation was accompanied by greater plant height and stem diameter and reduced specific leaf area and leaf Na+ and Cl-concentrations. In cotton, oxygation increased lint yield and WUE by 18% and 16%, respectively, compared with the control, and was accompanied by greater canopy light interception, plant height and stem diameter. Oxygation also led to a greater rate of photosynthesis, higher relative water content in the leaf, reduced crop water stress index and lower leaf water potential. It did not, however, affect leaf Na+ or Cl- concentration. Oxygation invariably increased, whereas salinity reduced the K+ : Na+ ratio in the leaves of both species. Oxygation improved yield and WUE performance of salt tolerant and moderately tolerant crops under saline soil environments, and this may have a significant impact for irrigated agriculture where saline soils pose constraints to crop production.     

The Effects of Saline Water Drip Irrigation on Tomato Yield,Quality, and Blossom-End Rot Incidence --- A 3a Case Study in the South of China

Saline water resources are abundant in the coastal areas of south China. Most of these resources still have not been effectively utilized. A 3-year study on the effects of saline water irrigation on tomato yield, quality and blossom-end rot (BER) was conducted at different lower limits of soil matric potential (-10 kPa, -20 kPa, -30 kPa, -40 kPa and -50 kPa). Saline water differing in electrical conductivity (EC) (3 dS/m, 4 dS/m, 4.5 dS/m, 5 dS/m and 5.5 dS/m) was supplied to the plant after the seedling establishment. In all three years, irrigation water with 5.5 dS/m salinity reduced the maximum leaf area index (LAI_m) and chlorophyll content the most significantly when compared with other salinity treatments. However, compared with the control treatment (CK), a slight increase in LAI_m and chlorophyll content was observed with 3~4 dS/m salinity. Saline water improved tomato quality, including fruit density, soluble solid, total acid, vitamin C and the sugar-acid ratio. There was a positive relationship between the overall tomato quality and salinity of irrigation water, as analyzed by principal component analysis (PCA). The tomato yield decreased with increased salinity. The 5.5 dS/m treatment reduced the tomato yield (Y_t) by 22.4~31.1%, 12.6~28.0% and 11.7~27.3%, respectively in 2012, 2013 and 2014, compared with CK. Moreover, a significant (P≤0.01) coupling effect of salinity and soil matric potential on Y_t was detected. Saline water caused Y_t to increase more markedly when the lower limit of soil matric potential was controlled at a relatively lower level. The critical salinity level that produced significant increases in the BER_i was 3 dS/m~4 dS/m. Following the increase in BER_i under saline water irrigation, marketable tomato yield (Y_m) decreased by 8.9%~33.8% in 2012, 5.1%~30.4% in 2013 and 10.1%~32.3% in 2014 compared with CK. In terms of maintaining the Y_t and Y_m, the salinity of irrigation water should be controlled under 4 dS/m, and the lower limit of soil matric potential should be greater than -20 kPa.