Cereal/legume rotations affect chemical properties and biological activities in two West African soils

A more widespread use of cereal/legume rotations has been suggested as a means to sustainably meet increasing food demands in sub-Saharan West Africa. Enhanced cereal yields following legumes have been attributed to chemical and biological factors such as higher levels of mineral nitrogen (N_min) and arbuscular mycorrhizae (AM) but also to lower amounts of plant parasitic nematodes. This study was conducted under controlled conditions to examine the relative contribution of AM, plant parasitic nematodes and increased nitrogen (N) and phosphorus (P) availability to cereal/legume rotation effects on two West African soils. Sample soils were taken from field experiments at Gaya (Niger) and Fada (Burkina Faso) supporting continuous cereal and cereal/legume rotation systems and analysed for chemical and biological parameters. Average increases in cereal shoot dry matter (DM) of rotation cereals compared with continuous cereals were 490% at Gaya and 550% at Fada. Shoot P concentration of rotation millet was significantly higher than in continuous millet and P uptake in rotation cereals was on average 62.5-fold higher than in continuous cereals. Rotation rhizosphere soils also had higher pH at both sites. For the Fada soil, large increases in Bray1-P and organic P were observed in bulk and rhizosphere soils. Plant parasitic nematodes in roots of continuous cereals were 60–80-fold higher than in those of rotation cereals. In both cropping systems mycorrhizal infection rates were similar at 37 days after sowing (DAS) but at 57 DAS AM infection was 10–15% higher in rotation sorghum than in continuous sorghum. This study provides strong evidence that cereal/legume rotations can enhance P nutrition of cereals through improved soil chemical P availability and microbiologically increased P uptake.     

红壤旱地不同复种方式养地效果

为了提出适宜南方红壤区旱地质量提升的持续高效种植模式,在江西农业大学科技园开展田间试验,以传统复种方式为对照,从土壤理化性状、微生物及酶活性等多方面分析比较不同复种方式对土壤的养地效果,为提出可持续发展的农田耕作模式提供理论基础。结果表明:不同复种方式中,绿肥种植和绿肥翻压还田对土壤具有明显养地效果,其中处理C"黑麦草-花生‖玉米-粟‖荞麦"具有较高的土壤阳离子交换量、有机质、碱解氮、全磷含量以及土壤酶活性和较多的土壤微生物种类、数量,从而显著提高土壤肥力和土壤持续生产力,养地效果最佳;处理B"混播绿肥(油菜、紫云英、肥田萝卜)-大豆‖玉米-绿豆‖芝麻"降低土壤容重,增加土壤孔隙度,改善土壤的通气性、透水性,明显提高土壤pH值、全氮、有效磷、全钾和速效钾含量,养地效果次之。因此,大力推广应用冬季绿肥是促进红壤旱地生态系统可持续发展的有效耕作措施。     

生物炭对不同土壤化学性质、小麦和糜子产量的影响

以小麦和糜子为供试作物,利用室外盆栽试验,研究了不同添加量生物炭与矿质肥配施对两种不同土壤化学性质及小麦和糜子产量的影响。生物炭当季用量设5个水平：B0 (0 t/hm2)、B5 (5 t/hm2)、B10 (10 t/hm2)、B15 (15 t/hm2)和B20 (20 t/hm2),氮磷钾肥均作基肥施用。结果表明：1.与对照相比,施用生物炭可以显著增加新积土糜子季土壤pH值,其他处理随生物炭用量的增加虽有增加趋势但差异不显著;显著增加新积土土壤阳离子交换量,增幅为1.5 %—58.2 %;显著增加两种土壤有机碳含量,增幅为31.1 %—272.2 %;2.两种土壤的矿质态氮含量、新积土土壤有效磷和速效钾含量随生物炭用量的增加而显著提高,氮磷钾增幅分别为6.0 %—112.8 %、3.8 %—38.5 %和6.1 %—47.2 %;3.生物炭可显著提高塿土上作物氮吸收量,而作物磷、钾吸收量虽有增加,但差异不显著。生物炭对小麦和糜子的增产效应尚不稳定,在试验最高用量时甚至产生轻微抑制作用。总之,施用生物炭在一定程度上可以改善土壤化学性质,提高土壤有效养分含量,但生物炭对土壤和作物的影响与土壤、作物类型及土壤肥力密切相关。     

Structural changes associated with poliovirus inactivation in soil.

The loss of infectivity of poliovirus in moist and dried soils was a result of irreversible damage to the virus particles. The damage included (i) dissociation of viral genomes and capsids and (ii) degradation of viral ribonucleic acid (RNA) in the soil environment. Under drying conditions, capsid components could not be recovered from the soils. Further studies in sterile soils indicated that, under moist conditions, the viral RNA was probably damaged before dissociation from the capsid. However, in sterile, dried soil, RNA genomes were recovered largely intact from the soil. These results suggest that polioviruses are inactivated by different mechanisms in moist and drying soils.     

Structural changes associated with poliovirus inactivation in soil.

The loss of infectivity of poliovirus in moist and dried soils was a result of irreversible damage to the virus particles. The damage included (i) dissociation of viral genomes and capsids and (ii) degradation of viral ribonucleic acid (RNA) in the soil environment. Under drying conditions, capsid components could not be recovered from the soils. Further studies in sterile soils indicated that, under moist conditions, the viral RNA was probably damaged before dissociation from the capsid. However, in sterile, dried soil, RNA genomes were recovered largely intact from the soil. These results suggest that polioviruses are inactivated by different mechanisms in moist and drying soils.     

Responses of Wetland Tree Species to Hydrology and Soils

We conducted a study of the flood tolerance of nine wetland tree species on seven soil types. Seedlings were subjected to 11 months of continuous shallow inundation or moist soil conditions on three mineral soils, two organic soils, a manufactured soil designed to mimic the practice of layering muck over mineral soil, and a stockpiled topsoil. Taxodium ascendens, T. distichum, Acer rubrum, and Pinus serotina suffered no mortality; Fraxinus carolininna (1%), Liquidambar styraciflua (8%), P. elliottii (8%), and Gordonia lasianthus (24%) suffered low to moderate mortality; and Persea palustris (46%) suffered significant mortality. In general, greatest net height and total biomass were achieved on moist organic soils, and least net height and total biomass were achieved on stockpiled topsoil and inundated soils. Responses to hydrological conditions were less pronounced for Taxodium spp. If the results of this experiment are transferable to the field, then Acer rubrum, Fraxinus caroliniana, Pinus serotina, Taxodium ascendens, and Taxodium distichum seedlings can reasonably be expected to survive at least one year under a broad range of hydrological and edaphic conditions. With the exception of Taxodium spp., first-year growth for the species of this study can be facilitated by maintaining moist but not inundated conditions. These findings suggest that transfer of organic soils will benefit restoration and creation efforts, and that layering organic soil over mineral soil is more effective than using mineral soils or stockpiled topsoil.     

Soil moisture influence on micronutrient cation availability under aerobic conditions

Summary The three major soil series comprising the Gezira scheme (Sudan) are Hosh, Suleimi, and Laota. Surface soil samples from each soil series were employed to study the effect of soil moisture on the DTPA-extractable micronutrient cation under aerobic conditions. The study continued for 8 weeks using an incubation technique at two levels of soil moisture (continuously moist and moist/dry cycles). The DTPA-extractable Cu, Fe, Mn and Zn from air-dry soil samples were much higher compared to values from their incubated counterparts. For the three soils the CO₂ production (microbial activity) reached the maximum in 5 weeks and then levelled off while the lowest values of micronutrient cation from the incubated soils were obtained between 2 to 8 weeks.Generally, the study suggests that the hot dry months preceding crop growth should increase clay surface acidity and hence availability of mironutrient cations.Contribution from the Texas Agricultural Experiment Station, Texas A&M University, College Station. TX 77843, U.S.A.     

拟茎点霉B3与有机肥配施对连作草莓生长的影响

通过盆栽试验探讨了内生拟茎点霉B3与有机肥配施对连作草莓土壤的改善及对草莓生长的影响。试验共设5个处理,分别为对照(CK)、施有机肥与灭菌固体培养基(A)、施有机肥与内生拟茎点霉B3固体菌种(B)、施有机肥与绿色木霉、黑曲霉、枯草芽孢杆菌固体菌种(C)、施加有机肥与绿色木霉、黑曲霉、枯草芽孢杆菌和内生拟茎点霉B3固体菌种(D)。结果表明:A、B、C和D处理平均单果鲜重分别为对照(CK)的1.1、1.4、0.9和1.1倍。B处理比对照增产19.7%,A处理增产8.2%,C和D处理产量均比CK低。B处理草莓生长最好,植株株高及叶面积均值比其它4个处理大。发病率及病情指数结果表明B处理抗病效果最明显,推断内生拟茎点霉B3可以用作生防菌剂。进一步的研究表明土壤真菌和细菌数量在整个生育期先上升后下降,在花期达到最大。成熟期A、B、C、D处理的土壤放线菌数量分别比CK增加7.2%、160.3%、124.5%及82.6%。在花期,B处理及D处理蔗糖酶酶活达到最大,其中A、B、C及D处理的蔗糖酶酶活分别比CK高11.1%、69.4%、50.3%及77.2%。B处理整个生育期都保持较高的土壤蔗糖酶活性。花期是草莓生长的关键期,需氮量较高。A、B、C及D处理脲酶酶活分别比CK处理高250.0%、700.0%、250.0%及175.0%,B处理花期土壤脲酶酶活性显著高于其它4个处理,促进了有机氮向速效氮的转化。花期A、C处理磷酸酶酶活比对照低67.0%、46.7%,B、D处理比对照高122.5%,227.5%。B处理在整个生育期都有较高的土壤磷酸酶酶活, D处理组在花期土壤磷酸酶酶活较高。可见含内生拟茎点霉B3菌的B及D处理组能增加土壤磷酸酶酶活。B处理在苗期和花期土壤纤维素酶活较低,而结果期和成熟期较高。说明内生拟茎点霉B3菌剂与有机肥配施可以改善连作草莓土壤微生物区系,提高土壤酶活性,增强草莓抗病能力,增加草莓产量,是一种有效缓解草莓连作障碍的方法。     

Effects of Amendments and Water Conditions on the Chemical Speciation of Cd and Pb in Contaminated Paddy Soil in a Mining Area

Lime, sepiolite and peat were used as amendments to study their effects on the chemical speciation of Cd and Pb in a polluted paddy soil under moist and water-logged conditions. The results showed that application of amendments reduced acid-extractable Cd (up to 12.56% and 5.07%) and Pb (up to 6.69% and 2.68%) in moist and water-logged soils, respectively. The reducible Cd and residual Cd was increased while the oxidizable Cd was decreased after adding amendments. However, the oxidizable Pb was increased while the residual Pb was decreased in amended soil, and the reducible Pb presented a different changing trend under moist and water-logged conditions. The soil pH was significantly correlated with different fractions of Cd and Pb in soil, which indicated a distinct influence of soil pH on the redistribution process of Cd and Pb fractions in amended soil.     

Root-induced increases in soil pH and nutrient availability to field-grown cereals and legumes on acid sandy soils of Sudano-Sahelian West Africa

A field experiment with millet (Pennisetum glaucum L.), sorghum [Sorghum bicolor (L.) Moench], cowpea (Vigna unguiculata L.) and groundnut (Arachnis hypogeae L.) was conducted on severely P-deficient acid sandy soils of Niger, Mali and Burkina Faso to measure changes in pH and nutrient availability as affected by distance from the root surface and by mineral fertiliser application. Treatments included three rates of phosphorus (P) and four levels of nitrogen (N) application. Bulk, rhizosphere and rhizoplane soils were sampled at 35, 45 and 75 DAS in 1997 and at 55 and 65 DAS in 1998. Regardless of the cropping system and level of mineral fertiliser applied, soil pH consistently increased between 0.7 and two units from the bulk soil to the rhizoplane of millet. Similar pH gradients were observed in cowpea, but pH changes were much smaller in sorghum with a difference of only 0.3 units. Shifts in pH led to large increases in nutrient availability close to the roots. Compared with the bulk soil, available P in the rhizoplane was between 190 and 270% higher for P-Bray and between 360 and 600% higher for P-water. Exchangeable calcium (Ca) and magnesium (Mg) levels were also higher in the millet rhizoplane than in the bulk soil, whereas exchangeable aluminium (Al) levels decreased with increasing pH close to the root surface. The results suggest an important role of root-induced pH increases for crops to cope with acidity-induced nutrient deficiency and Al stress of soils in the Sudano-Sahelian zone of West Africa. This revised version was published online in June 2006 with corrections to the Cover Date.     

Response of millet and sorghum to a varying water supply around the primary and nodal roots

Background and Aims

Cereals have two root systems. The primary system originates from the embryo when the seed germinates and can support the plant until it produces grain. The nodal system can emerge from stem nodes throughout the plant''s life; its value for yield is unclear and depends on the environment. The aim of this study was to test the role of nodal roots of sorghum and millet in plant growth in response to variation in soil moisture. Sorghum and millet were chosen as both are adapted to dry conditions.

Methods

Sorghum and millet were grown in a split-pot system that allowed the primary and nodal roots to be watered separately.

Key Results

When primary and nodal roots were watered (12 % soil water content; SWC), millet nodal roots were seven times longer than those of sorghum and six times longer than millet plants in dry treatments, mainly from an 8-fold increase in branch root length. When soil was allowed to dry in both compartments, millet nodal roots responded and grew 20 % longer branch roots than in the well-watered control. Sorghum nodal roots were unchanged. When only primary roots received water, nodal roots of both species emerged and elongated into extremely dry soil (0·6–1·5 % SWC), possibly with phloem-delivered water from the primary roots in the moist inner pot. Nodal roots were thick, short, branchless and vertical, indicating a tropism that was more pronounced in millet. Total nodal root length increased in both species when the dry soil was covered with plastic, suggesting that stubble retention or leaf mulching could facilitate nodal roots reaching deeper moist layers in dry climates. Greater nodal root length in millet than in sorghum was associated with increased shoot biomass, water uptake and water use efficiency (shoot mass per water). Millet had a more plastic response than sorghum to moisture around the nodal roots due to (1) faster growth and progression through ontogeny for earlier nodal root branch length and (2) partitioning to nodal root length from primary roots, independent of shoot size.

Conclusions

Nodal and primary roots have distinct responses to soil moisture that depend on species. They can be selected independently in a breeding programme to shape root architecture. A rapid rate of plant development and enhanced responsiveness to local moisture may be traits that favour nodal roots and water use efficiency at no cost to shoot growth.     

In situ studies of soil mineral N fluxes: Some comments on the applicability of the sequential soil coring method in arable soils

Is the sequential in situ incubation of undisturbed soil cores, developed for forest stands applicable to arable soils? The incubation of covered and uncovered soil cores allows the estimation of net nitrogen mineralization (NNM), plant nitrogen uptake (N_uptake) and potential leaching losses (N_trans). The amounts and temporal dynamics of these N fluxes were determined at four arable soils in a two-year study. Results suggest that: (i) the method can not be recommended for the estimation of N uptake and leaching losses, but (ii) it is suitable for the estimation of NNM; (iii) incubations should preferably be started when soil is moist; (iv) the length of incubation periods should be reduced (<4 weeks); (v) dynamics of NNM is mainly determined by temperature and moisture conditions if there is no interference by agricultural management. Inputs of straw, manure, slurry or green manure strongly influence the amount and the dynamics of NNM.     

The influence of phosphorus and nitrogen on millet and clover growing in soils affected by salinity

Summary The growth of foxtail millet and clover in soils of varying degrees of salinity (0.5 to 13 mmhos/cm), treated with nitrogen and phosphorus, was studied. Salinity levels were achieved by addition of sodium chloride. Nitrogen (10 to 60 ppm N) and phosphorus (6.4 to 44.8 ppm P) were added as NH₄NO₃ and H₃PO₄, respectively. The growth of millet decreased sharply with increase in soil salinity, when N-P treatments were not applied. The development of this plant altered under saline conditions, however, when nitrogen and phosphorus were added; various N-P combinations affected plant growth in saline soil differently. Phosphorus, when applied at relatively high rates, significantly improved plant growth. Increased rates of nitrogen in the N-P treatments generally had no significant effect on growth; it was reduced when the N/P ration was highest. Clover ceased to grow when the salinity of the soil exceeded 7 mmhos/cm and no N-P was added. Phosphorus enhanced the growth of clover, and at high rates of its application in the N-P combinations, clover grew even at the highest salinity level tested (13 mmhos/cm). Nitrogen increase had no marked effect on plant development. Comparing enhancement of growth at high salinity levels, clover was somewhat less affected by the N-P treatment than millet. The top/root ratio of clover generally increased with increase of phosphorus in the N-P combinations. This research (Parts I and II) was supported in part by a grant from the U.S. Department of Agriculture under P. L. 480.     

Some factors affecting the mineralization of organic sulphur in soils

Summary Factors affecting the release of sulphate from a number of eastern Australian soils were studied.All of the soils released sulphate when dried. The amounts released were influenced by the manner in which the soil was dried. Air-drying in the laboratory at 20°C released least sulphate.Sulphate was mineralized in all soils by incubation at 30°C but the amounts mineralized could not be related to soil type or any single soil property. The ratio of nitrogen mineralized: sulphur mineralized varied widely between soils and was generally appreciably greater than the ratio of total nitrogen: organic sulphur in the soils.A rapid flush of mineralization of both sulphur and nitrogen took place when some of the soils were rewetted and incubated after they had been dried in the laboratory and stored for 4 to 5 months. Following this, the rate of mineralization was similar to that in the original undried soil. During this flush, the enhancement of sulphur mineralization was relatively greater than that of nitrogen so that the ratio of nitrogen mineralized: sulphur mineralized was considerably smaller than that during later phases of the incubation or that of the original moist soil. Soils collected after they had remained dry in the field for a similar period of time did not show this type of mineralization although they had initially done so when collected moist and air-dried in the laboratory.The effects of temperature, soil moisture, toluene and formaldehyde, and the addition of calcium carbonate to soils on the mineralization of sulphur were similar to their effects on the mineralization of nitrogen.     

Modelling yield losses of aluminium-resistant and aluminium-sensitive wheat due to subsurface soil acidity: effects of rainfall, liming and nitrogen application

Subsurface soil acidity reduces the growth of roots, which can potentially decrease crop yields. However, the magnitude of these yield reductions is dependent on interactions between factors such as the depth and severity of subsurface soil acidity, plant resistance to acidity, and water and nutrient availability. The Agricultural Production Systems Simulator (APSIM) was used to examine effects of these factors and their interactions on wheat yields in the Mediterranean climatic regions of Western Australia. The model was linked to historical meteorological data of the region (up to 90 different seasons), and was run for three locations representing low, medium and high rainfall zones and three constant but contrasting soil acidity profiles in a deep sandy soil with two wheat cultivars differing in aluminium (Al) resistance. The simulated results showed inherently high variability between seasons in grain yield, rooting depth and nitrogen leaching. Subsurface soil acidity could decrease average grain yields by up to 60%, particularly in soil profiles with acidity in deep layers. The adverse effects of acidity on wheat yields were greater in the high than the low rainfall zone. Amelioration of acidity by 75% in the entire profile or in the top 20-cm layer improved the yield of the Al-sensitive wheat cultivar. Growing Al-resistant wheat partially eliminated the negative effects of acidity on yields in soils with severe subsurface acidity and almost fully eliminated these negative effects in soils with moderate subsurface acidity. The yield benefits arising from growing Al-resistant wheat were greater than those from ameliorating acidity in the 0–20 cm layer by liming. Increasing nitrogen input increased yields of both Al-sensitive and Al-resistant wheat grown in acid soils in all the rainfall zones, but the yield increments were much greater in the high than the low rainfall zones. Applications of nitrogen fertilisers mitigate the effect of acidity on yields of Al-sensitive wheat in soils with shallow (10–40 cm) subsurface acidity. Furthermore, the improved yield by growing Al-resistant wheat and amelioration of acidity was correlated with increased rooting depth and was associated with decreased nitrogen leaching. Possible agronomic management options to combat the subsurface acidity problem are discussed.     

The influence of fertilizers,soil organic matter and soil compaction on maize yields on the Surinam ‘Zanderij’ soils

Summary In connection with the growing interest in Surinam to exploit the soils in the hinterland, some trials were carried out on Zanderij soils to study productivity, fertilizer need and influence of some special soil factors on yield. The test crop was maize. The yields were generally low which might partly be attributed to the relative dry weather conditions during the trials. On all soils investigated, yield responses to phosphate application were high. On loamy soils there was sometimes a response to nitrogen and on sandy soils to potassium. Yields on sands were lower than on loamy sands and sandy loams. The most important yield determining soil factor proved to be organic matter. On compacted soils yields were considerably lower which was due to increased mechanical impedance for root growth and in some cases to inadequate aeration. Also published as Bulletin of the Agricultural Experiment Station, Paramaribo, Surinam. Also published as Bulletin of the Agricultural Experiment Station, Paramaribo, Surinam.     

Dry matter response of ryegrass to ammonium and nitrate sources of nitrogen as a function of soil texture and moisture

Summary InLolium perenne cv. S23 grown in pots of soil to which nitrogen was applied at rates of 0, 60, 120 and 180 mg N/kg, ammonium significantly increased root mass compared with nitrate, whereas both nitrogen sources produced similar yields of herbage. Total dry matter production in the herbage and roots increased within the textural sequence: loamy sand, coarse sandy loam and loam. The increases in the latter two soils over the loamy sand were 35% and 50%, respectively. Depletions of available water of 50% and 80% reduced yields at the first harvest by 19% and 50% compared with the field capacity. The corresponding reductions in the second harvest were only 16% and 10%, because residual effects were then limiting. The amount of dry matter produced per unit of nitrogen absorbed indicated that textural class was less restrictive than moisture supply to efficient use of nitrogen within the plant. Furthermore, its efficient physiological use was limited at the 50% depletion, although its absorption from the soil was not affected. The results illustrated the inefficiency of the substitution of nitrogen for soil moisture: even at low yield levels three times more nitrogen was absorbed per unit increase in dry matter at 80% depletion of available water compared with the field capacity. The significant first-order interactions that affected yield were moisture by soils, and moisture by nitrogen rate.     

Survival of Cowpea Rhizobia in Soil as Affected by Soil Temperature and Moisture

Successful inoculation of peanuts and cowpeas depends on the survival of rhizobia in soils which fluctuate between wide temperature and moisture extremes. Survival of two cowpea rhizobial strains (TAL309 and 3281) and two peanut rhizobial strains (T-1 and 201) was measured in two soils under three moisture conditions (air-dry, moist (−0.33 bar), and saturated soil) and at two temperatures (25 and 35°C) when soil was not sterilized and at 40°C when soil was sterilized. Populations of rhizobia were measured periodically for 45 days. The results in nonsterilized soil indicated that strain 201 survived relatively well under all environmental conditions. The 35°C temperature in conjunction with the air-dry or saturated soil was the most detrimental to survival. At this temperature, the numbers of strains T-1, TAL309, and 3281 decreased about 2 logs in dry soil and 2.5 logs in saturated soil during 45 days of incubation. In sterilized soil, the populations of all strains in moist soil increased during the first 2 weeks, but decreased rapidly when incubated under dry conditions. The populations did not decline under saturated soil conditions. From these results it appears that rhizobial strains to be used for inoculant production should be screened under simulated field conditions for enhanced survival before their selection for commercial inoculant production.     

Infectivity variation of Discaria trinervis-nodulating Frankia in Patagonian soil according to season and storage conditions

Changes in the infectious capacity of soilborne Frankia from the same site may depend on environmental conditions. To test this, we examined the effect of season of sampling, sample storage protocol and storage time. The nodulation capacity of Frankia from rhizospheric soils of Discaria trinervis (Hook et Arn.) Reiche (Rhamnaceae) growing in northwest Patagonia (Argentina) was measured using the most probable number method. Soil samples were collected seasonally and either stored moist at 4°C or air dried at room temperature for few days. Old (air-dried) soil samples were also assayed. All soils nodulated D. trinervis seedlings. Nodulation units (NU) ranged from 44 (spring, moist storage) to about 1 ml⁻¹ of soil (summer moist, and summer and autumn, air-dried storage), with intermediate values in other samples. Soils stored for 12 years, 6 months or 1 week had similar NU. Frankia NU positively correlated with soil water content ( r = 0.6, P < 0.05); therefore, it is likely that soil moisture is a relevant factor regulating soilborne Frankia nodulation ability in Patagonian soils. We suggest that Frankia can remain as spores or grow saprophytically in Patagonian soils.     

Hydrologic Regime Controls Soil Phosphorus Fluxes in Restoration and Undisturbed Wetlands

Many wetland restoration projects occur on former agricultural soils that have a history of disturbance and fertilization, making them prone to phosphorus (P) release upon flooding. To study the relationship between P release and hydrologic regime, we collected soil cores from three restoration wetlands and three undisturbed wetlands around Upper Klamath Lake in southern Oregon, U.S.A. Soil cores were subjected to one of three hydrologic regimes—flooded, moist, and dry—for 7.5 weeks, and P fluxes were measured upon reflooding. Soils from restoration wetlands released P upon reflooding regardless of the hydrologic regime, with the greatest releases coming from soils that had been flooded or dried. Undisturbed wetland soils released P only after drying. Patterns in P release can be explained by a combination of physical and biological processes, including the release of iron‐bound P due to anoxia in the flooded treatment and the mineralization of organic P under aerobic conditions in the dry treatment. Higher rates of soil P release from restoration wetland soils, particularly under flooded conditions, were associated with higher total P concentrations compared with undisturbed wetland soils. We conclude that maintaining moist soil is the means to minimize P release from recently flooded wetland soils. Alternatively, prolonged flooding provides a means of liberating excess labile P from former agricultural soils while minimizing continued organic P mineralization and soil subsidence.