Seasonal flooding,soil salinity and primary production in northern prairie marshes

Hydrologic regime is an important control of primary production in wetland ecosystems. I investigated the coupling of flooding, soil salinity and plant production in northern prairie marshes that experience shallow spring flooding. Field experiments compared whitetop (Scolochloa festucacea) marsh that was: (1) nonflooded, (2) flooded during spring with 25 cm water and (3) nonflooded but irrigated with 1 cm water · day^–1. Pot culture experiments examined whitetop growth response to salinity treatments. The electrical conductivity of soil interstitial water (EC_e) at 15 cm depth was 4 to 8 dS· m^–1 lower in flooded marsh compared with nonflooded marsh during 2 years. Whitetop aboveground biomass in flooded marsh (937 g · m^–2, year 1; 969 g · m^–2, year 2) exceeded that of nonflooded marsh (117 g · m^–2 year 1; 475 g · m^–2, year 2). Irrigated plots had lower EC_e and higher aboveground biomass than nonflooded marsh. In pot culture, EC_e of 4.3 dS · m^–1 (3 g · L^–1 NaCl) reduced total whitetop biomass by 29 to 44% and EC_e of 21.6 dS · m^–1 (15 g · L^–1 NaCl) reduced biomass by more than 75%. Large reductions of EC_e and increases of whitetop growth with irrigation indicated that plants responded to changes in soil salinity and not other potential environmental changes caused by inundation. The results suggest that spring flooding controls whitetop production by decreasing soil salinity during spring and by buffering surface soils against large increases of soil salinity after mid-summer water level declines. This mechanism can explain higher marsh plant production under more reducing flooded soil conditions and may be an important link between intermittent flooding and primary production in other wetland ecosystems.     

Response of wheat to subsoil salinity and temporary water stress at different stages of the reproductive phase

To examine the effects of subsoil NaCl salinity in relation to water stress imposed at different growth stages, wheat was grown in a heavy texture clay soil (vertosol) under glasshouse conditions in polythene lined cylindrical PVC pots (100 cm long with 10.5 cm diameter) with very low salinity level (EC_e 1.0 dS/m; ESP 1.0 and Cl 30 mg/kg soil) in top 10 cm soil (10–20 cm pot zone) and low salinity level (EC_e 2.5 dS/m, ESP 5, and Cl 100 mg/kg soil) in top 10–20 cm soil (20–30 cm pot zone). The plants were exposed to three subsoil salinity levels in the 20–90 cm subsoil (30–100 cm pot zone) namely low salinity (EC_e: 2.5 dS/m, ESP: 5, Cl: 100 mg/kg soil), medium salinity (EC_e: 4.0 dS/m, ESP: 10, Cl: 400 mg/kg) and high salinity (EC_e: 11.5 dS/m, ESP: 20, Cl: 1950 mg/kg) in the subsoil (20–90 cm soil layer: 30–100 cm pot zone). Watering of plants was withheld for 20 days commencing at either early booting or anthesis or mid grain filling, and then resumed until maturity, and these treatments were compared with no water stress. Water stress commencing at anthesis stage had the most depressing effect on grain yield and water use efficiency of wheat followed by water stress at grain filling stage and early booting stage. High subsoil salinity reduced grain yield by 39.1, 24.3%, and 13.4% respectively in plants water-stressed around anthesis, early booting, and mid grain filling compared with 36.6% in well-watered plants. There was a significant reduction in root biomass, rooting depth, water uptake and water use efficiency of wheat with increasing subsoil salinity irrespective of water regimes. Plants at high subsoil salinity had 64% of their root biomass in the top 0–30 cm soil and there was a marked reduction in subsoil water uptake. Roots also penetrated below the non-saline surface into salinised subsoil and led to attain high concentration of Na and Cl and reduced Ca/Na and K/Na ratio of flag leaf at anthesis stage. Results suggest that high subsoil salinity affects root growth and water uptake, grain yield and water use efficiency even in well water plants. Water stress at anthesis stage had the most depressing effect on wheat.     

Desodification from calcareous saline sodic soil through phytoremediation with Phragmites australis (Cav.) Trin. ex Steud. and gypsum

The reclamation of saline sodic soils requires sodium removal and the phytoremediation is one of the proven low-cost, low-risk technologies for reclaiming such soils. However, the role of Phragmites australis in reclaiming saline sodic soils has not been evaluated extensively. The comparative reclaiming role of P. australis and gypsum was evaluated in a column experiment on a sandy clay saline sodic soil with EC_e 74.7 dS m^?1, sodium adsorption ratio (SAR) 63.2, Na⁺ 361 g kg^?1, and pH 8.46. The gypsum at 100% soil requirement, planting common reed (P. australis) alone, P. australis + gypsum at 50% soil gypsum requirements, and leaching (control without plant and gypsum) were four treatments applied. After 11 weeks of incubation, the results showed that all treatments including the control significantly reduced pH, EC, exchangeable Na⁺, and SAR from the initial values, the control being with least results. The gypsum and P. australis + gypsum were highly effective in salinity (EC_e) reduction, while sodicity (SAR) and Na⁺ reductions were significantly higher in P. australis + gypsum treatment. The reclamation efficiency in terms of Na⁺ (83.4%) and SAR (86.8%) reduction was the highest in P. australis + gypsum. It is concluded that phytoremediation is an effective tool to reclaim saline sodic soil.     

Effects of residual soil salinity resulting from irrigation with sulphate waters on lettuce

Summary The response of lettuce (Lactuca sativa L.) to residual soil salinity as influenced by the ionic composition of two different saline waters (EC_w=3.1 dS/m, referenced at 25°C) and rain water, was investigated in a greenhouse experiment with three successive plantings of lettuce in the same soil. One of the saline waters was saturated with gypsum (SO₄=35 mol (−)m⁻³) and the other contained SO₄ at 15 mol (−)m⁻³ and Na and Cl at 18 and 14 mol (±)m⁻³, respectively (mixed water). All waters were applied with a 0.3 leaching fraction. Soil water salinity and sodium adsorption ratio (SAR) increased in both cases using saline waters. The effect of mixed saline water was higher and became more marked after each planting, resulting from higher contribution of Na and Cl to soil salinity. With both saline waters, soil solution became saturated with gypsum. At first planting, gypsum saturated and mixed waters produced fresh yield increases of 15 and 24%, respectively, relative to rain water. At second planting, however, there was reduction in yield of 11 and 22%, respectively, relative to rain water; at third planting yield reduced by 22 and 76% with gypsum saturated and mixed water, respectively.     

Salinity-yield response functions of barley genotypes assessed with a triple line source sprinkler system

Evaluation of the salt tolerance of crop cultivars under field conditions is greatly complicated by the typical temporal and spatial variability of soil salinity. We obtained the grain yield – salinity response functions of 124 barley genotypes by growing them in ten salinity treatments imposed by a Triple Line Source Sprinkler (TLS) system during five consecutive years. Additional objectives were to ascertain the consistency and reproducibility over years of these functions, to quantify the deleterious effects of saline sprinkling irrigations, and to assess correlations between salinity tolerance and leaf sap salt concentration. The consistency and reproducibility of the response functions within and between years were adequate (only 8% of the response functions were discarded for statistical reasons). The Y _m (grain yield without salinity) and the EC₅₀ (the EC _e that reduces yield by 50%) estimates were not correlated (P > 0.05) suggesting that the most productive genotypes were not necessarily less salinity tolerant. Y _m was positively and significantly (P < 0.01) correlated with Y₆ and Y₁₂ (fitted grain yields at EC _e values of 6 dS m^-1, and 12 dS m^-1, respectively), indicating that it is a useful statistic in the selection of barley genotypes most productive under medium and high salinities. Foliar salt uptake due to saline sprinkling irrigations decreased the EC₅₀ by around 50% as compared with the salinity tolerance obtained with surface irrigation systems. No consistent relationships were found between either Y _m or EC₅₀ and the leaf sap osmotic potential, Cl, Ca, Na and K concentrations. They could not therefore be used in screening for salinity tolerance of barley. On the basis of the evidence from the present study, Y _m is the best statistic for predicting the most productive barley genotypes in salt-affected soils. This revised version was published online in June 2006 with corrections to the Cover Date.     

Effect of soil and water salinity on tomato growth

The yield of tomatoes for processing (Lycopersicon esculentum var. VF145 B. 7879) grown in artificially salinized plots, was reduced by 10% for every 1.5 mmhos/cm increase in EC_e above 2.0 mmhos/cm. Yield reduction was the same for equal mean soil salinities regardless of leaching and the rate of salt accumulation in the soil. Total soluble solids content increased with increasing salinity to offset, to a large extent, the yield reduction. Reduction in water uptake, as a result of an increase in soil salinity was directly related to fruit yield reduction, but not to stover yield which was not affected by salinity. The salt tolerance during germination was similar to subsequent growth in the salinity range of this experiment.Contribution from the Agricultural Research Organization. The Volcani Center, Bet Dagan, Israel 1972. Series, No. 2225-E.Contribution from the Agricultural Research Organization. The Volcani Center, Bet Dagan, Israel 1972. Series, No. 2225-E.     

Growth of mycorrhizal tomato and mineral acquisition under salt stress

 High salt levels in soil and water can limit agricultural production and land development in arid and semiarid regions. Arbuscular mycorrhizal fungi (AMF) have been shown to decrease plant yield losses in saline soils. The objective of this study was to examine the growth and mineral acquisition responses of greenhouse-grown tomato to colonization by the AMF Glomus mosseae [(Nicol. And Gerd.) Gerd. and Trappe] under varied levels of salt. NaCl was added to soil in the irrigation water to give an EC_e of 1.4 (control), 4.7 (medium) and 7.4 dS m^–1 (high salt stress). Plants were grown in a sterilized, low P (silty clay) soil-sand mix. Mycorrhizal colonization was higher in the control than in saline soil conditions. Shoot and root dry matter yields and leaf area were higher in mycorrhizal than in nonmycorrhizal plants. Total accumulation of P, Zn, Cu, and Fe was higher in mycorrhizal than in nonmycorrhizal plants under both control and medium salt stress conditions. Shoot Na concentrations were lower in mycorrhizal than in nonmycorrhizal plants grown under saline soil conditions. The improved growth and nutrient acquisition in tomato demonstrate the potential of AMF colonization for protecting plants against salt stress in arid and semiarid areas. Accepted: 21 February 2000     

On the dependence of salt tolerance of beans (Phaseolus vulgaris L.) on soil water matric potentials

Summary Bean plants (Kora cv) were grown in potted soil artificially salinized by adding NaCl and CaCl₂ to the irrigation water to obtain an electrical conductivity of the soil saturation extract (EC_e) thirty days after emergence of 0.1, 0.3, 0.5 and 0.7 S/m at 25°C and a sodium adsorption ratio (SAR) of 4 (mmol/l)². Thereafter, plants were irrigated when soil water matric potential (_M) was in the range of –20 to –30 kPa (wet treatment) and when _M was in the range of –40 to –60 kPa (dry treatment).Transpiration rates (Tr) and leaf extension rates (LER) per plant or per unit of leaf area were decreased by increasing soil salinity and by decreasing soil moisture. However, a given decrement of _M produced a considerable larger decrement in Tr of LER than an equivalent decrement of soil water osmotic potential (₀). Absolute yields of green pods under wet treatments were from twice to one and a half time as large under the wet than under the dry treatment at equivalent values of ₀. Relative yields were reduced by 25% when EC_e were about 0.5 S/m and 0.7 S/m in the dry and wet treatment respectively. Salt tolerance data of crops may not have a quantitative interest when soil irrigation regimes under which they were obtained are not specified.     

Effect of salinity and inoculation on growth,nitrogen fixation and nutrient uptake ofVigna radiata (L.) Wilczek

This study reports the effect of salinity and inoculation on growth, ion uptake and nitrogen fixation byVigna radiata. A soil EC_e level of 7.5 dS m⁻¹ was quite detrimental causing about 60% decline in dry matter and grain yield of mungbean plants whereas a soil EC_e level of 10.0 dS m⁻¹ was almost toxic. In contrast most of the studied strains of Rhizobium were salt tolerant. Nevertheless, nodulation, nitrogen fixation and total nitrogen concentration in the plant was drastically affected at high salt concentration. A noticeable decline in acetylene reduction activity occurred when salinity level increased to 7.5 dS m⁻¹.     

Copper uptake kinetics in hydroponically-grown durum wheat (Triticum turgidum durum L.) as compared with soil’s ability to supply copper

This paper focuses on the causes of zonation on agricultural land affected by secondary salinity between two halophytic grasses, puccinellia (Puccinellia ciliata Bor. cv. Menemen) and tall wheatgrass (Thinopyrum ponticum (Podp.) Z.-W. Liu & R.R.-C. Wang cv. Tyrrell). We hypothesized that the differences in zonation of puccinellia and tall wheatgrass were caused primarily by differences in the tolerance of these two species to waterlogging under saline conditions. This hypothesis was tested by conducting experiments in the field and in the glasshouse in irrigated sand cultures. At a saltland field site, locations dominated by puccinellia had EC_e values that were consistently higher (11–12 dS/m in early spring, and 5–9 dS/m in late summer) than locations dominated by tall wheatgrass. However locations dominated by puccinellia also had a watertable that was shallower (0.07–0.09 m in the high rainfall season; 0.11–0.13 m in the low rainfall season) than locations dominated by tall wheatgrass. In the glasshouse both species had similar growth responses to salinity under drained conditions, with a 50% decrease in shoot dry mass (DM) at ～300 mM NaCl. However, the combination of salinity (250 mM NaCl) and waterlogging increased puccinellia shoot DM by 150% but decreased shoot DM of tall wheatgrass by 90% (compared with salinity alone). Under saline/waterlogged conditions, puccinellia showed better exclusion of Na⁺ and maintenance of K⁺/Na⁺ in the shoots than tall wheatgrass. We conclude that the zonation of puccinellia and tall wheatgrass is associated with differences in their ion regulation which leads to substantial differences in their growth under saline/waterlogged conditions.     

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.     

Salt tolerance of eggplant

Summary No quantitative information is available regarding the salt tolerance of eggplant (Solanum melongena L.). The present study was conducted over a two-year period in small field plots irrigated by drip, where irrigation frequency was also a variable. The salt tolerance function may be described by the equation Y_r=100–6.9 (EC_e−1.1), where Y_r=relative yield of fruit, EC_e=the mean integrated electrical conductivity at the soil saturation extract, 1.1 dS/m=threshold salinity. Salt was distributed reasonably uniformly within the root zone.     

Rapid Salinity Mapping by Electromagnetic Induction for Determining Riparian Restoration Potential

The feasibility of measuring soil salinity with electromagnetic induction (EM) for determining riparian restoration potential was investigated on a 28-hectare plot at the Bosque del Apache National Wildlife Refuge in central New Mexico. The plot was cleared of exotic Tamarix chinensis (saltcedar), surveyed and gridded into 1370.2 hectare sections. Soil samples and EM measurements were taken at each section. We compared laboratory-determined EC_e values from the soil samples with EC_a values calculated from the EM measurements using a model developed by Rhoades et al. (1990). Direct comparison of EC_e values determined from the two methods yields a low correlation due to sample-size differences but the calculated EC_a was able to accurately predict whether the measured EC_e would lie above or below some threshold value. An assessment of general site suitability for riparian restoration with electromagnetic induction has proven to be a rapid, accurate, and cost-effective alternative to intensive soil sampling.     

咸水非充分灌溉对土壤水盐分布及玉米产量的影响

通过不同矿化度的咸水灌溉春玉米试验,研究了石羊河流域中游咸水充分灌溉和非充分灌溉对土壤水盐分布及玉米产量的影响. 结果表明: 土壤含水量峰值均出现在灌溉期, 充分灌溉变化幅度高于非充分灌溉;土壤含盐量随灌水矿化度的增大而增大, 相同灌水矿化度下,非充分灌溉处理的土壤含盐量均较充分灌溉处理低; 非充分灌溉处理土壤盐分累积层较充分灌溉处理上移; 80～100 cm土壤含水量和含盐量保持稳定,不受灌溉水量和水质的影响.与淡水充分灌溉相比,咸水灌溉下玉米产量降低约15%～22%;9 g·L^-1、6 g·L^-1、3 g·L^-1咸水非充分灌溉下玉米收获后1 m土层平均土壤含盐量分别比充分灌溉降低8.1%、12.4%和18.4%,而产量仅分别降低3.4%、6.8%和3.0%.     

Root water uptake and profile soil water as affected by vertical root distribution

Water uptake by plant roots is a main process controlling water balance in field profiles and vital for agro-ecosystem management. Based on the sap flow measurements for maize plants (Zea mays L.) in a field under natural wet- and dry-soil conditions, we studied the effect of vertical root distribution on root water uptake and the resulted changes of profile soil water. The observations indicate that depth of the most densely rooted soil layer was more important than the maximum rooting depth for increasing the ability of plants to cope with the shortage of water. Occurrence of the most densely rooted layer at or below 30-cm soil depth was very conducive to maintaining plant water supply under the dry-soil conditions. In the soil layers colonized most densely by roots, daytime effective soil water saturation (S _e) always dropped dramatically due to the high-efficient local water depletion. Restriction of the rooting depth markedly increased the difference of S _e between the individual soil layers particularly under the dry-soil conditions due likely to the physical non-equilibrium of water flow between the layers. This study highlights the importance of root distribution and pattern in regulating soil water use and thereby improving endurance of plants to seasonal droughts for sustainable agricultural productivity.     

Growth performance and physiological response in the halophyte Lycium barbarum grown at salt-affected soil

As a traditional Chinese medicinal plant, Lyciumbarbarum is of high economic value and has attracted many considerable interests in recent years. The plant is a perennial halophyte grown under extreme conditions, especially under highly saline soil. A pot experiment was carried out to quantify the responses of L. barbarum plants to soil salinity applied at 100 and 200 mM NaCl. The results demonstrate that 100 mM NaCl soil improves the growth of L. barbarum seedlings. Because the 100 mM NaCl soil enhanced plant height and dry matter by 20% and 30% compared with the nonsalinised soil, it is considered suitable, and the 200 mM NaCl soil showed negative effects, too extreme for the growth of L. barbarum. The leaf cations and betaine content increased significantly under salt stress. The leaf chlorophyll, gas exchange, photochemical efficiency, leaf area and soluble sugar contents showed a significant decrease under 200 mM NaCl stress compared with the nonsalinised and the 100 mM NaCl‐affected soil. The results do not provide a basic mechanism for the observed growth stimulation; however, they suggest that L. barbarum may be an economic species for cultivation in moderately saline areas such as northwest China.     

Effect of saline irrigation on plant water traits,photosynthesis and ionic balance in durum wheat genotypes

In the era of climate change, decreased precipitation and increased evapo-transpiration hampers the yield of several cereal crops along with the soil salinity and poor ground water resource. Wheat being the moderately tolerant crop face many challenges in the arid and semi-arid regions under irrigated agriculture. In view of this, the study was planned to explore the potential of durum wheat genotypes under salinity on the basis of physiological traits. Experiment was designed as RBD in three replications to evaluate 15 wheat genotypes with moderate saline irrigation (EC_iw – 6 dS m⁻¹) and extreme saline irrigation (EC_iw – 10 dS m⁻¹) along with one set of control (Best available water). Different physiological traits such as water potential (ψ_p), osmotic potential (ψ_s), relative water content (RWC), Na⁺ and K⁺ content were recorded in roots as well as shoots at the reproductive stage whereas photosynthetic rate and chlorophyll content were measured in the flag leaves. A significant variability (p < 0.001) was noted among the genotypes under different stress environments and it was observed that durum genotype HI 8728 and HI 8737 showed less reduction in plant water traits (RWC, ψ_p and ψ_s) than the salinity tolerant checks of bread wheat KRL 99 and KRL 3–4. HD 4728 and HI 8708 maintained higher photosynthetic rate as well as higher chlorophyll content under the extreme salinity level of EC_iw – 10 dSm⁻¹. No significant differences were found in root Na⁺ in genotypes KRL 99 (3.17^g), KRL 3–4 (3.34^g) and HI 8737 (3.41^g) while in shoots, lowest accumulation was seen in KRL 99, MACS 3949 and KRL 3–4 at EC_iw – 10 dSm⁻¹. The mean range of K⁺ content was 7.60–9.74% in roots and 4.21–6.61% in shoots under control environment which decreased to 50.77% in roots and 46.05% in shoots under extreme salinity condition of EC_iw – 10 dSm⁻¹. At EC_iw – 10 dSm⁻¹, KRL 99 maintained highest K^+/Na⁺ in both root and shoot followed by KRL 3–4, HI 8737, MACS 3949, HD 4728 in roots and MACS 3949, KRL 3–4, MACS 4020, HD 4758, MACS 3972 and HI 8713 in shoots. The differential response of durum wheat genotypes under salinity particularly for physiological traits, confer their adaptability towards stress environments and exhibit their potential as genetic sources in breeding programs for improving salt stress tolerance.     

Evaluation of Spinacia oleracea (L.) for phytodesalination and augmented production of bioactive metabolite, 20-hydroxyecdysone

In this study, adaptive features of Spinacia oleracea to different levels of salinity, its use in desalination and production of 20-Hydroxyecdysone were studied. Plants showed survival up to EC 12 dS/m with reduced growth as compared with control. Net photosynthesis rate, transpiration, stomatal conductance, and water use efficiency of salt treated plants declines with increasing salinity stress. Higher antioxidant enzyme activities and compatible solutes accumulation were observed in salt treated plants as function of osmotic adjustment. Significant Na⁺ sequestration and Na/K ratio were noted with increase in salt stress in comparison to the control. Since the plant accumulates a bioactive, secondary metabolite 20-Hydroxyecdysone (20E), we observed significant 20E content in plants grown at EC 4–12 dS/m in comparison to control. Furthermore, a preliminary field experiment, showed significant reduction in the soil electrical conductivity by 1.8 ds/m after 90 days of plant growth with Na⁺ sequestration in plant biomass. Subsequent to this growth period, the phytodesalinized soil supported the significant growth of a glycophyte (rice). Our results suggest that S. oleracea can adapt to saline conditions with antioxidant defense and osmotic adjustment. The plant can be used as a potential candidate for desalination and also for enhanced production of 20-Hydroxyecdysone.     

Effect of soil salinity on plant distribution and production at Loburu delta,Lake Bogoria National Reserve,Kenya

A study was carried out at Loburu delta, Lake Bogoria National Reserve, Kenya, on the effect of different levels of soil salinity and moisture on plant species distribution, production, reproductive strategy and litter decomposition. The soils are coarse and vary significantly in levels of salinity and moisture. The highest salinity was greater than 3.0 S/m, ECe. Soil moisture was significantly higher in the more saline than non‐saline or low salinity soils because of ground seepage. Sixteen plant species were collected but only Sporobolus spicatus and Cyperus laevigatus were determined to be true halophytes. Biomass and above‐ground production were significantly higher in the high and medium saline soils than the non‐saline or hyper‐saline soils (>3.0 S/m, Ece). Precipitation promoted various aspects of production in both halophytes at various levels of salinity. Soil salinity did not influence biomass allocation to reproductive structures but precipitation enhanced allocation to stolons in Sporobolus spicatus. The dead plant mass was significantly higher than biomass at all salinities, which indicated low grazing pressure at the site. Litter decomposition was only marginally reduced by high soil salinity. It was concluded that low moisture limits biomass and production on the non‐saline soils and salinity is responsible for low production in the hyper‐saline soils.     

基于盐分梯度的黑河中游湿地植物多样性及其与土壤因子的关系

湿地植物多样性的研究对维持湿地生态系统完整性和稳定性有着重要意义。以黑河中游湿地为研究对象,基于野外采样数据和不同盐分梯度植物群落多样性指数,重点分析不同盐分梯度植物多样性变化及其与土壤因子关系。结果表明:黑河中游湿地植物组成比较丰富,共出现植物30科71属102种;随土壤盐分梯度增加,植物群落组成发生显著变化,Margalef丰富度指数(R)和Shannon-Weiner多样性指数(H)均减小,说明研究区植物多样性随盐分增加而减少;不同盐分梯度影响植物多样性的土壤因子存在差异,低盐梯度是pH、速效钾和全氮,中盐梯度是pH、速效磷和速效钾,高盐梯度是有机质、全磷、速效钾和速效氮。该研究结果对于认识不同盐分梯度下影响植物多样性的主要土壤因子具有重要意义,同时对黑河中游湿地植物多样性的有效管理和维持具有一定的参考价值。