Descriptions of Nymphs of \u3ci\u3eItzalana Submaculata\u3c/i\u3e Schmidt (Homoptera: Fulgoridae), a Species New to the United States

The 3rd, 4th, and 5th instar nymphs of ltzalana submaculata Schmidt are described from southern Texas. Previously recorded only from Surinam, this is the first record of this fulgorid from the United States and Mexico

Blood lactate clearance after maximal exercise depends on active recovery intensity

AIM: High-intensity exercise is time-limited by onset of fatigue, marked by accumulation of blood lactate. This is accentuated at maximal, all-out exercise that rapidly accumulates high blood lactate. The optimal active recovery intensity for clearing lactate after such maximal, all-out exercise remains unknown. Thus, we studied the intensity-dependence of lactate clearance during active recovery after maximal exercise.<p></p> METHODS: We constructed a standardized maximal, all-out treadmill exercise protocol that predictably lead to voluntary exhaustion and blood lactate concentration >10 mM. Next, subjects ran series of all-out bouts that increased blood lactate concentration to 11.5±0.2 mM, followed by recovery exercises ranging 0% (passive)-100% of the lactate threshold.<p></p> RESULTS: Repeated measurements showed faster lactate clearance during active versus passive recovery (P<0.01), and that active recovery at 60-100% of lactate threshold was more efficient for lactate clearance than lower intensity recovery (P<0.05). Active recovery at 80% of lactate threshold had the highest rate of and shortest time constant for lactate clearance (P<0.05), whereas the response during the other intensities was graded (100%=60%>40%>passive recovery, P<0.05).<p></p> CONCLUSION: Active recovery after maximal all-out exercise clears accumulated blood lactate faster than passive recovery in an intensity-dependent manner, with maximum clearance occurring at active recovery of 80% of lactate threshold

Patent Institutions: Shifting Interactions Between Legal Actors

This contribution to the Research Handbook on Economics of Intellectual Property Rights (Vol. 1 Theory) addresses interactions between the principal legal institutions of the U.S. patent system. It considers legal, strategic, and normative perspectives on these interactions as they have evolved over the last 35 years. Early centralization of power by the U.S. Court of Appeals for the Federal Circuit, newly created in 1982, established a regime dominated by the appellate court\u27s bright-line rules. More recently, aggressive Supreme Court and Congressional intervention have respectively reinvigorated patent law standards and led to significant devolution of power to inferior tribunals, including newly created tribunals like the USPTO\u27s Patent Trial and Appeals Board. This new era in institutional interaction creates a host of fresh empirical and normative research questions for scholars. The contribution concludes by outlining a research agenda

Water Resources of the Dakota Aquifer in Kansas

The Dakota aquifer system underlies most of the western two-thirds of Kansas and includes sandstone units in the Cretaceous Dakota, Kiowa, and Cheyenne Sandstone formations. The underlying Jurassic Morrison Formation in southwest Kansas is also considered by state statute to be part of the Dakota system. The Dakota aquifer has been developed as a water-supply source where the groundwater is fresh or only slightly saline and where other more easily obtained water supplies are not available. A total of 2,237 wells with active water rights and active uses made of water as of the end of 2011 were determined to produce greater than 5% of their total yield from the Dakota aquifer. Most of these wells are located where the Dakota aquifer underlies the High Plains aquifer (HPA) in southwest Kansas. In the 36 counties in which water-right-permitted wells pump partially or solely from the Dakota aquifer, the wells with Dakota yield are estimated to comprise 9% of the total of wells with water-right permits in all aquifers. Most (78%) of the water-right-permitted wells that draw part or all of their water from the Dakota aquifer are used for irrigation. Stock, municipal, and industrial wells comprise nearly all of the other uses (9.6%, 8.9%, and 2.2%, respectively, of the wells with some Dakota yield). The mean annual volume of water used from the Dakota aquifer by water-right-permitted wells in Kansas is estimated to have been 117,000 acre-ft/yr (1.44 x 108 m3/yr) from 2006 to 2010. The use was greatest in southwest Kansas (approximately 86% of the total Dakota use). The mean annual use for other regions ranged from approximately 0.5% of the total Dakota use for west-central Kansas, to 2.4% for central, 2.9% for south-central, and 8.1% for north-central Kansas. Although Dakota water use in north-central Kansas was much lower than in southwest Kansas, the percent Dakota use relative to total use from all aquifers was the highest (nearly 20%) of all the regions. The percent Dakota use compared to total use from all aquifers for the other regions is 5.2% for southwest, 2.5% for central, 2.0% for south-central, and 0.4% for west-central Kansas. About 90% of the mean annual use from the Dakota aquifer during 2006-2010 was for irrigation, most of which was in southwest Kansas. For stock and municipal purposes, water usage was nearly 4% each of the total volume pumped from the Dakota aquifer. However, municipal demands accounted for 41% and 18% of the total use from the Dakota in central and north-central Kansas, respectively. The total number of "domestic" wells, defined as those for which water-right permits are not required, that currently produce most or all of their water from the Dakota aquifer in Kansas is estimated to be more than 11,000 (about 8,000 for north-central and central Kansas and nearly 3,200 for south-central, west-central, and southwest Kansas). Water use from the Dakota aquifer by "domestic" wells is estimated to be 4,800 acre-ft/yr (5.9 x 106 m3/yr) in central Kansas, 1,500 acre-ft/yr (1.9 x 106 m3/yr) in north-central Kansas, and a total of 1,700 acre-ft/yr (2.1 x 106 m3/yr) in south-central, west-central, and southwest Kansas. The total "domestic" well use (about 8,000 acre-ft/yr) is about 6.4% of the approximately 125,000 acre-ft/yr (1.54 x 108 m3/yr) pumped from the Dakota aquifer by both permitted and "domestic" wells in Kansas. The processes of mixing, reactive cation exchange, and mineral dissolution and precipitation have produced a complex range of chemical characteristics for groundwater in the Dakota aquifer. Water quality in the aquifer ranges from very fresh (<300 mg/L total dissolved solids [TDS]) to saltwater (>10,000 mg/L TDS). Freshwaters in the outcrop and subcrop portions of the Dakota aquifer in north-central and central Kansas are usually calcium-bicarbonate type waters. Calcium-sulfate type water in some regions can result from one of two processes: (1) weathering of pyrite in shales in Dakota strata and concomitant dissolution of calcite or dolomite and (2) recharge from upper Cretaceous strata that was affected by the same processes or by dissolution of gypsum. Large areas of the Dakota aquifer contain saline water (sodium-chloride type water) that was derived from the upward intrusion of saltwater from underlying Permian units, especially the Cedar Hills Sandstone in central and north-central Kansas. The saltwater is derived from the dissolution of evaporite deposits containing rock salt (halite) in the Permian. The salinity of groundwater in the Dakota aquifer generally increases with depth, particularly across substantial shale units of appreciable lateral extent that confine or separate aquifer units. Sodium-bicarbonate type water, which exists in parts of the confined Dakota aquifer in central and west-central Kansas, is generated by the flushing of saline water from the aquifer by groundwater recharge of calcium-bicarbonate or calcium-sulfate types. During this process, calcium (and magnesium) in the freshwater is exchanged for sodium on clays in Dakota strata. Fluoride concentrations increase in the sodium-bicarbonate water as a result of dissolution of calcium-containing fluoride minerals during the decrease in calcium in the groundwater caused by the exchange process. Fluoride concentrations exceed the maximum contaminant level (MCL) of 4 mg/L for public drinking water supply in some areas of the confined Dakota aquifer. About 10% of the sample records for the Dakota aquifer exceed the MCL for arsenic and the action level for lead, although some of the high lead values could be related to lead in plumbing systems. Uranium concentration and the radioactivity from radium isotopes and alpha particles exceed the MCL for public drinking waters in a small percentage of Dakota groundwaters. Many other natural constituents and properties in Dakota waters exceed recommended or suggested levels for drinking water, such as TDS, chloride, sulfate, iron, manganese, and ammonium ion concentrations, especially in saline water in the confined aquifer and in groundwaters that have chemically reducing conditions. The main contaminant from anthropogenic activities in Dakota groundwater is nitrate. Nitrate-nitrogen concentrations exceeding the MCL of 10 mg/L primarily occur in shallow wells in the unconfined aquifer in central and north-central Kansas. The expected sources are animal and human waste and fertilizer that enter groundwaters by shallow recharge or through the annular space of poorly constructed wells. Development of the Dakota aquifer has been dependent on both the hydrogeologic properties of the aquifer and the salinity of the groundwater. The Kansas Geological Survey has identified an area of nearly fresh to slightly saline waters in upper Dakota strata that could be important for future water supplies. The area is triangular in shape, with its base along the south lines of Sheridan and Graham counties and its northern extent into south-central Norton County. Another factor in aquifer development is the decline in the water table in the HPA where it overlies and is hydraulically connected to the Dakota aquifer in southwest Kansas. Many new wells have been completed in both the HPA and underlying Dakota strata. In cases in which the new construction is a replacement well, the previous well was often only completed in the HPA. Thus, the percentage of wells completed in both aquifers is increasing. Continued assessment of the water resources potential of the Dakota aquifer is especially needed in southwest Kansas but is difficult due to the very limited data for depth-to-water measurements in the Dakota in that area. A selected group of wells across the Dakota in southwestern Kansas should be equipped with continuous monitoring equipment so that a better understanding of the relationship between the Dakota and the overlying HPA can be obtained

The Coherent Radio Emission from the RS CVn Binary HR 1099

We used the Australia Telescope in March-April 2005 to observe the RS CVn binary HR 1099 at 1.384 and 2.368 GHz at two epochs, each of 9 h in duration and 11 days apart. During two episodes of coherent emission, we employed a recently installed facility to sample the data at 78 ms intervals to measure the fine temporal and spectral structure of HR 1099. Our main observational results include: ~100% left hand circularly polarised emission was seen at both 1.384 and 2.368 GHz during both epochs; in the first event the emission feature drifted across the spectrum; three 22 min integrations made at 78 ms time resolution showed that the modulation index of the Stokes V parameter increased monotonically as the integration time was decreased and was still increasing at our resolution limit; we believe that the highly polarised emission is due to electron-cyclotron maser emission (ECME) operating in the corona of one of the binary components. We discuss two kinds of maser sources that may be responsible for driving the observed events. We suggest that the ECME source may be an aurora-like phenomenon due to the transfer of plasma from the K2 subgiant to the G5 dwarf in a strong stellar wind.Comment: Accepted for publication in the Publications of the Astronomical Society of Australi

Water Resources of the Dakota Aquifer in Kansas

The Dakota aquifer system underlies most of the western two-thirds of Kansas and includes sandstone units in the Cretaceous Dakota, Kiowa, and Cheyenne Sandstone formations. The underlying Jurassic Morrison Formation in southwest Kansas is also considered by state statute to be part of the Dakota system. The Dakota aquifer has been developed as a water-supply source where the groundwater is fresh or only slightly saline and where other more easily obtained water supplies are not available. A total of 2,237 wells with active water rights and active uses made of water as of the end of 2011 were determined to produce greater than 5% of their total yield from the Dakota aquifer. Most of these wells are located where the Dakota aquifer underlies the High Plains aquifer (HPA) in southwest Kansas. In the 36 counties in which water-right-permitted wells pump partially or solely from the Dakota aquifer, the wells with Dakota yield are estimated to comprise 9% of the total of wells with water-right permits in all aquifers. Most (78%) of the water-right-permitted wells that draw part or all of their water from the Dakota aquifer are used for irrigation. Stock, municipal, and industrial wells comprise nearly all of the other uses (9.6%, 8.9%, and 2.2%, respectively, of the wells with some Dakota yield). The mean annual volume of water used from the Dakota aquifer by water-right-permitted wells in Kansas is estimated to have been 117,000 acre-ft/yr (1.44 x 108 m3/yr) from 2006 to 2010. The use was greatest in southwest Kansas (approximately 86% of the total Dakota use). The mean annual use for other regions ranged from approximately 0.5% of the total Dakota use for west-central Kansas, to 2.4% for central, 2.9% for south-central, and 8.1% for north-central Kansas. Although Dakota water use in north-central Kansas was much lower than in southwest Kansas, the percent Dakota use relative to total use from all aquifers was the highest (nearly 20%) of all the regions. The percent Dakota use compared to total use from all aquifers for the other regions is 5.2% for southwest, 2.5% for central, 2.0% for south-central, and 0.4% for west-central Kansas. About 90% of the mean annual use from the Dakota aquifer during 2006-2010 was for irrigation, most of which was in southwest Kansas. For stock and municipal purposes, water usage was nearly 4% each of the total volume pumped from the Dakota aquifer. However, municipal demands accounted for 41% and 18% of the total use from the Dakota in central and north-central Kansas, respectively. The total number of "domestic" wells, defined as those for which water-right permits are not required, that currently produce most or all of their water from the Dakota aquifer in Kansas is estimated to be more than 11,000 (about 8,000 for north-central and central Kansas and nearly 3,200 for south-central, west-central, and southwest Kansas). Water use from the Dakota aquifer by "domestic" wells is estimated to be 4,800 acre-ft/yr (5.9 x 106 m3/yr) in central Kansas, 1,500 acre-ft/yr (1.9 x 106 m3/yr) in north-central Kansas, and a total of 1,700 acre-ft/yr (2.1 x 106 m3/yr) in south-central, west-central, and southwest Kansas. The total "domestic" well use (about 8,000 acre-ft/yr) is about 6.4% of the approximately 125,000 acre-ft/yr (1.54 x 108 m3/yr) pumped from the Dakota aquifer by both permitted and "domestic" wells in Kansas. The processes of mixing, reactive cation exchange, and mineral dissolution and precipitation have produced a complex range of chemical characteristics for groundwater in the Dakota aquifer. Water quality in the aquifer ranges from very fresh (<300 mg/L total dissolved solids [TDS]) to saltwater (>10,000 mg/L TDS). Freshwaters in the outcrop and subcrop portions of the Dakota aquifer in north-central and central Kansas are usually calcium-bicarbonate type waters. Calcium-sulfate type water in some regions can result from one of two processes: (1) weathering of pyrite in shales in Dakota strata and concomitant dissolution of calcite or dolomite and (2) recharge from upper Cretaceous strata that was affected by the same processes or by dissolution of gypsum. Large areas of the Dakota aquifer contain saline water (sodium-chloride type water) that was derived from the upward intrusion of saltwater from underlying Permian units, especially the Cedar Hills Sandstone in central and north-central Kansas. The saltwater is derived from the dissolution of evaporite deposits containing rock salt (halite) in the Permian. The salinity of groundwater in the Dakota aquifer generally increases with depth, particularly across substantial shale units of appreciable lateral extent that confine or separate aquifer units. Sodium-bicarbonate type water, which exists in parts of the confined Dakota aquifer in central and west-central Kansas, is generated by the flushing of saline water from the aquifer by groundwater recharge of calcium-bicarbonate or calcium-sulfate types. During this process, calcium (and magnesium) in the freshwater is exchanged for sodium on clays in Dakota strata. Fluoride concentrations increase in the sodium-bicarbonate water as a result of dissolution of calcium-containing fluoride minerals during the decrease in calcium in the groundwater caused by the exchange process. Fluoride concentrations exceed the maximum contaminant level (MCL) of 4 mg/L for public drinking water supply in some areas of the confined Dakota aquifer. About 10% of the sample records for the Dakota aquifer exceed the MCL for arsenic and the action level for lead, although some of the high lead values could be related to lead in plumbing systems. Uranium concentration and the radioactivity from radium isotopes and alpha particles exceed the MCL for public drinking waters in a small percentage of Dakota groundwaters. Many other natural constituents and properties in Dakota waters exceed recommended or suggested levels for drinking water, such as TDS, chloride, sulfate, iron, manganese, and ammonium ion concentrations, especially in saline water in the confined aquifer and in groundwaters that have chemically reducing conditions. The main contaminant from anthropogenic activities in Dakota groundwater is nitrate. Nitrate-nitrogen concentrations exceeding the MCL of 10 mg/L primarily occur in shallow wells in the unconfined aquifer in central and north-central Kansas. The expected sources are animal and human waste and fertilizer that enter groundwaters by shallow recharge or through the annular space of poorly constructed wells. Development of the Dakota aquifer has been dependent on both the hydrogeologic properties of the aquifer and the salinity of the groundwater. The Kansas Geological Survey has identified an area of nearly fresh to slightly saline waters in upper Dakota strata that could be important for future water supplies. The area is triangular in shape, with its base along the south lines of Sheridan and Graham counties and its northern extent into south-central Norton County. Another factor in aquifer development is the decline in the water table in the HPA where it overlies and is hydraulically connected to the Dakota aquifer in southwest Kansas. Many new wells have been completed in both the HPA and underlying Dakota strata. In cases in which the new construction is a replacement well, the previous well was often only completed in the HPA. Thus, the percentage of wells completed in both aquifers is increasing. Continued assessment of the water resources potential of the Dakota aquifer is especially needed in southwest Kansas but is difficult due to the very limited data for depth-to-water measurements in the Dakota in that area. A selected group of wells across the Dakota in southwestern Kansas should be equipped with continuous monitoring equipment so that a better understanding of the relationship between the Dakota and the overlying HPA can be obtained