溶质类型与矿化度对半干旱盐渍化地区果园土壤水分有效性的影响

盐渍化土壤水分有效性是制约土地生产能力的关键因素之一。研究不同盐分类型及矿化度的盐溶液对土壤水分有效性的影响, 可为微咸水合理灌溉以及促进土壤生产潜力的发挥提供科学依据。本研究采用离心法在室内研究了脱水过程中灌溉水的溶质类型(NaCl和Na₂SO₄)与矿化度(0、1 g·L^-1、3 g·L^-1、5 g·L^-1、10 g·L^-1)对半干旱盐渍化地区果园土壤水分有效性的影响。结果表明: 不同矿化度的NaCl和Na2SO4处理均可使田间持水量、暂时萎蔫系数、永久萎蔫系数、迟效水和无效水较对照有所降低。不同矿化度的NaCl处理以及1 g·L^-1的Na₂SO₄处理土壤全有效水和速效水都较对照增加, 3 g·L^-1、5 g·L^-1和10 g·L^-1的Na₂SO₄处理土壤全有效水和速效水都较对照减小。不同矿化度的NaCl和Na₂SO₄处理均可使土壤通气孔隙和毛管孔隙相对减少, 非活性孔隙增大, 其中矿化度为5 g·L^-1的NaCl和Na₂SO₄处理对其影响最为明显, 通气孔隙分别较对照减小16.8%和14.8%, 毛管孔隙分别较对照减小5.2%和6.5%, 非活性孔隙分别较对照增加15.7%和14.4%。NaCl对于土壤比水容量和毛管断裂的延迟效果比NaSO₄明显。且土壤溶液盐分含量增加, 土壤持水能力下降、供水性能增加而土壤抗旱性降低。     

磷比色测定的某些问题

磷的比色测定在文献中常见的有钼黄和钼蓝法。钼黄生色的原理是在某种浓度的酸溶液中,若有钼酸根、钒酸根和磷酸根存在,能结合成一种深黄色的络合物P₂O₅·R₂O₃·22MoO₃·nH₂O。钼蓝生色的原理是在一定条件下,磷酸和钼酸所结合成的杂多酸(hetropoly acids)H₃[P(Mo₃O₁₀)₄]·nH₂O(磷钼酸)在还原剂的作用下能还原成深蓝色的复杂氧化物(MoO₃+Mo₂O₃)。     

保水型专用肥对制种玉米田土壤蓄水量的影响及最佳施肥量研究

在甘肃省河西内陆灌区的制种玉米田,采用田间试验方法,研究了保水型专用肥对土壤物理性质和蓄水量的影响及制种玉米田最佳施肥量。结果表明,影响玉米产量的因素由大到小依次为:CO(NH₂)₂>(NH₄)₂HPO₄>糠醛渣>保水剂>ZnSO₄·7H₂O;因素间最佳组合为:CO(NH₂)₂600kg/hm²,(NH₄)₂HPO₄350kg/hm²,ZnSO₄·7H₂O 30kg/hm²,保水剂19.98kg/hm²,糠醛渣15 000kg/hm²。保水型专用肥施肥量与玉米制种田容重呈负相关关系,与孔隙度、蓄水量、玉米植物学性质和经济性状呈正相关关系。随着保水型专用肥施用量梯度的增加,玉米穗粒数、穗粒重、百粒重、产量在增加,但边际产量、边际利润表现为递减,保水型专用肥施用量在10.00t/hm²的基础上再增加2.50t/hm²,收益出现负值。经回归统计分析,保水型专用肥施用量与玉米产量可用一元二次方程拟合,经济效益最佳施肥量为9.99t/hm²,玉米的理论产量为6 715.33kg/hm²。     

大豆分离蛋白成膜性研究

该文通过单因素试验和正交试验对大豆分离蛋白的成膜性进行研究。结果表明，大豆分离蛋白浓度、增塑剂(甘油)、还原剂(Na₂SO)、交联剂(谷氨酰胺转胺酶)对膜的性能有较大影响，最佳处理条件为：大豆分离蛋白5.0%、甘油1.5%、Na₂SO₃ 0.1%、TG酶0.2%，大豆分离蛋白浓度对膜性能影响最大，其次是甘油含量，Na₂SO₃和TG酶的浓度对膜性能影响较小。     

用电导热散法研究可变电荷土壤粘粒与离子的相互作用

本工作选用二种可变电荷土壤粘粒(<2μ),分别含有0.35×10^-4-1.3×10^-4mol/L的不同电解质,在不同含水量下,在5—50℃范围内测量其直流电导率的变化。试验结果表明,电导热散法是研究土壤粘粒与离子相互作用的有用手段;电导率-温度曲线上的折点温度是随含水量、电解质种类和土壤类型而不同。在相同含水量下,含有不同电解质的红壤体系的折点温度具有如下的变化顺序:CaCl₂>Na₂SO₄>KCl>Ca(NO₃)₂>NaNO₃;砖红壤体系的折点温度明显高于红壤体系。折点温度的高低是土壤粘粒与离子相互作用强度的反映。     

90℃下老化时结晶磷铁矿的生成条件

溶液中Fe与P反应并不直接生成结晶磷铁矿,中间经过无定形阶段。溶液的pH对Fe-P无定形物质的组成及由无定形Fe-P向结晶磷铁矿转化都有很重要的作用。在90°下老化80天,用加入的Fe(NO₃)₃和NaH₂PO₄浓度及混合后的溶液pH计算得到的﹝Fe³⁺﹞﹝H²PO₄^-﹞值可以较好地判断溶液中是否会有结晶磷铁矿生成。本文的实验条件下,结晶磷铁矿生成的条件是-log{﹝Fe³⁺﹞﹝H₂PO₄^-﹞} ≤ 6.09(加入的P/Fe比 ≥ 1)。     

测定盐土中Cl-的Hg(CNS)2-Fe(NO3)2比色法

Hg(CNS)₂-Fe(NO₃)₃比色法测定盐土中Cl^-快速准确,其变异系数小于5%,回收率98.5%-102.4%,与莫尔法相比,其绝对相差< 0.1g/kg。尤其适宜于批量样品及现代化的仪器分析。其适宜工作条件是:在50ml比色液中加0.75g/L Hg(CNS)₂ 8ml,20g/L Fe(NO₃)₃·9H₂O 10ml。定容10分钟后于460nm下用3cm光径比色。     

用电导频散法研究Cl-、SO42-和H2PO4-阴离子与土壤的相互作用

本文介绍了采用电导频散装置测量分别含有10^-4mol/LHCl、5×10^-5mol/L H₂SO₄和10^-4mol/L H₃PO₄的黄棕壤、棕壤、黑土和砖红壤悬液(20-30g/kg)的电导频散曲线,频散曲线上均呈现频率范围相当宽的坪区,频散曲线的特性分析结果表明,黄棕壤和棕壤在3种酸溶液中的始散频率(0.6-1kHz)低于黑土悬液(16-28kHz),而砖红壤的始散频率最高(25-47kHz;Cl^-、SO₄^2-和H₂PO₄^-离子与4种土壤的相对亲合力(REC_1.5/REC_tp-1)顺序为Cl^- < SO₄^2- < H₂PO₄^-,在不同土壤之间的顺序则随酸溶液而异.     

La(NO3)3 对盐胁迫下黑麦草幼苗生长及抗逆生理特性的影响

为探讨稀土元素镧(La)对牧草盐胁迫伤害的缓解作用, 采用水培法研究了叶面喷施20 mg·L^-1La(NO₃)₃ 对NaCl 胁迫下黑麦草幼苗生长及其抗逆生理特性的影响。结果表明: 盐胁迫显著抑制黑麦草幼苗的生长, 提高叶片电解质渗漏率及丙二醛(MDA)、O₂^- 和H₂O₂ 含量, 其作用随盐浓度的增大而增强。超氧化物歧化酶(SOD)、过氧化氢酶(CAT)、抗坏血酸过氧化物酶(APX)活性和抗坏血酸(AsA)、谷胱甘肽(GSH)、可溶性蛋白质、脯氨酸含量随盐浓度增大呈先升后降趋势, 可溶性糖和Na⁺/K⁺比逐渐增大, 质膜H⁺-ATP 酶活性逐渐降低, 过氧化物酶(POD)活性及POD 同功酶数量表达增强。喷施La(NO₃)₃ 处理可降低盐胁迫下黑麦草幼苗叶片的O₂^- 和H₂O₂ 含量, 提高SOD、CAT、POD、APX 和质膜H⁺-ATP 酶的活性及POD 同功酶的表达, 使AsA、GSH、可溶性蛋白质、可溶性糖和游离脯氨酸含量及幼苗生物量增加, Na⁺/K⁺比降低。表明La(NO₃)₃ 可通过提高抗氧化系统的活性和积累渗透溶质减轻盐胁迫伤害, 从而提高黑麦草的耐盐性。     

Chemical Behavior of Chromium in Soils: Ⅲ. Mechanism of Cr(Ⅵ) Adsorption by Soils

An analysis of Cr (Ⅵ)-sorbed surface of the soils by using a scanning electron microscope and an electron probe microscope has proved that aluminium is the chief element affecting Cr (Ⅵ) adsoption. As the ionic strength of the solution increased, the amounts of Cr (Ⅵ) adsorbed by goethite and soils decreased. Cr (Ⅵ) adsorption was greatly depressed in the presence of SO₄^2-, WO₄^2-, MoO₄^2-, HPO₄^2- and H₂PO^4- which competed for anion adsorption sites. The depressing extent of these anions was found to follow the sequence: HPO₄^2-, H₂PO^4->MoO₄^2->WO₄^2->SO₄^2->>Cl^-, NO^3-. The amounts of Cr (Ⅵ) desorption varied with different extractants.     

Interactions of NaCl and Na2SO4 on soil organic C mineralization after addition of maize straws

NaCl and Na₂SO₄ often dominate salt compositions in saline soils. While either salt alone affects soil organic matter mineralization, their interactions on soil organic matter dynamics are unknown. This study aimed to investigate interactive effects of the two salts on organic C mineralization and microbial biomass C of the saline soils after addition of maize straws. Both NaCl and Na₂SO₄ were applied at 0, 40 and 80 mmol Na kg⁻¹ soil and the incubation was undertaken at soil water content of 15% and 20% (w/w) in dark at 28.5 °C for 70 days. The study found significant interactions of NaCl and Na₂SO₄ on CO₂-C evolution during the early incubation periods—a suppressing effect at days 1-2 but a stimulating effect at days 6-8 and 17-20, and thereafter the salt interactions were influenced by water content. The interactions of water content with NaCl or Na₂SO₄ on CO₂-C evolution were observed through the incubation periods except days 1-2, showing that the salt effects were dependent on water content. Total CO₂ evolution over the 70-day-long incubation decreased with increasing NaCl but increased with increasing Na₂SO₄ compared to the nil-salted treatment. Salt interactions on soil microbial biomass C were observed at days 7, 21, but not at day 49. Microbial biomass C increased at day 7 in the soils treated with either NaCl or Na₂SO₄ but decreased where the two salts were combined. At day 21, microbial biomass C increased with NaCl but decreased with Na₂SO₄ regardless whether the counterpart salt was added. The results suggest that soil organic C mineralization can be affected by the interactions of NaCl and Na₂SO₄, possibly through the salt-induced changes in microbial biomass community structure.     

Effects of salts on dry matter yield and nitrogen and phosphorus contents of rice plants

Abstract

The effects of different kinds and concentrations of salts on dry matter yield and nitrogen (N) and phosphorus (P) contents of rice plants under greenhouse conditions were determined for two silt loam soils, one from southern Ohio (Clermont) and one from Arkansas (Crowley). Yield and N and P contents tended to be enhanced by low salt concentration but to be depressed at higher concentration. The chloride salts (NaCl, CaCl₂) were most detrimental to yield and N and P contents, while the sulfate salts (especially Na₂SO₄,) were beneficial when the electrolyte concentration and P in the soil were not high.

The degree of adverse response to salts in the irrigation water and of favorable response to P fertilizer were reflected in the levels of electrolyte and available P in the soils studied. Total N content of the rice tissue increased much more from N and P additions than did total P content. The NaCl (1.5 mmhos/cm) and NaCl + Na₂SO₄ (3.0 mmhos/cm) salt treatments vere generally least detrimental, and NaCl and NaCl + CaCl₂both at 3.0 mmhos/cm were most detrimental to yield and N and P contents of tissue.

In the non‐lethal response range, salt‐depression of yield and N and P contents of tissue may well be largely or partially overcome by fertilizer application. In this study, the best combination of fertilizer and salt was the highest level of N (268 kg N/ha) and intermediate level of P (67 kg P/ha), in combination with NaCl + Na₂SO₄.     

克拉玛依人工碳汇林区景观地球化学特征与规律

以克拉玛依人工碳汇林区的土壤可溶性盐分离子、地下水矿化度和植被为研究对象, 综合运用描述性统计和相关性分析等方法, 研究其景观地球化学特征, 旨在通过对克拉玛依人工碳汇林区的景观地球化学特征的研究, 为这一地区盐渍化土壤改良和沙漠化防治提供理论依据。结果表明: 克拉玛依人工碳汇林区土壤Cl^-、SO₄^2-、Ca²⁺在0~80 cm范围内变异系数较大, 80~100 cm范围内, 土壤总盐和各离子变异系数相对较小; 盐分表聚现象严重; 该地区盐土类型主要是硫酸盐型, 其中SO₄^2-和Na⁺+K⁺为土壤可溶性盐的主要成分。研究区地下水呈弱碱性, 除HCO₃^-外, 其他离子和矿化度表现出较强的变异性; 地下水的化学类型主要为Cl·SO₄-Na, 矿化度和Cl^-、SO₄^2-、Na⁺+K⁺相关系数较为显著。种植人工碳汇林后, 除土壤HCO₃^-含量有轻微上升外, 其他离子均有所下降, 其中SO₄^2-含量的降低趋势最为明显。俄罗斯杨林分土壤含盐量随种植年限的增长明显降低, 种植后的土壤盐渍化状况有明显改善。     

胀果甘草原生境土壤盐分特征分析

 通过野外调查采样和土样化学测定,分析胀果甘草原生境下土壤盐分的特征。结果表明:研究区土壤盐分普遍较高且表聚作用明显,土壤表层0～10 cm土层盐分均值高达32+.08g/kg,属典型的强度盐渍化土;土壤盐分组成中,含阳离子Ca2+、Na+、Mg2+、K+和阴离子Cl-、SO24、HCO-3,不含CO2-3,土壤盐分的特征因子为Ca2+、C1-、SO2-4、NaCa+,其盐渍类型主要为硫酸盐-氯化物型,重碳酸盐是土壤盐分的次要成分;该生境土壤中在整个垂直剖面上Ca2+的含量丰富,属典型钙质土。     

COMPARATIVE STUDY OF DIFFERENT SALTS (SODIUM CHLORIDE,SODIUM SULFATE,POTASSIUM CHLORIDE,AND POTASSIUM SULFATE) ON GROWTH OF FORAGE SPECIES

Osmotic and specific ion effects are the most frequently mentioned mechanisms by which saline substance reduces plant growth. However, the relative importance of osmotic and specific ion effect on plant growth seems to vary depending on the salt tolerance of the plant under study. Tall wheatgrass (TW), perennial ryegrass (PR), African millet (AM) and Rhodesgrass (Rh) were grown in nutrient solution with sodium chloride (NaCl), sodium sulfate (Na₂SO₄), potassium chloride (KCl), and potassium sulfate (K₂SO₄) salinity up to electrical conductivity (EC) 27 dS m^?1. Growth of all plant species decreased significantly at high level (EC 27 dS m^?1) of NaCl and Na₂SO₄ salts. However, the growth of none of the plant species was affected significantly by KCl and K₂SO₄ at any level. Even leaf and shoot fresh weights were enhanced by K₂SO₄ in all plant species, except AM. Chlorine (Cl) was taken up in similar quantities from KCl and NaCl solutions and the content of the respective cations was similar to each other. Further sensitivity to sulfate and chloride was equal when sodium concentrations in shoots were equal, regardless of the anion composition of the media. The sodium (Na) concentration of the leaves of the plant species increased with increased NaCl and Na₂SO₄ levels in the nutrient solutions. The leaf Na concentration of TW was lower than that of the other plant species. However, the root Na concentration of TW was higher than that of the other plant species. Increased NaCl and Na₂SO₄ concentrations had a marked effect on leaf water potential of all plant species, and the TW showed higher leaf water potential at all levels of salts. Tall wheatgrass adjusted osmotically by accumulating electrolytes from the nutrient solution and by accumulation of glycinebetaine. Sodium was generally found more injurious than Chloride in all the four forage species. Salt tolerance could be ascribed as greater exclusion of Na ion.     

Interactive effects of sodium chloride,sodium sulfate,calcium sulfate,and calcium chloride on snapbean growth,photosynthesis, and ion uptake

Excessive sodium (Na) accumulation in soil, which can be a problem for production agriculture in arid and semiarid regions, may be ameliorated by calcium (Ca). The mechanisms of Ca amelioration of Na stress in plants have received much more attention than has the effect of the anion of the Ca salt. Our objective was to determine the relative effects of the chloride (Cl^‐) and sulfate (SO₄ ^2‐) anions on Ca amelioration of Na stress. We exposed Phaseolus vulgaris L., cv. Contender seedlings growing in 1‐L styrofoam pots under greenhouse conditions to sodum chloride (NaCl) or sodium sulfate (Na₂SO₄) at concentrations of 0, 15, 30, 45, and 60 mmol/L combined with either 15 and 30 mmol/L of calcium sulfate (CaSO₄) or calcium chloride (CaCl₂). Plants in each styrofoam pot were irrigated with 300 mL of salt solution (leaching fraction = 0.25) every fourth day for four weeks. Increasing Na concentration decreased shoot dry weight, number and weight of pods, and number of nodules. The photo‐ synthesis rate was affected by all levels and types of Na salts. Calcium sulfate treatments ameliorated Na‐induced salinity in snapbeans more than did comparable CaCl₂ treatments. The thermodynamic activity of Ca, Na, and Cl was linearly related to the tissue content of each ion.     

Ameliorative Effect of Hydro Gel Substrate on Growth,Inorganic Ions,Proline, and Nitrate Contents of Bean under Salinity Stress

The effect of varying hydrogel (0, 0.5, and 1.0% w/w) supply on some agro-physiological properties, such as dry matter, nutrient contents, chlorophyll contents, proline content, and ionic balance of bean plants in different salt sources and stress due to doses were investigated. Plants were treated with eight salt sources [sodium chloride (NaCl), sodium sulfate (Na₂SO₄), calcium chloride (CaCl₂), calcium sulfate (CaSO₄), potassium chloride (KCl), potassium sulfate (K₂SO₄), magnesium chloride (MgCl₂), magnesium sulfate (MgSO₄)] and four concentrations (0, 30, 60, and 120 mM doses) for 60 days in a growth media. Salt type, doses, and hydrogel (HG) affected the soil electrical conductivity. Soil salinity affected the parameters considered, and changed the nutrient balance of plants. High salt concentration caused substantial reduction in plant growth. Different salt concentrations negatively affected plant dry weight. The highest decrease of plant root dry weight was obtained with NaCl application followed by Na₂SO₄, CaCl₂, CaSO_4, MgCl₂, MgSO₄, KCl, and K₂SO₄, and similarly NaCl, Na₂SO₄, CaCl₂, CaSO_4, KCl, K₂SO₄, MgCl₂, and MgSO₄ in root dry weight. Total chlorophyll and nitrate contents of plants decreased with increasing salt doses, and the lowest value was obtained for NaCl application. Proline contents of plants were increased with increasing salt doses, and the highest value was obtained with the NaCl application. The effects of salt concentrations in nitrogen (N), potassium (K), and phosphorus (P) content of plants were significant. The presence of salt in the growth medium induced an important decrease the macro nutrient of the root and shoot part of plant such as N, P, K, calcium (Ca), and magnesium (Mg) content, but the N and P content of root and shoot part of the plant were increased with increasing of the HG application doses. The highest N and P increases were obtained with the 1.0 HG application for all salt types for both the root and shoots of plants. The HG added to saline soil significantly improved the variables affected by high salinity and also increased plant N and P, reduced soil electricity conductivity, nitrate, proline, and electrolyte leakage of plants, enhanced plant root and shoot dry weight by allowing nutrients and water to release to the plant as needed. The results suggested that HG has great potential for use in alleviating salinity stress on plant growth and growth parameters in saline soils of arid and semi-arid areas. This HG appears to be highly effective for use as a soil conditioner in vegetable growing, to improve crop tolerance and growth in saline conditions. It is intended to confirm the results of these studies by field trials.     

Soils,surficial geology,and geomicrobiology of saline-sodic wetlands,North Platte River Valley,Nebraska, USA

Saline-sodic wetlands along a 200-km stretch of the North Platte River Valley in western Nebraska, USA lie within an important agricultural region, but their processes, salt mineralogy, and geomicrobiology have not previously been investigated. Putative anthropogenic salinization has long been a concern, yet early historical accounts of widespread surface salts in the area have never been applied as comparative standards. Surface salts in the area originate from soil capillarity and surface evaporation. Thenardite (Na₂SO₄) and/or mirabilite (NaSO₄·10 H₂O) dominate, depending on ambient conditions. Bloedite (Na₂Mg[SO₄]₂·4[H₂O]), halite (NaCl), burkeite (Na₆CO₃[SO₄]₂), and calcite (CaCO₃) are minor constituents. Historical accounts indicate that salts accumulated naturally long before Euramerican settlement, apparently as a result of rock–water interaction in nearby volcaniclastic sediments of the Brule Formation.Ephemeral to permanent water-holding basins in the wetlands contain Na⁺-rich waters that vary widely in electrical conductivity (as high as 159 mS/cm) and in ionic composition, but local spring waters are extremely dilute. Basin floors exhibit a unique type of microrelief, which appears to form by the filling of microlows with water and the dispersal of soil material therein by Na⁺, followed by dewatering and collapse of the soil with drying. Illite dominates basin surface soils, but smectite dominates at depth; high soil pH, available K⁺, and frequent wetting–drying cycles in the wetlands suggest that in-situ illitization may have occurred. Soil crusts and vesicular surface horizons are common as are upward increases in electrical conductivity. The activity of sulfate-reducing microbes forms prominent near-surface horizons of sulfate reduction in saturated soils, which retract or disappear entirely during dry episodes.Saline-sodic wetland soils in the study area change on daily to seasonal scales. Cycles of surface salt development, microbial activity, and microrelief genesis are all controlled by regular wetting–drying cycles and the interaction of ponded surface waters and shallow groundwaters. Relatively unique aspects of microbial ecology and surface processes make the soils important as “geomicrobial reactors” wherein important parts of hydrological and geochemical cycles occur.     

Germination and growth response of flax (Linum usitatissimum) to salinity stress by different salt types and concentrations

This investigation was conducted to explore the effects of salt types with different concentrations on germination and growth parameters of flax seeds. The experiment was set out as a factorial experiment based on a completely randomized design with three replications. We used six kinds of salts (NaCl, CaCl₂, CaCO₃, Na₂SO₄, Na₂CO₃ and KCl) with concentrations of 0, 50, 100 and 200 mM. According to the results, the inhibitory effects of the five salt types differed substantially, especially in the case of CaCO₃, Na₂CO₃ and Na₂SO₄. Inhibitory effects of these salts were very strong compared to those of NaCl and CaCl₂. Germination of flax seeds by various salts was in the order of NaCl > CaCl₂ > KCl > Na₂CO₃ > Na₂SO₄ > CaCO₃. The effect of salt concentration was obvious, too. Seeds of flax were able to germinate even in 200 mM NaCl, but they only germinated in distilled water or at very low CaCO₃, Na₂CO₃ and Na₂SO₄ concentrations (50 mM).     

民勤绿洲盐生草生境土壤盐分特征及离子组成

对民勤绿洲盐生草周围不同距离范围内的总体盐分状况、盐分离子组成及离子之间的相关性进行了研究。结果表明,盐生草具有一定的聚盐作用,在其周围形成了一定的"盐岛"效应。在距盐生草0-60 cm范围内,土壤剖面中的土壤盐渍化程度随土层的加深而加重,土壤阴离子主要有Cl^-和SO₄^2-,阳离子主要有Na⁺和Ca²⁺,土壤盐分主要是氯化钠、氯化钙、硫酸钠和硫酸钙,其次是氯化镁和硫酸镁。其中在盐生草周围0-40 cm范围内,垂直剖面0-20 cm土层土壤全盐含量为0.98~1.52 g/kg,属于非盐渍化土壤,20-40 cm土层土壤全盐含量达到了2.25~2.30 g/kg,属于轻度盐渍化土壤,40-60 cm土层土壤全盐含量达到了3.10~3.16 g/kg,属中度盐渍化;在距盐生草60 cm处,垂直剖面0-40 cm土层土壤全盐含量为0.83~1.86 g/kg,属非盐渍化,40-60 cm土层土壤全盐含量达到了2.43 g/kg,属轻度盐渍化。除HCO₃^-外,土壤盐分含量与各盐分离子之间均呈极显著正相关。