Drainage Regimes Research Articles

Better Ways to Work Together

This interpretive essay looks broadly at natural resources law in the United States, at the body of law that has emerged out of lawmaking efforts to divide nature into parts, to prescribe use-rights in these parts, and to resolve ensuing conflicts. Generations ago private use rights were defined clearly in ways that enabled owners and outsiders to know the reach of private rights. Most lands were devoted to single resource uses. The situation today has become quite different. Use-rights today are vaguer (with more vagueness to come). Also, more lands are thought to contain multiple resources and value now extends to aesthetics and ecosystem functions. The upshots include rising conflicts, more impaired markets in resources, and evident failures to promote either efficient resource uses or desirable landscapes. These upshots, the essay contends, are linked to a general inability to see clearly the functions that natural resources law is called upon to perform in setting after setting, and, going further, then to link today’s conflicts to the specific ways that current law poorly performs these necessary functions. For reasons considered, private resource-use rights need to be embedded more expressly within well-designed governance regimes; within governance systems that are empowered to resolve conflicts among competing interests and, in doing, to bring contextual clarity to specific private entitlements. This means moving beyond longstanding assumptions that (i) the law defines rights, (ii) governments regulate uses, and (iii) courts resolve disputes — legal functions that, in fact, increasingly overlap. Needed today are new governance systems that blend these legal functions so as to enhance resource-use flexibility, to tailor rights to particular settings (physical and social), and to accommodate shifting needs and values. The best systems will likely blend the public and private in novel ways to resolve disputes more quickly, at lower cost, and with more involvement by affected parties. As examples the essay considers wildlife, surface water (in riparian and appropriation systems), minerals, drainage, and fire regimes.

Bayesian network for point and diffuse source phosphorus transfer from dairy pastures in South otago, new zealand.

Many factors affect the magnitude of nutrient losses from dairy farm systems. Bayesian Networks (BNs) are an alternative to conventional modeling that can evaluate complex multifactor problems using forward and backward reasoning. A BN of annual total phosphorus (TP) exports was developed for a hypothetical dairy farm in the south Otago region of New Zealand and was used to investigate and integrate the effects of different management options under contrasting rainfall and drainage regimes. Published literature was consulted to quantify the relationships that underpin the BN, with preference given to data and relationships derived from the Otago region. In its default state, the BN estimated loads of 0.34 ± 0.42 kg TP ha for overland flow and 0.30 ± 0.19 kg TP ha for subsurface flow, which are in line with reported TP losses in overland flow (0-1.1 kg TP ha) and in drainage (0.15-2.2 kg TP ha). Site attributes that cannot be managed, like annual rainfall and the average slope of the farm, were found to affect the loads of TP lost from dairy farms. The greatest loads (13.4 kg TP ha) were predicted to occur with above-average annual rainfall (970 mm), where irrigation of farm dairy effluent was managed poorly, and where Olsen P concentrations were above pasture requirements (60 mg kg). Most of this loading was attributed to contributions from overland flow. This study demonstrates the value of using a BN to understand the complex interactions between site variables affecting P loss and their relative importance.

A multi‐point electrical resistance measurement system for characterization of foam drainage regime and stability

Foam drainage regimes are significantly associated with the nature of the hydrodynamic resistance in foam structure. A multi‐point electrical resistance measurement technique has been applied for characterization of the drainage regimes and quantifying stability within standing foams. The capacity of the technique was confirmed by the estimation of macroscopic drainage rates for aqueous foams stabilized with sodium dodecyl sulfate. The drainage of sodium dodecylbenzenesulfonate, a commercial form of linear alkylbenzene sulfonate that is the most frequently used in household detergents was studied in detail by two complementary methods (forced and free drainage). The experimental data could be fitted using a power‐law with an exponent of 1/3 for forced drainage and of 1.0 for free drainage. These data indicate the following drainage behavior: mobile bubble surfaces, causing plug‐like flow within Plateau borders, thus dissipation mainly occurs inside the nodes. This research introduced an accurate method for quantifying foam stability that can be assessed by variations of real‐time measured foam heights that incorporate the evolution of the liquid content. © 2014 American Institute of Chemical Engineers AIChE J, 60: 3143–3150, 2014

Morphological, drainage and eolian controls on the microtidal Patara Beach sediments (eastern Mediterranean): Textural, geochemical and mineralogical investigations

The effects of dominant hydrodynamic, morphological, fluvial and hinterland geological source conditions on the texture and composition of the microtidal and dissipative Patara Beach (Mediterranean coast of SW Turkey) sediments were investigated at 47 locations. Patara Beach sediments are composed entirely of sand. Fine sand (5–94%) was more abundant in the northwestern section, while medium sand contents (2–94%) increased in the central and southeastern sections. Moderately-to well sorted (mostly 0.3–0.7 Ø) sediments tend to show overall better sorting towards the southeast, in the net longshore current direction. Terrigenous carbonate grains derived from the hinterland constituted 6–50% (as CaCO3) with varying tendencies to increase or decrease within sections alongshore. Total heavy mineral concentrations in bulk sediments (1–17%, mostly <5%) were highest in localities of offshore sandy spit formation and with intense aeolian processes. The heavy mineral concentration comprises magnetite, hematite, amphiboles, pyroxene, epidote, garnet, and chromite, a mineral assemblage reflecting mafic/ultramafic/ophiolitic and metamorphic sources and mineral deposits. The concentrations of major elements (Si, Al, Ca, K, Na, P, Fe, Ti) and others (Co, Ba) are comparable with the average composition of Earth's crust rocks, and variations can be related to the varying texture and lithologies of the sediments. Higher abundances of Mg (3.3–7.7%), Cr (0.2–6.7%) and Ni (195–588 ppm) must be contributed by particular ophiolite sources. Mn (3385–4585 ppm) indicates presently-mined mineral deposits on the coast. Wind, wave, current and fluvial drainage regimes and corresponding morphological changes together with distribution of geological source rocks have great influences on the texture and composition of Patara Beach sediments.

61 Five-min heart rate variability can predict obstructive angiographic coronary disease

<h3>Introduction</h3> Malignant pleural effusions (MPEs) can complicate most cancers, causing dyspnoea and impairing quality of life (QoL). Indwelling pleural catheters (IPCs) are a novel management approach allowing ambulatory fluid drainage and are increasingly used as an alternative to pleurodesis. IPC drainage approaches vary greatly between centres. Some advocate aggressive (usually daily) removal of fluid to provide best symptom control and chance of spontaneous pleurodesis. Daily drainages however demand considerably more resources and may increase risks of complications. Others believe that MPE care is palliative and drainage should be performed only when patients become symptomatic (often weekly to monthly). Identifying the best drainage approach will optimise patient care and healthcare resource utilisation. <h3>Methods and analysis</h3> A multicentre, open-label randomised trial. Patients with MPE will be randomised 1:1 to daily or symptom-guided drainage regimes after IPC insertion. Patient allocation to groups will be stratified for the cancer type (mesothelioma vs others), performance status (Eastern Cooperative Oncology Group status 0–1 vs ≥2), presence of trapped lung (vs not) and prior pleurodesis (vs not). The primary outcome is the mean daily dyspnoea score, measured by a 100 mm visual analogue scale (VAS) over the first 60 days. Secondary outcomes include benefits on physical activity levels, rate of spontaneous pleurodesis, complications, hospital admission days, healthcare costs and QoL measures. Enrolment of 86 participants will detect a mean difference of VAS score of 14 mm between the treatment arms (5% significance, 90% power) assuming a common between-group SD of 18.9 mm and a 10% lost to follow-up rate. <h3>Ethics and dissemination</h3> The Sir Charles Gairdner Group Human Research Ethics Committee has approved the study (number 2015-043). Results will be published in peer-reviewed journals and presented at scientific meetings. <h3>Trial registration number</h3> ACTRN12615000963527; Pre-results.

Improving water management practices to reduce nutrient export from rice paddy fields

Nitrogen (N) and phosphorus (P) loss from rice paddy fields represents a significant threat to water quality in China. In this project, three irrigation–drainage regimes were compared, including one conventional irrigation–drainage regime, i.e. continuous submergence regime (CSR), and two improved regimes, i.e. the alternating submergence–nonsubmergence regime (ASNR) and the zero‐drainage irrigation technology (ZDIT), to seek cost‐effective practices for reducing nutrient loss. The data from these comparisons showed that, excluding the nutrient input from irrigation, the net exports of total N and total P via surface field drainage ranged from −3.93 to 2.39 kg ha−1 and 0.17 to 0.95 g ha−1 under the CSR operation, respectively, while N loss was −2.46 to −2.23 kg ha−1 and P export was −0.65 to 0.31 kg ha−1 under the improved regimes. The intensity of P export was positively correlated to the rate of P application. Reducing the draining frequency or postponing the draining operation would shift the ecological role of the paddy field from a nutrient export source to an interception sink when ASNR or the zero‐drainage water management was used. In addition, since the rice yields are being guaranteed at no additional cost, the improved irrigation–drainage operations would have economic as well as environmental benefits.

Subglacial modulation of the hydrograph from glacierized basins

AbstractThe extent of basin glacierization has important implications for the hydrograph in part, because snow, firn and ice impart different delays in water transport through the system. Here, the significance of subglacial drainage morphology in modulating the hydrograph is examined with a one‐dimensional physically based model. The conceptual model of subglacial drainage comprises both ‘fast’ and ‘slow’ elements, respectively associated with summer and winter drainage regimes. The additional possibility of a permeable glacier substrate is taken into account by allowing water transport in a subglacial aquifer. Forced by prescribed rates of melt‐water delivery to the glacier bed, the model predicts glacier discharge by drainage system provenance. The effects of (1) ‘hard’ versus ‘soft’ glacier beds, (2) subsurface permeability and groundwater flow, and (3) glacier geometry are then investigated. Hydrograph character, in the form of peak timing and amplitude, symmetry with respect to the forcing, and the amplitude of diurnal fluctuations, is affected by the partitioning of water through the various flow elements. Hard beds and impermeable substrates maximize the discharge routed through the fast‐drainage system in the simulations, generally resulting in higher seasonal discharge maxima and stronger diurnal variations in discharge. High hydraulic transmissivities, either at the glacier bed or in underlying strata, hinder the development of the fast‐drainage system in the simulations, producing hydrographs of lower amplitude. Glacier geometry has a modest effect, with adverse bed slopes, very thick or very thin ice and short glacier lengths favouring prolonged drainage through the slow system. These results suggest that the morphology and evolution of the subglacial drainage system may play a significant role in determining the character of the hydrograph from glacierized basins. Copyright © 2008 John Wiley &amp; Sons, Ltd.

Stationary bathtub vortices and a critical regime of liquid discharge

A modified Lundgren model is applied for the description of stationary bathtub vortices in a viscous liquid with a free surface. Laminar liquid flow through the circular bottom orifice is considered in the horizontally unbounded domain. The liquid is assumed to be undisturbed at infinity and its depth is taken to be constant. Three different drainage regimes are studied: (i) subcritical, where whirlpool dents are less than the fluid depth; (ii) critical, where the whirlpool tips touch the outlet orifice; and (iii) supercritical, where surface vortices entrain air into the intake pipe. Particular attention is paid to critical vortices; the condition for their existence is determined and analysed. The influence of surface tension on subcritical whirlpools is investigated. Comparison of results with known experimental data is discussed.

Mobility of arsenic and selected metals during re-flooding of iron- and organic-rich acid-sulfate soil

The drainage-induced oxidation of iron-sulfide minerals in acid-sulfate soils has adversely affected large areas of coastal floodplains. Re-flooding of these soils, via the re-establishment of more natural drainage regimes, is a potential remediation approach. Here we describe the mobility of Al, As, Fe, Mn, Ni and Zn during controlled re-flooding of an Fe- and organic-rich acid-sulfate soil material. Soil re-flooding caused the onset of microbially-mediated Fe(III)-reduction, which raised the pH of the initially acidic (pH 3.4) soil to pH 6.0 to 6.5, thereby immobilizing Al. The process of Fe(III)-reduction released high concentrations of FeII and was associated with significant mobilization of As. During the early stages of re-flooding, FeII mobility was controlled by dissolution of schwertmannite (Fe8O8(OH)6SO4) with an ion activity product (IAP) of 1019 ± 2. The mobility of FeII was subsequently controlled by the precipitation of siderite (FeCO3) with an IAP spanning 10− 10 to 10− 7.5. The formation of acid-volatile sulfide (AVS), as a product of SO4-reduction, further retarded the mobility of FeII. Interactions with AVS also strongly immobilized Mn, Ni and Zn, yet had little effect on As which remained relatively mobile in the re-flooded soil. This study shows that the mobilization of As and Fe during soil re-flooding should be considered when planning remediation approaches for acid-sulfate soils.

Mass budget of the grounded ice in the Lambert Glacier–Amery Ice Shelf system

AbstractWe used remote-sensing and in situ measurements of surface accumulation rate, ice surface velocity, thickness and elevation to evaluate the mass budgets of grounded ice-flow regimes that form the Lambert Glacier–Amery Ice Shelf system. Three distinct drainage regimes are considered: the western and eastern margins of the ice shelf, and the southern grounding line at the major outlet glacier confluence, which can be identified with drainage zones 9, 11 and 10 respectively of Giovinetto and Zwally (2000). Our findings show the entire grounded portion of the basin is approximately in balance, with a mass budget of –4.2±9.8 Gt a–1. Drainages 9, 10 and 11 are within balance to the level of our measurement uncertainty, with mass budgets of –2.5±2.8 Gt a–1, –2.6±7.8 Gt a–1 and 0.9±2.3 Gt a–1, respectively. The region upstream of the Australian Lambert Glacier basin (LGB) traverse has a net mass budget of 4.4±6.3 Gt a–1, while the downstream region has –8.9±9.9 Gt a–1. These results indicate that glacier drainages 9, 10 and 11, upstream and downstream of the Australian LGB traverse, are in balance to within our measurement error.

The potential of grass field margin management for enhancing beetle diversity in intensive livestock farms

Summary Declining populations of UK grassland flora and fauna have been attributed to intensification of agricultural management practices, including changes in cutting, fertilizer, grazing and drainage regimes. We aimed to develop field margin management practices that could reverse declines in intensively managed grassland biodiversity that would have application in the UK and Europe. Here we focus on one aspect of grassland biodiversity, the beetles. In four intensively managed livestock farms in south‐west England, 10‐m wide field margins in existing grasslands were managed to create seven treatments of increasing sward architectural complexity. This was achieved through combinations of inorganic (NPK) fertilizer, cattle grazing, and timing and height of cutting. To examine the potential influence of complexity on faunal diversity, beetles were identified to species level from suction samples taken between 2003 and 2005, and their assemblage structure was related to margin management, floral assemblages and sward architecture. Beetle abundance, and species richness and evenness were influenced by margin management treatment and its interaction with year. Correlations with sward architecture and the percentage cover of dominant forbs and grasses were also found. Functional groups of the beetles showed different responses to the management treatments. In particular, higher proportional abundances of seed/flower‐feeding guilds were found in treatments not receiving NPK fertilizer. The assemblage structure was shown to respond to margin management treatments, sward architecture and the percentage cover of dominant forbs and grasses. The most extensively managed treatments were characterized by distinct successional trajectories from the control treatment. Synthesis and applications. This study provides management options suitable for use within agri‐environment schemes intended to improve faunal diversity associated with intensively managed lowland grasslands. Field margins receiving either no management or a single July silage cut were shown to support greater abundances and species richness of beetles, although subtler modifications of conventional management may also be beneficial, for example the absence of NPK fertilizer while maintaining grazing and silage cutting systems.

Effect of cosurfactant on the free-drainage regime of aqueous foams

We report results of drainage in aqueous foams of small bubble size D ( D = 180 μm ) prepared with SDS-dodecanol solutions. We have performed free-drainage experiments in which local drainage rates are measured by electrical conductivity and by light scattering techniques. We have investigated the role of the surfactant–cosurfactant mass ratio on the drainage regime. The results confirm that a drainage regime corresponding to a high surface mobility can indeed be found for such small bubbles, and show that an increase in the cosurfactant content can induce a transition to a low surface mobility drainage regime. We show that the transition is not linked to variations of the bulk properties, but rather to variations of the interfacial properties. However, the results show that the added amount of dodecanol to trigger the transition is quite high, evidencing that the relevant control parameter for drainage regimes includes both bubble size and interfacial contributions.

Maize Nitrogen Response as Affected by Soil Type and Drainage Variability

Site-specific application of nitrogen (N) to maize (Zea mays L.) may provide economic and environmental benefits. Variations in soil drainage and texture within fields are often believed to cause localized differences in soil N availability and therefore are a potential basis for site-specific N fertilizer application. The objective of this study was to evaluate the effect of imposed variations in drainage conditions in two soils on early season soil water conditions, soil nitrate levels, and crop response to N fertilizer. Maize was grown for three years following conversion from sod. Two soil drainage regimes and three N rates (22, 100 and 134 kg ha−1) were experimentally imposed on plots on two soil types, a clay loam and a loamy sand. Soil water potential and soil nitrate content were intensively monitored for the 0–150 and 150–300 mm soil layers during the early growing season. Early season soil water potentials showed small effects of drainage variability at the 75 and 225 mm depths. However, the clay loam soil experienced prolonged periods of saturation after significant precipitation, while the loamy sand never experienced such conditions. Soil nitrate levels were strongly affected by cropping history, but were also subjected to losses as a result of precipitation and short-term soil saturation. Maize N response was minimally affected by differences in soil drainage conditions in all 3 years. In years with a wet spring, justification exists for higher N fertilizer rates on finer-textured soils. This study therefore showed only moderate potential for varying N application within fields based on soil type and drainage conditions, but suggests that seasonal differences in N dynamics greatly affect maize N response.

Ice–water interactions during floods from Grænalón glacier-dammed lake, Iceland

AbstractThis paper explores changing ice–water interactions during jökulhlaups from Grænalón, a 5 × 108m3 subaerial lake dammed by Skeiðarárjökull, Iceland. Unstable drainage of Grænalón since the early 20th century has resulted in 45 jökulhlaups whose hydrologic character has varied enormously. Geomorphic observations and geophysical measurements from the inlet and outlet zones of the subglacial floodwater tract constrained the hydromechanical factors governing ice–water interactions at Grænalón. To date, three distinct drainage regimes have occurred in response to the changing surface elevation of Grænalón. Shifts from one drainage regime to another involved pronounced changes in jökulhlaup magnitude, timing and cyclicity. Present hydraulic conditions for lake drainage differ from the classical view of a pressure-coupled lake draining directly beneath an ice dam. Instead, low-amplitude drawdown occurs at regular, frequent intervals when hydrostatic pressure in a shallow, rock–ice trench enables water to flow beneath a sagging ice barrier. Floodwater exits Skeiðarárjökull in a supercooled state due to rapid hydraulic displacement from an overdeepened subglacial basin.

Liquid drainage through aqueous foam: study of the flow on the bubble scale

Macroscopic properties of foams are highly dependent on the liquid volume fraction, which has motivated many studies on foam drainage in the last decade. Theoretical developments and recent experimental results have suggested that two macroscopic drainage regimes could be expected, in relation with flow transitions occurring at the microscopic level, essentially in the Plateau border channels. We have constructed a setup, the Plateau border apparatus, to study the hydrodynamics of a single Plateau border channel, focusing on the surface properties of the foaming solution. Experimental results have shown that the actual theoretical models only partially predict the dissipation of liquid flow through a Plateau border channel. The major discrepancies can be explained considering additional dissipation processes related to the properties of the interface, and to the liquid flows induced in adjoining films as the liquid flows in the channel. Evidence of the hydrodynamic coupling between the channel and the adjoining films is given in the paper.

Quantitative description of foam drainage: transitions with surface mobility.

We have performed forced drainage experiments on aqueous foams of bubble diameters D varying from 0.18 to 8 mm, and made with different surfactant and protein solutions (providing different surface viscoelastic properties). Changing bubble size or surface properties allows to evolve between two drainage regimes, the respective dimensionless permeabilities also varying with these parameters. We show that the bubble size and surface properties can be incorporated into a single surface mobility parameter that controls the transition between the two drainage regimes. The permeability measurements indicate how do the hydrodynamic resistances of the foam channels and nodes depend on surface mobility. Taking advantage of the large range of experimental conditions, leading to a variation of the mobility parameter over more than 3 decades, a simple and consistent description of both the drainage regimes and the transition in between them is obtained. For the smallest bubbles (D < 0.5 mm) anomalous behaviors are observed and discussed.

Análise da equação de Swamee-Jain para cálculo do fator de atrito

Objetivou-se, com este trabalho, estudar o comportamento da equação de Swamee-Jain nas mais variadas situações de condução de água em sistemas pressurizados, para isto se desenvolveu um aplicativo computacional para realizar simulações variando o diâmetro interno do tubo, a velocidade de escoamento e a rugosidade absoluta das paredes da tubulação. A base de comparação do estudo se compunha das equações mais empregadas no cálculo do fator de atrito da equação universal de Darcy-Weissbach, respeitando-se seus respectivos regimes de escoamento e limitações. A partir de então, concluiu-se que, para o regime turbulento em conduto liso, a equação de Swamee-Jain apresentou diferenças de valores de f em relação às equações específicas requerendo, para melhor precisão, um fator de correção. Para os outros tipos de escoamento a concordância foi considerada satisfatória.

Thin-Film Hydrodynamics in Fluid Interface-Atomic Force Microscopy

Repulsive and attractive hydrodynamic interactions are measured between an oil droplet (n-hexadecane) and various glass microspheres in aqueous environments with an atomic force microscope (AFM). The magnitude and form of the hydrodynamics in a spherically wrapping thin film are investigated with a parametric study on external approach velocity and probe radius. The actual sphere−drop separation at closest approach can be experimentally deconvoluted in some situations from parametric data without ambiguity. Theoretical force profiles are calculated from the augmented Young−Laplace equation modified to allow for two distinct hydrodynamic drainage regimes: Reynolds lubrication for thick films with slightly deformed drops and a wrapping film condition for the indented interface. Also, an increase in film stability is directly observed as a function of velocity between a hydrophobized glass sphere and oil in pure water and in the presence of sodium dodecyl sulfate (SDS) below the critical micelle concentration (CMC).

Interpreting pH and nitrate concentration in solutions drained from acid soils. Possible artefacts of lysimeters

Abstract. Solutions collected from lysimeters of acid soils can show pH values close to or even above neutral. Laboratory experiments on an acid soil from Burundi were planned to test if denitrification or CO2 degassing might explain such a paradox. In the first experiment, soil profiles were reconstituted in columns and leached with 55 μm Ca(NO3)2 solutions at 30 °C and 4 °C. Two drainage regimes were applied: intermittent suction or no suction at the bottom of the columns. In the second experiment, pH values were measured in solutions drained from different horizons at 30 °C, before and after equilibration with ambient air. Sterilized soil was also tested in the same way. Results from experiment 1 showed that despite the accumulation of water in the bottom of soil profiles when no suction was applied, aeration still existed so that reduction reactions, namely denitrification, are not expected to affect greatly the percolate composition. Indeed nitrate concentration was similar in both drainage regimes and was close to the input value. The pH values in percolates were close to 7 at 30 °C and they dropped to about 5.5 when the columns were at 4 °C. In experiment 2, equilibration of percolates with ambient air resulted in pH increase which was greater for the top horizon (C‐rich) but negligible when the soil was first sterilized. These convergent results illustrate the very important effect of CO2 degassing on pH of drained solutions when microbial activity is stimulated at high temperatures, in C‐rich soil. This is of prime importance when interpreting results from lysimeter experiments. By chance, this study also showed that large quantities of nitrate can be produced in soil at low temperatures.

The Role of Gypsum in Production of Sulfate-Induced Deformation of Lime-Stabilized Soils

Gypsum is a major source of sulfate that produces sulfate-induced heave in lime-treated soils beneath roads and other paved structures. This deformation of pavement subgrade is known to result from the growth of the basic hydrous calcium aluminum sulfate mineral, ettringite, or a silica-bearing analog, thaumasite. The problem occurs in soils that have been treated with lime (CaO) for subgrade stabilization. Gypsum is a common sulfate mineral in sedimentary rocks and soils, and in north Texas it is present in soils developed on the montmorillonitic Eagle Ford Group shales (Upper Cretaceous). Because these soils are highly unstable the conventional treatment for road subgrade includes the addition of lime (CaO) or some other cementitious material such as fly ash or Portland cement. The pyrite-bearing Eagle Ford shale contains gypsum (CaSO4 • 2H2O) produced by reaction of calcium carbonate in the shale with acid sulfate from oxidation weathering of pyrite (FeS2). Sulfate movement upward in the soils can occur by capillarity, and it can be carried downward by infiltration, an often incomplete or interrupted event that leaves gypsum stranded as a soil evaporite. Once formed, the moderately soluble gypsum is retained in the clay-rich soils because of their low hydraulic conductivities, which makes them, in essence, reservoirs of gypsum. Experiments performed for this study confirm that gypsum in a lime-treated subgrade soil can supply sulfate for the growth of the expansive mineral ettringite. No sulfate external to the subgrade of the road is necessary for the reaction to occur. Gypsum is widely distributed in soils and surface outcrops in the western U.S. and should be the first mineral suspected where sulfate-induced heave has been diagnosed. Although gypsum is a moderately soluble mineral, it may be abundant in soils in regions with humid climates if its sulfate is derived from pyritic black shales by oxidation during soil formation. Eagle Ford soils do not produce sulfate-induced heave everywhere that road base has been lime-treated, but the problem is observed most frequently where roads follow streams, or run across low-lying areas or hillside slopes. Other studies have documented a correlation between deformation and major precipitation events. Ground water, soil water, and surface drainage regimes appear to control the specific sites at which severe deformation may take place within the stratigraphically-controlled belts of gypsum-bearing soils. Soluble sulfate tests currently in use to identify soils with the potential for sulfate-induced heave are known for inconsistent results. Total sulfate in a soil is a better predictor of the problem, and when gypsum is the sulfate mineral it can be determined quantitatively by existing laboratory methods. Stratigraphy is a first-order guide to where sulfate-induced heave may occur in the north Texas region, thus geologic maps of the Eagle Ford shale outcrop belt are also indicators of areas of possible sulfate-induced deformation.