Effect of different levels of water salinity on the decomposition of organic manures in a brackish water fish pond soil

Effects of different water salinity levels on the decomposition of the two organic manures cowdung and poultry manure were studied under laboratory condition. Application of the manures increased the free CO₂ content and decreased D.O. levels of water. pH values of soil and water declined slightly on addition of the manures. The amount of nitrogen, released from the organic manures to water and soil phases, increased gradually with the period of incubation but decreased with increase in water salinity levels. NH₄ ⁺ was found to occur in comparatively higher amount than NO₃ ^–, due to prevailing anaerobic environmental conditions. The amount of added organic carbon remaining in the soil decreased gradually as the decomposition proceeded, but recorded slightly higher values with increase in water salinity levels.The results showed that the rates of decomposition of added organic manures were comparatively lower under higher water salinity levels and hence indicated that use of well decomposed manures might be more suitable for use under such water salinities in brackish water fish ponds.This work formed a part of a thesis submitted for the Degree of Doctor of Philosophy to Bidhan Chandra Agricultural University, West Bengal in 1978This work formed a part of a thesis submitted for the Degree of Doctor of Philosophy to Bidhan Chandra Agricultural University, West Bengal in 1978     

Effects of deforestation and cultivation on soil CEC and contents of exchangeable bases: A case study in Simlipal National Park,India

Deforestation in the tropics seems to be a serious problem probably because of the reduction in soil CEC and the consequent losses of nutrients from the soils. Here, changes in these parameters as influenced by deforestation as well as vegetative cover were studied; statistical methods were applied to interpret the results. Cultivation causes a significant reduction in CEC, total content of the exchangeable bases and exchangeable Ca2+ and Mg2+ levels compared to the adjoining unmanaged forest land. Levels of exchangeable K⁺ and Na⁺, however, do not change significantly. Evergreen forest soils have the highest levels of CEC, total exchangeable bases, exchangeable Ca²⁺ and K⁺. Deciduous forest, grassland and cultivated soils have statistically similar contents of exchangeable Ca²⁺, Mg²⁺, K⁺ and Na⁺. Exchangeable Mg²⁺, however, is not affected by vegetative cover. Soil CEC shows fairly good correlation with the organic carbon content only in evergreen forest soils. In others, organic carbon apparently does not influence CEC significantly. All soils show excellent correlation between their CEC and total exchangeable bases. It is concluded that for regeneration of weathered tropical soils, an evergreen cover provides the most effective means; deciduous vegetation or grass cover do not seem promising.     

Ion metabolism in a halophilic blue-green alga,Aphanothece halophytica

The intracellular ion content of the halophilic blue-green alga, Aphanothece halophytica was studied as a function of age, external sodium and external potassium concentration. Intracellular Na⁺ was found to be about 0.38 millimoles/g dry mass. Intracellular K⁺ concentrations were as high as 1 M and varied directly with external salinity. Intracellular Ca⁺⁺ and Mg⁺⁺ were in the range previously reported for fresh water blue-green algae despite their extremely high extracellular concentrations. Average cell size is consistent at room temperature with two exceptions. When the outside K⁺ is lower than 6.5 mM the cells tend to be smaller with less intracellular K⁺ and high Ca⁺⁺. In stationary phase cultures the cells are larger with high intracellular Mg⁺⁺ and low K⁺.     

Early changes of 'leak flux' and the cation content of lymphocytes by concanavalin A.

The leak fluxes of Na⁺, K⁺, Mg⁺⁺ and Ca⁺⁺ in mouse thymocytes are increased by Concavaline A (Con A), within minutes after mitogen addition. The intracellular Mg⁺⁺ and K⁺ concentrations were decreased and the Na⁺ and Ca⁺⁺ contents were increased by Con A in mouse thymocytes and spleen cells.     

Inorganic transformation of applied phosphorus in brackishwater fish pond soil under different water salinity levels

Transformation of applied phosphorus in a brackishwater fish pond soil was studied under different water salinity levels, as occurring in such ponds, in presence and in absence of added organic matter. Added phosphorus was found to disappear rapidly from the water phase with some variations under different water salinities. The amount of added phosphorus in saloid-bound form increased with increase in water salinity but the same in Bray's (No. 2) extractable form showed a reverse trend. Applied phosphorus was transformed mostly into insoluble calcium phosphate form which increased with increase in water salinity. Transformation was intermediate into iron phosphate and the least into aluminium phosphate form. Application of organic matter reduced the fixation of added phosphorus into the iron phosphate form during the initial period of study and thus increased availability of phosphorus both in water as well as soil phases.This work formed a part of a thesis submitted for the Degree of Doctor of Philosophy to Bidhan Chandra Agricultural University, West Bengal in 1978This work formed a part of a thesis submitted for the Degree of Doctor of Philosophy to Bidhan Chandra Agricultural University, West Bengal in 1978     

On the selective adsorption of cations in the cell wall of the green algaValonia utricularis

The selective adsorption of the cations Na⁺, K⁺, Mg⁺⁺ and Ca⁺⁺ by the cell wall of the Mediterranean algaValonia utricularis (Siphonocladales, Chlorophyceae) from sea water of 40 %. S was investigated by extraction of cell-wall preparations, eluted before in 1.1 mol methanol (adjusted to pH 8) with 0.1 n formic acid in a Soxhlet apparatus. Na⁺ and K⁺ were determined by flame photometry, Mg⁺⁺ and Ca⁺⁺ by complexometric titration with EDTA. From calculation of the dry weight:fresh weight ratios and the chloride determinations in the eluates, the Donnan free-space fraction of the total cell-wall volume was calculated to about 35 %, and the analytical results of the cation concentrations in the extracts expressed asVal cm^–3 DFS. This calculation is based on the assumption that the acidic groups of the noncellulosic matrix material, carrying negative charges by dissociation at the reaction of sea water (ph about 8) are responsible for the adsorption of cations by exhibition of a Donnan effect. The results obtained show clearly that besides the divalent cations Mg⁺⁺ and Ca⁺⁺, which according to the physico-chemical laws of the Donnan distribution must be relatively accumulated to the second power of the monovalent ones, potassium is also enriched by selective adsorption, and the K⁺:Na⁺ ratio increased significantly compared with that in sea water. This seems to indicate that the strength of attraction between the cations and the negative sites is dependent on the radii of the ions and the state of hydration and/or polarisation of the ions and binding sites.     

In-vitro-studies on the influence of cations, neurotransmitters and tubocurarine on calcium-ganglioside-interactions.

The influence of K⁺, Na⁺, Mg⁺⁺, Li⁺, a serotonin, acetylcholine and tubocurarine on calcium-ganglioside-interactions was studied by way of equilibrium dialysis using ⁴⁵Ca as tracer. Experiments were carried out at 22 °C and 4 °C, respectively. The concentrations of the substances were in the range of physiologically relevant conditions. Cations caused a release of Ca⁺⁺ from calcium-ganglioside-complexes in the sequence of their molar efficiency: Mg⁺⁺ ≈ Li⁺ > K⁺ ≈ Na⁺. Tubocurarine, serotonin and acetylcholine also affected calcium-ganglioside-interactions. Ca⁺⁺ was displaced from ganglioside most effectively by tubocurarine, followed by serotonin, whereas acetylcholine competed considerably more weakly.     

Response of sugarcane to different types of salt stress

Summary Due to climatic conditions and prevailing water regime the yield and sucrose recovery in sugarcane are high in South Western India. However, excessive irrigation, poor drainage and luxuriant use of fertilizers have resulted in conversion of large fertile areas into saline lands. The salinity is due to the excess of Na⁺, Ca⁺⁺, Mg⁺⁺, SO₄ ^– and Cl^– ions. Individual salts of NaCl, Na₂SO₄, MgCl₂ and MgSO₄ were employed in culture experiments to study salt stress effect on sugarcane variety Co 740. It was observed that sulphate salinity was more toxic to sugarcane than the chloride one. Sulphate salts caused more inhibition of growth, chlorophyll synthesis, PEPCase activity, decreased the uptake of K⁺ and Ca⁺⁺ ions but stimulated nitrate reductase. The stress did not result in proline accumulation in the sugarcane cultivar Co 740. The degree of toxicity of different ions in decreasing order in sugarcane cultivar Co 740 is SO₄ ^–>Na⁺>Cl^–>Mg⁺⁺.     

Muscle: A Three Phase System : The partition of divalent ions across the membrane

The partition of sulfate, Ca⁺⁺, and Mg⁺⁺ across the membrane of the sartorius muscle has been studied, and the effect of various concentrations of these ions in the Ringer solution on the cellular level of Na⁺, K⁺, and Cl^- has been determined. The level of the three divalent ions in toad plasma and muscle in vivo has been assayed. Muscle was found to contain an almost undetectable amount of inorganic sulfate. Increases in the external level of these ions brought about increases in intracellular content, calculated from the found extracellular space as determined with radioiodinated serum albumin or inulin. Less of the cell water is available to sulfate than to Cl^-, and the Mg⁺⁺ space is less than the Na⁺ space. An amount of muscle water similar to that found for Li⁺ and I^- appears to be available to these divalent ions. Sulfate efflux from the cell was extremely rapid, and it was not found possible to differentiate kinetically between intra- and extracellular material. These results are consistent with the theory of a three phase system, assuming the muscle to consist of an extracellular phase and two intracellular phases. Mg⁺⁺ and Ca⁺⁺ are adsorbed onto the ordered phase, and increments in cellular content found on raising the external level are assumed to occur in the free intracellular phase.     

Conformational changes of membrane-bound (Na+−K+)-ATPase as revealed by antibody inhibition

Summary As different structural states of the (Na⁺–K⁺)-ATPase (EC 3.6.1.3) may lead to a changed reactivity to antibodies, the influence of Na⁺, K⁺, Mg⁺⁺, P_i and ATP on the reaction between highly purified (Na⁺–K⁺)-ATPase and antibodies directed against the membrane-bound enzyme was measured. The antigen antibody reaction was registered by measuring the antibody inhibition of (Na⁺–K⁺)-ATPase activity.In themembrane-bound but not in thesolubilized enzyme four different degrees of antibody inhibition were obtained at equilibrium of the antigen antibody reaction if different combinations of Na⁺, K⁺, Mg⁺⁺ and ATP were present during the incubation with the antibodies. Corresponding to the different degrees of inhibition, different rates of enzyme inhibition were measured. (a) The smallest degree of enzyme inhibition was obtained when (i) only Mg⁺⁺, (ii) Mg⁺⁺ and Na⁺ or (iii) Mg⁺⁺ and K⁺ were present during the antigen antibody reaction. (b) The enzyme activity was inhibited more strongly if Na⁺, Mg⁺⁺ and ATP were present together. (c) It was inhibited even more if only (i) Na⁺, (ii) K⁺, (iii) ATP or both (iv) ATP and Na⁺, (v) ATP and K⁺, (vi) ATP and Mg⁺⁺, or if (vii) no ATP and activating ions were present. (d) The highest degree of antibody inhibition was obtained if Mg⁺⁺, ATP and K⁺ were present together.In the presence of Mg⁺⁺ plus ADP and in the presence of Mg⁺⁺ plus the ATP analog adenylyl (--methylene) diphosphonate, Na⁺ and K⁺ did not influence the degree of antibody inhibition as they did in the presence of Mg⁺⁺ plus ATP. It was further found that the degree of antibody inhibition in the presence of Mg⁺⁺, ATP and K⁺ was affected by the sequence in which K⁺ and ATP were added to the enzyme prior to the addition of the antibodies.It is suggested that by antibody inhibition different conformations of the (Na⁺–K⁺)-ATPase could be detected. These conformations may possibly not occur in the solubilized enzyme and therefore do not seem to be necessarily linked to the intermediary steps of the ATP hydrolysis of the enzyme. The structural changes which are induced by Na⁺ and K⁺ in the presence of Mg⁺⁺ plus ATP are proposed to occur during the Na⁺–K⁺ transport.     

Myocardial electrolytes in hypobaric hypoxia

Male, white rats (Holtzmann) were exposed to 7,200 m in a barometric chamber for six hours a day for three weeks. Control rats were kept at a sea level altitude of 200 m in Peoria, Illinois. At the end of the exposure period the rats were guillotined and their hearts removed. Approximately equal size strips were cut out of the right ventricles (RV), septa (S) and left ventricles (LV) and weighed on a Mettler balance. All heart pieces were dried overnight in a 40°C oven and reweighed following cooling. They were digested in concentrated nitric acid, diluted with distilled water; and sodium, potassium, calcium and magnesium were determined by atomic absorption spectrophotometry. RV and S muscle from the high altitude rats (HA) had a significantly higher water content. RV muscle from HA rats contained significantly more Na⁺, K⁺ and Ca⁺⁺ and less Mg⁺⁺ than sea level controls (SL). LV muscle from HA animals contained significantly less Na⁺ than SL controls. Within the HA hearts, the RV contained sïgnificantly more Na⁺, K⁺ and Ca⁺⁺ and significantly less Mg⁺⁺ than the S or LV. Evidence indicates that chronic high altitude exposure results in significant alterations in electrolyte distribution throughout the heart.Presented at the Seventh International Biometeorological Congress, 17–23 August 1975, College Park, Maryland, U.S.A.     

Water and ion balance in hydrating oocytes of the grey mullet, Mugil cephalus (L.), during hormone-induced final maturation

Sequential changes in water content and inorganic ion concentrations occurring in intra-ovarian oocytes of the grey mullet, Mugil cephalus L., during hormone-induced final maturation are described. Post-vitellogenic oocytes have a water content of 59.4%. During final maturation, oocyte water increases rapidly to a maximum of 84.8% at oviposition. Hydration is accompanied by a relatively small increase in dry matter due to the concurrent uptake of inorganic ions and an apparent uptake of organic matter. Net uptake of Ca²⁺ during hydration is negligible. Net uptake of Mg^{2 +} and Na⁺ occurs in less than equimolar proportions. Net uptake of K⁺ and Cl^? occurs in greater than equimolar proportions prior to ovulation, returning to equimolarity at oviposition. Hence, hydration results in a dilution of intracellular Ca²⁺, Mg²⁺ and Na⁺ to minimum concentrations at oviposition. In contrast, K⁺ and Cl^? concentrations are slightly elevated prior to ovulation, returning to initial levels at oviposition. A 1:1 stoichiometric relationship in net uptake of K ⁺ andCl^? is evident. Intracellular osmotic pressure in post-vitellogenic oocytes is 203.4 ± 18.0 mOsmolkg^?1. Osmotic pressure rises to a peak of 421.3+ 17.3 mOsmol kg^?1 prior to ovulation, then declines to 313.3 ± 15.0 mOsmol kg^?1 at oviposition. This rise in osmotic pressure prior to ovulation cannot be accounted for solely on the basis of inorganic ion uptake and must be attributed to changes in intracellular concentrations of organic solutes as well. An apparent increase in non-ash dry matter during hydration suggests that a net uptake of organic solute is involved. A relatively small organic molecule with high osmotic activity (e.g., amino acids) is implicated.     

Impact of grazing around a watering point on soil status of a semi-arid rangeland in Ethiopia

The influence of long‐term livestock grazing on the soil status of a semi‐arid rangeland was studied along a grazing gradient from a watering point in southern Afar Region of Ethiopia for two seasons. The soil samples were analysed for organic carbon (OC), total nitrogen (N), available phosphorus (P), exchangeable cations (Ca²⁺, Mg²⁺, K⁺ and Na⁺), acidity (pH), cation exchange capacity, and particle size distribution (clay, silt and sand). No significant differences (P > 0.05) were observed for particle size distribution, OC, N, P and K contents along the grazing gradient further than 1500 m from the watering point. Ca²⁺ and Mg²⁺ were found to be dominant cations particularly in the severely degraded area contributing about 74% to the exchangeable cations. The study has also recognized high concentrations of Na⁺ and more than 11% exchangeable sodium percentage. Total exchangeable bases significantly declined (P < 0.05) along the grazing gradient and were indicative of the exchange complex of the soil being saturated with Ca²⁺ and Mg²⁺ ions. Thus this study concluded that there are soil differences in the grazing gradient caused by impact of grazing, particularly in the severely degraded area.     

Salt Tolerance in Aquatic Macrophytes: Ionic Relation and Interaction

Effects of seawater salinity (SWS) and pure NaCl on the intracellular contents of Na⁺, K⁺, Mg²⁺, Ca²⁺, chlorophylls (Chl) and carotenoids (Car) were studied in three submerged aquatic macrophytes, Hydrilla verticillata, Najas indica and Najas gramenia, which differed in their tolerance to salinity. NaCl resulted in significant increase in Chl/Car ratio in the salt-sensitive H. verticillata and moderately salt-tolerant N. indica, but not in the salt-tolerant N. gramenia. SWS treatment did not result in any significant change in the ratio. The intracellular content of Na⁺ increased significantly in all the test plants upon exposure to both NaCl and SWS. The content of K⁺ decreased significantly in these plants upon salinity treatment, except in N. gramenia. The contents of Ca²⁺ and Mg²⁺ decreased significantly upon NaCl treatment and remained unchanged or increased upon SWS treatment. No relationship between salt tolerance and K⁺/Na⁺ ratio was observed. The maintenance of a minimal level of K⁺ was observed to be the most probable requirement of salt tolerance in aquatic macrophytes.     

Role of external calcium in sodium and chloride transport in the gills of seawater-adaptedMugil capito

Summary When the mulletMugil capito is transferred to medium lacking Ca⁺⁺ (either Ca⁺⁺-free seawater or distilled water) the passive permeability of the gill to Na⁺ and Cl^– is increased and the activating effect of external K⁺ on the Na⁺ and Cl^– effluxes in hyposaline media is inhibited. The permeability of the gill increases progressively in proportion to the time of Ca⁺⁺ deprivation; it declines when Ca⁺⁺ is added again to the external medium. The active mechanisms for ion excretion are not reversible. At external Ca⁺⁺ concentrations from 0.1 to 10 mM the Na⁺ permeability is constant but the activation of Na⁺ efflux by K⁺ shows a maximum at a Ca⁺⁺ concentration of about 1 mM. For activation of Cl^– efflux external bicarbonate must be present, in addition to Ca⁺⁺, suggesting the existence of a Cl^–/HCO ₃ ^– exchange. The mechanism by which Ca⁺⁺ controls the passive branchial permeability is thus probably different from that involved in K⁺ activation of ion excretion. The Ca⁺⁺ effect on the K⁺ sensitive ionic excretory mechanisms seems to be related to intracellular Ca⁺⁺ movements. Thus, on the one hand, substances such as Ruthenium Red and La⁺⁺⁺ which both inhibit Ca⁺⁺ exchange, in media containing Ca⁺⁺ and HCO ₃ ^– also inhibit K⁺ activation of Na⁺ and Cl^– effluxes; on the other hand, the ionophore A 23187, a stimulator of Ca⁺⁺ exchange, when added to these media, activates the Na⁺ and Cl^– effluxes; its maximal effect on the Na⁺ flux occurs at 2 mM Ca⁺⁺.Abbreviations ASW-Ca artificial seawater minus calcium - DW deionised water - DWCa deionised water with 1 mM Ca⁺⁺ added - DWCaHCO ₃ DW with calcium plus bicarbonate - DWHCO ₃ DW with 1 mM sodium bicarbonate added - FW freshwater (tap water) - FWK freshwater with K⁺ added - P. D. potential difference - SW seawater The experiments reported in this paper were done with Jean Maetz who tragically died in August 1977. It is the last report about several years of friendly collaboration     

Prolactin regulation in the coho salmon,Oncorhynchus kisutch

Summary Parr and smolt sea water acclimated coho salmon,Oncorhynchus kisutch were subjected to gradual and direct transfers to fresh water. Plasma osmotic pressure, Na⁺, K⁺, Ca⁺⁺ and Mg⁺⁺ were similar in freshwater (FW) fish and seawater (SW) transferred controls for the 24 h following transfer. In spite of the similarity in osmotic pressure and ion levels, plasma cortisol concentrations were significantly increased immediately following salinity change while both pituitary and plasma prolactin decreased indicating enhanced secretion by the pituitary and clearance from the blood. In vitro experiments showed greater incorporation of tritiated leucine into prolactin (PRL) cells immediately after transfer to FW while prolactin injections into intact fish lowered activity in rostral pars distalis (RPD) cells as measured by the same technique, providing evidence of hormonal feedback. These experiments show that the increased synthesis and release of PRL that occurs in coho following movement into FW is not obviously correlated with plasma osmotic pressure, Na⁺ or Ca⁺⁺ concentrations as has been observed in other species of teleosts.Abbreviations FW freshwater - SW seawater - PRL prolactin - RPD rostral pars distalis     

Ionic regulation of the unicellular green algaDunaliella tertiolecta: Response to hypertonic shock

Summary The evolution of the volume, the Na⁺ and K⁺ contents and the glycerol and ATP contents were investigated after subjectingDunaliella tertiolecta cells to hypertonic shocks. It was found that the variations in the glycerol and the ion contents superimpose as the cell regulates its volume. Hypertonic shock induces a rapid increase (some minutes) in the Na⁺ influx and Na⁺ content followed by a decrease until a new steady value is reached after 30 min of cell transfer. The regulatory mechanism extruding Na⁺ out of the cells was dependent on the presence of K^– or Rb^– ions in the external medium. A transient pumping of K⁺ ions was found after subjecting the cells to a hypertonic shock. This increase in K⁺ content resulted from the transient increase in the K⁺ influxes. The K⁺ pumping mechanism was blocked by the absence of Ca⁺⁺ and Mg⁺⁺ ions in the external medium and was inhibited by DCCD, FCCP and DCMU, whereas ouabain, cyanide and PCMBS were ineffective. The increase in K⁺ content was observed if the hypertonic shock was induced by the addition of NaCl, glycerol or choline chloride. These results are interpreted on the basis of two distinct mechanisms: a Na^–/K^– exchange pump and a Na⁺ independent K⁺ pump. These ionic transfer mechanisms would participate in the osmoregulation ofDunaliella cells and would be of importance, particularly during the onset of the osmotic shock when glycerol synthesis is incomplete.     

Effect of NaCl,water stress or both on gas exchange and growth of wheat

Responses of wheat (Triticum aestivum L.) to various concentrations of NaCl and levels of drought were followed. With the rise of NaCl or drought, or NaCl and drought together, growth was retarded. The water content of shoots and roots was mostly unchanged. The chlorophyll and carotenoid contents were increased in plants subjected to salinity or drought or both. Only high salinity level induced a considerable decrease in net photosynthetic rate (P_N) and dark respiration rate (R_D). P_N and R_D were decreased with the decrease of soil moisture content. The content of Na⁺ in the shoots and roots of wheat plants increased with increasing salinity or decreasing soil moisture content or both treatments. Considerable variations in the content of K⁺, Ca²⁺ or Mg²⁺ were induced by the NaCl, drought or both treatments.     

Further Studies on the Roles of Sodium and Potassium in the Generation of the Electro-Olfactogram : Effects of mono-, di-, and trivalent cations

In the negative EOG-generating process a cation which can substitute for Na⁺ was sought among the monovalent ions, Li⁺, Rb⁺, Cs⁺, NH₄⁺, and TEA⁺, the divalent ions, Mg⁺⁺, Ca⁺⁺, Sr⁺⁺, Ba⁺⁺, Zn⁺⁺, Cd⁺⁺, Mn⁺⁺, Co⁺⁺, and Ni⁺⁺, and the trivalent ions, Al⁺⁺⁺ and Fe⁺⁺⁺. In Ringer solutions in which Na⁺ was replaced by one of these cations the negative EOG's decreased in amplitude and could not maintain the original amplitudes. In K⁺-Ringer solution in which Na⁺ was replaced by K⁺, the negative EOG's reversed their polarity. Recovery of these reversed potentials was examined in modified Ringer solutions in which Na⁺ was replaced by one of the above cations. Complete recovery was found only in the normal Ringer solution. Thus, it was clarified that Na⁺ plays an irreplaceable role in the generation of the negative EOG's. The sieve hypothesis which was valid for the positive EOG-generating membrane or IPSP was not found applicable in any form to the negative EOG-generating membrane. The reversal of the negative EOG's found in K⁺- , Rb⁺- , and Ba⁺⁺-Ringer solutions was attributed to the exit of the internal K⁺. It is, however, not known whether or not Cl^- permeability increases in these Na⁺-free solutions and contributes to the generation of the reversed EOG's.     

Effect of the anthraquinones emodin and physcion on availability of selected soil inorganic ions

The effects of emodin and physcion, two anthraquinones involved in Polygonum sachalinense allelopathy, were studied in soils amended with 5, 10 and 15 mg 100 g^-1 soil of each compound, and with their mixtures. Recovery of each compound and its effects on availability of soil Mn⁺⁺, Na⁺, K⁺, Mg⁺⁺, Ca⁺⁺ and PO₄^3- were monitored. Total phenolic content of each soil was determined to study the role of degraded phenolics. Soil amended with 5 mg of emodin and physcion gave maximum recovery of the two anthraquinones. Soil amended with different amounts of two anthraquinones and their mixture had significant lower values for pH compared to control. In general, both anthraquinones affect availability of soil inorganic ions. Compared to unamended control soil, a significant decrease in Mn⁺⁺ availability, and an increase in Na⁺ and K⁺ availability when emodin and physcion were added to the soil was observed. A correlation among soil inorganic ions, relative recovery of two compounds, and total phenolic content of amended soils was observed. Results indicate that emodin and physcion influence the availability of soil inorganic ions. The significance of the effect of allelopathic compounds on soil inorganic ions is discussed.