Variation in Phosphorus Sorption with Soil Particle Size

Phosphorus (P) is considered a primary cause for surface water eutrophication that leads to anoxia. Understanding the relationships between soil particle size and P sorption helps devise effective best management practices (BMPs) to control P transport by erosion, leaching, and overland flow from agricultural land. Consequently, this study examined the effect of surface soil particle size on the sorption of P in five soil series (four Ultisols and one Entisol) from the Mid-Atlantic region. The sorption of P in each soil was assessed by equilibrating (after shaking for 24?h) 5?g soil containing varied amounts of KH₂PO₄ in 20?mL of 0.01?M KCl solution. Phosphorus in solution was determined by the molybdate blue method of Murphy and Riley. The P adsorption characteristics of these soils were described using the Langmuir isotherm. Results indicated that variability in P sorption was related to particle size and soil type. Soil organic matter content contributed a great deal to P sorption in the Entisol. However, soil clay had influence on the P sorption characteristics of each soil. The maximum P retentive capacities of soils (as determined by Sm from Langmuir equation) and P sorbed at 500?mg P kg^?1 addition showed a linear relationship (r2 = 0.94). Therefore, based on the results obtained, the single point method of Bache and Williams may be appropriate to describe the maximum P sorption capacity of non-sandy soils, as observed in this study.     

Modeling Dicamba Sorption and Transport Through Zoysiagrass Thatch and Soil

The presence of turfgrass thatch complicates the sorption and transport of water soluble pesticides because the surface-applied pesticides must pass through an organic-rich thatch layer prior to entering the soil. The study was conducted (1) to determine the impact of zoysiagrass thatch (Zoy-sia japonica Steud.) on dicamba (3,6-dichloro-2-methoxy benzoic acid) transport through soil columns, and (2) to evaluate the effectiveness of linear equilibrium (LEM), two site nonequilibrium (2SNE) and one site nonequilibrium (1SNE) models to predict dicamba transport through columns containing a surface layer of thatch and columns devoid of thatch. The equilibrium sorption isotherms of ¹⁴C dicamba to homogenized samples of zoysiagrass thatch and a Sassafras loamy sand soil (fine loamy, mixed mesic, Typic Hapludult) were determined. Following the application of bromide to determine transport parameters, 0.56?kg dicamba ha^?1 was surface applied to undisturbed soil columns containing a surface layer of thatch and columns devoid of thatch and leachate samples collected for 12?h under steady-state unsaturated conditions. Zoysiagrass thatch (Kf = 0.82) had a three times greater sorption capacity than the soil (Kf = 0.28) beneath the thatch. Dicamba leaching for columns with thatch layers was ca. 21% less than soil columns devoid of thatch. When dicamba breakthrough curves were fitted to the different forms of the convective dispersive equation, the 2SNE model simulated dicamba transport better than LEM and 1SNE models, indicating the presence of two-site nonequilibrium sorption. Indications are that turfgrass thatch may have significant effects on dicamba leaching that presently used regulatory models based on LEM approach do not adequately consider.     

Predominance of Char Sorption over Substrate Concentration and Soil pH in Influencing Biodegradation of Benzonitrile

Incomplete combustion of field crop residues results in the production of char, a material rich in charcoal-type substances. Consequently, char is an effective adsorbent of organic compounds and when incorporated into soil may adsorb soil-applied pesticides, thereby altering their susceptibility to biodegradation. We investigated the relative importance of char, soil pH and initial substrate concentration in biodegradation of pesticides in soils by measuring the biodegradation of benzonitrile in soil as a function of soil char content (0% and 1% by weight), initial benzonitrile concentration (0.1, 1.06, and 10.2 mg l⁻¹) and soil pH (5.2, 6.9 and 8.5). Preliminary experiments revealed that wheat straw char had a much greater benzonitrile sorption capacity than did soil to which the char was added. The extent of benzonitrile degradation decreased as initial benzonitrile concentration increased in both buffer solution and soil slurry. In contrast, the degradation increased as initial benzonitrile concentration increased in char-amended slurry. In un-amended soil slurry, the benzonitrile degradation was lower at pH 5.2 than at pH 6.9 or 8.5, but in char-amended soil slurry the degradation was not affected by pH, again presumably due to adsorption of benzonitrile by the char. Adsorption by soil char appears to be more important than either initial substrate concentration or soil pH in controlling benzonitrile degradation in char-amended soil slurry. The presence of crop residue-derived chars may alter pesticide degradation patterns normally observed in soils and thus significantly affect their environmental fate.     

Impacts of Soil Organic Matter and Temperature on Sorption of Acetazolamide on Four Soils

Batch sorptions of acetazolamide (AZ) were conducted using four soils from China. Sorption of AZ was found to be impacted by OC, clay content, and soil pH, with higher k_d values for soils with higher clay content. The k_d values of SOM-removed soils are much lower than those of bulk soils. Sorption data were well fitted with a Freundlich model (r² > 0.99). Chelating with the metal ions on the surfaces of soil particles was probably involved. With pH increase, the electrostatic attraction between anionic AZ and positively charged soil surface may increase. The sorption capacity decreased when the temperature increased from 20 to 40°C, and the calculated thermodynamics parameters of ΔG₀, ΔH₀, and ΔS₀ indicated that the sorption was a non-spontaneous, physisorption, and exothermic process. Sorption coefficients (k_d) for the compound in soil were low (ranging from 0.42 to 1.19 L·kg^?1) and indicated that low level sorption of AZ with appreciable risk of ground water contamination.     

Influence of Soil Components on Sorption of Atrazine under Aerobic and Anoxic Conditions

The adsorption of atrazine onto untreated and soils when oxides and hydroxides of Fe, Mn, and organic matter have been reduced was studied under aerobic and anoxic conditions. The Freundlich model appeared to fit the isotherm data better than the Langmuir model, while second-order reaction rates were best fit for atrazine in the aqueous phase. Simple regression analysis indicated that the Fe content of the geosorbents is the most important primary factor controlling the sorption processes of atrazine (r² = 0.947). Similar sorption capacity of atrazine by geosorbents but different isotherm nonlinearity indicated different sorption domains due to structural modifications and hydrophobicity. The sample treated to significantly remove organic carbon exhibited the greatest organic carbon–normalized sorption capacity. There existed apparent sorption–desorption hysteresis for each sorbent–sorbate system with desorption being more significant under anoxic conditions. The study suggests that, in remediation exercise, in situ redox barriers such as Fe²⁺-enriched zones can be created by stimulation of Fe³⁺ through chemical reduction. This study observed that soil predominated by Fe and with low OC content is probably a more effective sorbent for atrazine, implying that atrazine applied to such soils is less likely to leach into groundwater.     

Sorption and Desorption of Napropamide in Sandy Soil Amended with Chicken Dung and Palm Oil Mill Effluent

Beach Ridges Interspersed with Swales (BRIS) is a sandy soil and in Malaysia it is found exclusively in the east coast of Peninsular Malaysia. It is a marginal soil because of its low nutrient and water-holding capacity. However, with proper management and organic matter amendments some areas with BRIS soil are cultivated. Napropamide is a selective herbicide widely used to control weeds in BRIS soil. No previous studies have been reported on the effects of organic matter amendments on napropamide sorption in BRIS soil. This study was conducted to determine sorption and desorption of napropamide in BRIS soil amended with chicken dung (CD) and palm oil mill effluent (POME) at 0, 20, 40, and 80 Mg ha^?1. Potential interaction of dissolved organic carbon (DOC) with napropamide and their competition for sorption sites were also determined. Sorption isotherm data were fitted to the log-transformed Freundlich's equation. Sorption of napropamide was higher in soils amended with CD and POME as compared to non-amended soil. At the same rates of application, sorption was higher in soil amended with CD than POME. The Freundlich's coefficient (K_f) values were 0.22, 3.96, and 41.6 for nonamended soil, soil amended with 80 Mg ha^?1 POME, and soil amended with 80 Mg ha^?1 CD, respectively. Desorption of napropamide showed positive hysteresis and the hysteresis were greater with higher rates of CD and POME. There was no association between napropamide and DOC extracted from BRIS soil amended with either CD or POME and also there were no competitions between napropamide and DOC extracted from either CD or POME for sorption sites of the soil samples.     

小球藻对镉离子的吸附速率方程

研究了小球藻对Cd^2 的吸附动力学。研究表明,小球藻对Cd^2 有一定的吸附作用,在吸附的起始阶段,吸附速率较快,且随温度的升高吸附速率增大,吸附过程在20min内达到平衡。结果还表明,该吸附是简单的一级反应,并由此建立了吸附反应的速率方程,推算出吸附反应的活化能Ea=31．42kl／mol。     

Effect of Soil Chemical and Physical Properties on Sorption and Desorption Behavior of Lead in Different Soils of India

Lead (Pb) is a non-biodegradable contaminant, present in the environment, especially near lead-based industrial sites, agricultural lands, and roadside soils. Bioavailability of Pb in the soil is controlled by the sorption and desorption behavior of Pb, which are further controlled by the soil chemical and physical properties. In this study, sorption and desorption amounts of Pb in soil were compared with soil physical (sand, silt, clay content) and chemical (pH; electrical conductivity, EC; percent organic carbon, (%OC); cation exchange capacity, CEC) properties. Twenty-six surface soils (0–5cm), expected to vary in physical and chemical properties, were collected from different parts of India and were treated with known concentration of Pb solution (40 μg/L). The amount of Pb sorbed and desorbed were measured and correlated with soil properties using simple linear regressions. Sorption was significantly (p ≤ 0.05) and positively correlated with pH, and %OC; desorption was significantly (p ≤ 0.05) negatively correlated with the same two factors. Stepwise multiple regressions were performed for better correlations. Predicted sorption and desorption amounts, based on multiple regression equations, showed reasonably good fit (R² = 0.79 and 0.83, respectively) with observed values. This regression model can be used for estimation of sorption and desorption amounts at contaminated sites.     

Characteristics of Soil Organic Matter and Sorption of Phenanthrene,Naphthalene 1,3,5-TCB and o-Xylene

Nonlinear isotherm behavior has been reported for the sorption of hydrophobic organic compounds (HOCs) in soil/water systems, but the mechanisms are unclear. The model of “soft” and “hard” carbon domains has been extensively cited in the sorption literature to account for nonlinear sorption behaviors, but the structural compositions of soil organic matter (SOM) are not well understood. The objective of this study was to examine the characteristics of SOM and the effect of SOM heterogeneity on sorption isotherm by elemental analysis, organic petrographic examination, scanning electron microscopy, ¹³C nuclear magnetic resonance and studying the sorption behaviors of phenanthrene, naphthalene, 1,3,5-trichlorobenzene and o-xylene in soil and its isolated fractions, humic acid (HA) and humin (denser particulates and lighter particulates). DP mainly contained low maturation and high paraffinic carbon huminite. LP was composed of inertinite, huminite, vitrinite and exinite, with smaller particle size and higher maturation than DP. Humic acid approached the lignite coal rank.

All isotherms were nonlinear, and nonlinearity increased in the following order: HA > DP > soil > BE > LP. The sorption of HOCs in soil was primarily regulated by SOM. Humic acid seemed to be the soft carbon domain and insoluble condensed organic matter (humin) the hard carbon domain. Isotherm nonlinearity was negatively correlated with hydrophobicity and molecular size, while sorption capacity increased with increase of these parameters. Aliphatic structures of SOM, as observed for LP, could also contribute to both isotherm nonlinearity and large sorption capacity.     

Sorption and precipitation of metals in activated sludge

A conceptual model describing the relative roles of sorption and precipitation processes for metals in solid-solution suspensions is presented. The model performance is demonstrated using experimental data on sorption and precipitation of metals in samples of activated sludge mixed liquor. Based on the experimental results presented here, it appears that, at total metal and mixed liquor suspended solids concentrations and pH values generally encountered in full-scale municipal (or combined municipal/industrial) activated sludge systems, metals are primarily removed by sorption processes.     

Influence of the Interactions Between Black Carbon and Soil Constituents on the Sorption of Pyrene

Biochar (a kind of black carbon (BC)) has been advocated as a promising additive to farmland, thus it is crucial to understand the influence of BC on the fate of hydrophobic organic chemicals (HOCs) when they exist in soil. This study explored the sorption of pyrene onto a BC sample obtained by pyrolyzing pine sawdust, two soils, clay (kaolinite), and the mixtures thereof to investigate the influence of the interactions between BC and soil constituents on the sorption of HOCs and the mechanisms therein. Sorption of pyrene onto soil?BC mixtures was significantly less than that predicted by the sum of the individual soil and BC sorption, indicating that the sorption of pyrene onto soil and BC did not occur independently. The reduction of BC sorption capacity in soil seemed primarily to be caused by soil dissolved organic matter (DOM), which attenuated pyrene sorption onto BC by 18.7%?40.3% (within pyrene equilibrium concentration range of 0.05?0.5 S _w). These were likely due to the blockage of micropores, reduced accessibility of sorption sites, and binding of pyrene by DOM in aqueous solution. In addition to the DOM effect, kaolinite also diminished pyrene sorption onto BC to some extent, which suggested additional interaction between BC and soil particles. Pyrene sorption onto the soil?BC mixtures varied with water content and contact time. The influence of wet versus dry conditions and contact time on the K_oc of pyrene was more obvious when pyrene equilibrium concentrations were lower. The effect of aging also varied with soil properties. In summary, BC could not behave independently in soil, and its sorption capacity was changed by its interactions with soil constituents, which may be influenced by soil properties, environmental condition, and contact time.     

Copper,Lead, Cadmium,and Zinc Sorption By Waterlogged and Air-Dry Soil

Competitive sorption of copper (Cu), lead (Pb), cadmium (Cd), and zinc (Zn) was studied in three soils of contrasting chemical and physical properties under air-dry and waterlogged conditions. Competitive sorption was determined using the standard batch technique using six solutions, each with Cu, Pb, Cd, and Zn concentrations of approximately 0, 2.5, 5, 10, 20, and 50?mg L^?1Waterlogged soils tended to sorb higher amounts of added Cu, Pb, Zn and Cd relative to soils in the air-dry condition; however, this increase in sorption was generally not statistically (p<0.05) significant. The magnitude of sorption under both waterlogged and air-dry conditions was affected by the type and amount of soil materials involved in metal sorption processes, and competition between other metals for the sorption sites. Metal sorption was closely correlated with soil properties such as cation exchange capacity, organic carbon, and Fe and Mn hydrous oxides. Exchangeable Al may have markedly reduced metal sorption due to its strong affinity for the sorption sites, while increases in exchangeable Mn may have enhanced Zn and Cd sorption. Heavy metal sorption was best described as a combination of both specific and nonspecific interactions. The extractability of Cu, Pb, Cd, and Zn under waterlogged and air-dry conditions was also studied. Three solutions containing these metals were mixed with each soil to achieve a final concentration of 0, 50, and 500?mg kg^?1. Each soil was extracted every 7 days using 1?M MgCl₂ (pH 7) to determine metal extractability. Metal extractability initially decreased then increased due to waterlogging. The increased extractability of added metals was closely related to increased solubility of Fe and Mn suggesting that dissolution of Fe and Mn, oxides under reducing conditions caused a release of previously sorbed Cu, Pb, Cd, and Zn.     

The Sorption of Ketotifen Fumarate by Chitosan

The purpose of this investigation was to determine the mechanism of interaction between ketotifen fumarate and chitosan at different pH values. The specific surface area of chitosan was determined using gas sorption analyzer. The sorption experiments were conducted at pH 7 and 10 using two different particle size ranges of chitosan. The solutions were prepared at constant ionic strength and buffer concentration, with only varying the pH. The rotating bottle method was used for measuring the sorption. The average specific surface areas for the two different particle size ranges of chitosan were found to be 4.56 and 0.74 m²/g. The Langmuir-like equation and a model independent equation were both applied to the sorption experimental data. The extent of ketotifen uptake at pH 7 for small and large particles of chitosan was found to be 1,073 and 2,204 mg/g respectively. While the extent of ketotifen uptake at pH 10 for small and large particles of chitosan was found to be 4 and 11 mg/g respectively. The aforementioned results indicated that sorption of ketotifen fumarate at pH 7 is extremely high compared to pH 10 and that the sorption increases by decreasing the specific surface area of chitosan. Based on the results obtained, the following conclusions were reached. Ketotifen might be absorbed into the bulk structure of chitosan in addition to being adsorbed on the surface and the ability of chitosan to swell at pH 7 has a significant role in increasing its uptake.     

Norfloxacin Sorption to Different Fractions in Sediments from Typical Water Systems in China

Sorption isotherms of Norfloxacin (NOF) to different fractions from six typical sediments in China were determined to compare the NOF sorption behavior and contribution of different fractions to total sorption. All sorption isotherms were nonlinear and fitted well with the Freundlich model. Sorption coefficients (K _f) by original sediments changed in larger magnitude, from 114 (mg/g)/(mg/L)ⁿ to 5271 (mg/g)/(mg/L)ⁿ, and black carbon with more aromatic carbon has more sorption capacity and nonlinearity. The sorption capacity K _f values were found to significantly correlate with SSA (specific surface area), OC (organic carbon), BC (black carbon), and TON (total organic nitrogen) (p < 0.05), but had no obvious relation with pH, CEC (cation exchange capacity), TOC/TON, and BC/TOC. The DOC removed, NaOH extracted, and 375°C heated fractions showed more nonlinear sorption than the original sediments, suggesting more heterogeneous sorption sites in these fractions. Among different sediment fractions, the 375°C heating fractions were responsible for >50% of the total NOF sorption over the whole concentration range. The contribution of DOC removed fractions to the total sorption was the highest at higher NOF concentration.     

Comparison of Pesticide Sorption by Physicochemically Modified Soils with Natural Soils as a Function of Soil Properties and Pesticide Hydrophobicity

The objectives of this paper were to determine the efficiency of physicochemically modified soils with a surfactant in the sorption of pesticides, the stability against washing of the pesticides sorbed, and the effective sorption capacity of surfactant adsorbed by soils as a function of pesticide hydrophobicity and soil characteristics. Five soils of different characteristics and five pesticides (penconazole, linuron, alachlor, atrazine and metalaxyl) with different Kow values were selected and octadecyltrimethylammonium bromide (ODTMA) was chosen as model of cationic surfactants. Sorption-desorption isotherms were obtained and constants Kf and Kfd for natural soils (from Freundlich equation) and K and Kd for ODTMA-soils (from linear equation) were determined. Sorption on ODTMA-soils was higher than on natural soils. K increased 27–165 times for penconazole, 22–77 times for linuron, 7–14 times for alachlor, 9–23 times for atrazine, and 21–333 times for metalaxyl in relation to Kf. Sorption coefficients normalized to 100% of total organic matter (TOM) from organo soils K_OM (K 100/%TOM), were always higher than those from natural soils Kf_OM (Kf 100/%OM), indicating that the organic matter (OM) derived from the ODTMA (OM_ODTMA) had a greater sorption capacity than the OM of the natural soil. K_OM values were also higher than the Kow (octanol/water distribution coefficient) value for each pesticide. The similarity of the high K_OM values for the sorption of each pesticide by the five soils and the linearity of isotherms point to a partitioning of the pesticides between surfactant and water. The use in this work of different soils and various pesticides, unusual in this type of investigation, allowed us to obtain equations to know the sorbed amount of a given pesticide by the surfactant-modified soils as a function of the OM content derived from the cation and the Kow of the pesticide. The results obtained are of interest when it becomes necessary to increase the sorption capacity of soils with low OM contents with a view to delaying pesticide mobility in soils from pollution point sources (high concentration in small area), and preventing the pollution of waters.     

Metal Sorption to Pseudomonas fluorescens: Influence of pH,Ionic Strength and Metal Concentrations

Migration behavior of radionuclides should be understood in order to estimate the impact of high-level radioactive waste (HLW) disposal on the environment. Bacteria, one of the major organic sorbents in solid and aquatic environments, can affect the fate of actinides and lanthanides by sorption onto their cell surfaces. In this study, the sorption of the radionuclide Americium (Am(III)) and several metal ions (Eu(III), Cu(II) and Ca(II)) to Pseudomonas fluorescens were measured under various conditions. It was revealed that as pH decreased, the sorption of Eu(III) and Am(III) increased when the metals were at relatively low concentrations but decreased at higher metal concentrations. On the other hand, sorption of Cu(II) followed the opposite trend. In the case of calcium, an increase in calcium ions was observed due to release from the cells. These findings suggest that the sorption mechanisms for low levels of Eu(III) and Am(III) on the cells of Pseudomonas fluorescens are different from those of Cu(II), Ca(II), and high concentrations of Eu(III) (> 10 ^{? 5} M).     

Cadmium Sorption Characteristics of Soil Amendments and its Relationship with the Cadmium Uptake by Hyperaccumulator and Normal Plants in Amended Soils

In order to select appropriate amendments for cropping hyperaccumulator or normal plants on contaminated soils and establish the relationship between Cd sorption characteristics of soil amendments and their capacity to reduce Cd uptake by plants, batch sorption experiments with 11 different clay minerals and organic materials and a pot experiment with the same amendments were carried out. The pot experiment was conducted with Sedum alfredii and maize (Zea mays) in a co-cropping system. The results showed that the highest sorption amount was by montmorillonite at 40.82 mg/g, while mica was the lowest at only 1.83 mg/g. There was a significant negative correlation between the n value of Freundlich equation and Cd uptake by plants, and between the logarithm of the stability constant K of the Langmuir equation and plant uptake. Humic acids (HAs) and mushroom manure increased Cd uptake by S. alfredii, but not maize, thus they are suitable as soil amendments for the co-cropping S. alfredii and maize. The stability constant K in these cases was 0.14–0.16 L/mg and n values were 1.51–2.19. The alkaline zeolite and mica had the best fixation abilities and significantly decreased Cd uptake by the both plants, with K ≥ 1.49 L/mg and n ≥ 3.59.     

Distinct Microbial Communities within the Endosphere and Rhizosphere of Populus deltoides Roots across Contrasting Soil Types

The root-rhizosphere interface of Populus is the nexus of a variety of associations between bacteria, fungi, and the host plant and an ideal model for studying interactions between plants and microorganisms. However, such studies have generally been confined to greenhouse and plantation systems. Here we analyze microbial communities from the root endophytic and rhizospheric habitats of Populus deltoides in mature natural trees from both upland and bottomland sites in central Tennessee. Community profiling utilized 454 pyrosequencing with separate primers targeting the V4 region for bacterial 16S rRNA and the D1/D2 region for fungal 28S rRNA genes. Rhizosphere bacteria were dominated by Acidobacteria (31%) and Alphaproteobacteria (30%), whereas most endophytes were from the Gammaproteobacteria (54%) as well as Alphaproteobacteria (23%). A single Pseudomonas-like operational taxonomic unit (OTU) accounted for 34% of endophytic bacterial sequences. Endophytic bacterial richness was also highly variable and 10-fold lower than in rhizosphere samples originating from the same roots. Fungal rhizosphere and endophyte samples had approximately equal amounts of the Pezizomycotina (40%), while the Agaricomycotina were more abundant in the rhizosphere (34%) than endosphere (17%). Both fungal and bacterial rhizosphere samples were highly clustered compared to the more variable endophyte samples in a UniFrac principal coordinates analysis, regardless of upland or bottomland site origin. Hierarchical clustering of OTU relative abundance patterns also showed that the most abundant bacterial and fungal OTUs tended to be dominant in either the endophyte or rhizosphere samples but not both. Together, these findings demonstrate that root endophytic communities are distinct assemblages rather than opportunistic subsets of the rhizosphere.     

Free Cyanide Sorption on Freshwater Sediment and Model Components

The sorption of free cyanide (HCN) on mineral components of sediment, activated carbon, and a freshwater sediment was studied via batch experiments in synthetic freshwater at pH 6.4–7.6. It was found that free cyanide did not sorb to any significant extent on sediment mineral components, but did sorb strongly to activated carbon and moderately to a freshwater sediment. Results of experiments with 100 and 150 μ g/L free cyanide spike amounts resulted in no observed sorption to kaolin clay, Ottawa sand, or alumina in the synthetic freshwater. Extensive removal of free cyanide from the aqueous phase was observed in the partitioning experiments with the powdered activated carbon. Results with whole sediment indicated up to 46% removal of free cyanide from the aqueous phase in experiments with 20 and 50 μ g/L free cyanide. The organic-carbon-normalized distribution coefficient K_oc (= C_s/C_wf_oc) for free cyanide sorption on the activated carbon (f_oc = 1.0), 4.2 L/g_s, was similar to the K_oc value for free cyanide sorption on the freshwater sediment (f_oc = 0.0031), approximately 12.9 L/g_s. The results indicate that free cyanide can sorb to sediments with organic carbon content under freshwater conditions, primarily through interaction of HCN with organic carbon in the sediment.     

Sorption and release of radiocaesium from particulate matter of the Baltic coastal zone

Laboratory expriments have demonstrated that radiocaesium can be released in different proportions from Baltic sediments, depending on the type and origin of sediment, contact time and solid-to-liquid phase ratio. Rapidly accumulating sediments in areas affected by river discharge have much higher percentage of exchangeable radiocaesium than slowly accumulating marine sediments. The latter have been shown to {uptake radiocaesium from overlying sea water at high suspended loads. Pronounced radiocaesium gradients at sediment-water interface in Gda\'nsk Bay can be explained by either diffusion from pore water or desorption from sediment particles uprised by waves and/or bottom currents, or a combination of both. Desorption is likely to decrease with age of the sediment.