Georgianne W. Moore

Saltcedar Water Use: Realistic and Unrealistic Expectations

Abstract Saltcedar (Tamarix spp.) is a widespread invasive plant found in riparian corridors and floodplains in 16 western states. In addition to being associated with such problems as increased soil salinity and decreased plant diversity, saltcedar has been reported to be a prolific water user. Popular press articles widely report that each individual saltcedar tree can use as much as 757 L (200 gallons) per day. Consequently massive control and removal efforts are underway to reduce transpirational water loss and increase water salvage for arid and semiarid environments. Although the potential economic benefits of these control efforts are touted, it has not been proven whether such water savings are possible on a stream level. The original citation for the 757-L estimate does not list the experimental design or techniques used to arrive at this value. We use three lines of evidence—peer-reviewed scientific literature, sap flux rates and sap wood area, and potential evaporation rates—to demonstrate the improbability that saltcedar, or any other woody species, can use this much water per tree on a daily basis. A more realistic estimate of maximum tree-level daily water use derived from sap flux measurements would be < 122 L · d−1 (32.2 gallons). Estimates of water salvage would be grossly overestimated using the popular water use value (757 L · d−1), and economic benefits from saltcedar control based solely on water salvage are questionable.

Thermal-dissipation sap flow sensors may not yield consistent sap-flux estimates over multiple years

Sap flow techniques, such as thermal dissipation, involve an empirically derived relationship between sap flux and the temperature differential between a heated thermocouple and a nearby reference thermocouple inserted into the sapwood. This relationship has been widely tested but mostly with newly installed sensors. Increasingly, sensors are used for extended periods. After several months, tree growth, wounding, or other changes in water flow path may impair sensor performance. To quantify changes in sensor performance over time, we installed 23 sensors (one per tree) in 16-year-old Douglas-fir [Pseudotsuga menziesii (Mirb.) Franco] and red alder (Alnus rubra Bong.) in the western Cascades of Oregon and measured daily average sap flux (Js) from April through July 2001 and 2002. We assumed the measurements from 2001 to be unimpaired and the response of Js to vapor pressure deficit (δ) to be consistent under the same edaphic conditions. Differences from this assumption were attributed to “temporal sampling errors.” During the study, soil moisture (θ), did not differ on similar calendar dates, yet the slope of Js versus δ decreased significantly in the second year. In 2002, Js in Douglas-fir was 45% less than in 2001; in red alder, 30% less. Variations in δ could not explain the differences. A correction for temporal sampling errors improved estimates of Js from sensors used for more than one season. Differences in temporal sampling errors between the two species reveal underlying causal mechanisms. Evidence is presented that cambial growth causes errors in Douglas-fir.

Tree mortality from an exceptional drought spanning mesic to semiarid ecoregions.

Significant areas of the southern USA periodically experience intense drought that can lead to episodic tree mortality events. Because drought tolerance varies among species and size of trees, such events can alter the structure and function of terrestrial ecosystem in ways that are difficult to detect with local data sets or solely with remote-sensing platforms. We investigated a widespread tree mortality event that resulted from the worst 1-year drought on record for the state of Texas, USA. The drought affected ecoregions spanning mesic to semiarid climate zones and provided a unique opportunity to test hypotheses related to how trees of varying genus and size were affected. The study was based on an extensive set of 599 distributed plots, each 0.16 ha, surveyed in the summer following the drought. In each plot, dead trees larger than 12.7 cm in diameter were counted, sized, and identified to the genus level. Estimates of total mortality were obtained for each of 10 regions using a combination of design-based estimators and calibrated remote sensing using MODIS 1-yr change in normalized difference vegetation index products developed by the U.S. Forest Service. As compared with most of the publicized extreme die-off events, this study documents relatively low rates of mortality occurring over a very large area. However, statewide, regional tree mortality was massive, with an estimated 6.2% of the live trees perishing, nearly nine times greater than normal annual mortality. Dead tree diameters averaged larger than the live trees for most ecoregions, and this trend was most pronounced in the wetter climate zones, suggesting a potential re-ordering of species dominance and downward trend in tree size that was specific to climatic regions. The net effect on carbon storage was estimated to be a redistribution of 24-30 Tg C from the live tree to dead tree carbon pool. The dead tree survey documented drought mortality in more than 29 genera across all regions, and surprisingly, drought resistant and sensitive species fared similarly in some regions. Both angiosperms and gymnosperms were affected. These results highlight that drought-driven mortality alters forest structure differently across climatic regions and genera.

Does Shrub Removal Increase Groundwater Recharge in Southwestern Texas Semiarid Rangelands

Abstract Evapotranspiration (ET) is a key component limiting groundwater recharge past the root zone in semiarid regions. Vegetation management may alter groundwater recharge if ET is altered due to changes in vegetation type or cover. This study quantifies changes in groundwater recharge following vegetation cover change from native woodland to pasture in a semiarid region of southwest Texas. The Carrizo–Wilcox aquifer is a valuable groundwater resource in this area, where overuse by dependent farming practices has lowered aquifer levels significantly in the last 85 yr. Combining data from short-term (30 mo) monitoring of the changes in soil moisture and long-term (5–30 yr) changes in total soil chloride indicated deep drainage increased slightly where land had been cleared of vegetation. Annual recharge rates below rooting depths (standardized to 155 cm) averaged only 0.72 ± 0.2 mm · yr−1 (mean ± SE) in areas not cleared of woody vegetation, as estimated by chloride mass balance. Upon clearing, 72% of the total chloride naturally occurring in the soil profile was flushed away within 30 yr, leading to an estimated 2.59 ± 1.7 mm · yr−1 additional recharge. Deep soil moisture in recently cleared land increased by up to 17% during the growing season of wet years (double the average rainfall) but did not increase in dry or normal precipitation years, providing supporting evidence that more water penetrated below the roots under certain environmental conditions. These results demonstrate that brush management can increase recharge by modest, but measurable, amounts depending on site-specific soil characteristics and degree of reduction in vegetation.

Ecophysiological Responses of Giant Reed (Arundo donax) to Herbivory

Abstract The effect of invasive species might be lessened if herbivores reduced transpiration and growth rates; however, simply removing photosynthetic material might not ensure that the transpiration rate of active leaf tissue decreases. We assessed whether biological control has an injurious effect on the target plant species, giant reed (Arundo donax), by quantifying leaf photosynthetic and transpiration responses to two herbivores: an armored scale, Rhizaspidiotus donacis, and a stem-galling wasp, Tetramesa romana. Herbivory by a sap-feeding scale and a stem-galling wasp both separately and together, reduces the rates of leaf level physiological processes in A. donax. The effect of the wasp increases with density and reduces photosynthesis by reducing the carboxylation rate of ribulose-1,5-bisphosphate carboxylase oxygenase, which controls CO2 fixation in photosynthesis. The scale insect reduces photosynthesis by decreasing the maximum rate of electron transport, which determines how much light energy can be captured in photosynthesis. The effect of the armored scale takes approximately 5 mo after infestation, which coincides with generation time. When both insects are present at the same time, the effect of their herbivory appears additive after time for the scale to reproduce. We conclude that a combination of two herbivores can have a stronger physiological effect than one type of herbivore, likely because of their different effects on leaf function. Nomenclature: Arundo scale, Rhizaspidiotus donacis Leonardi; Arundo wasp, Tetramesa romana Walker; Giant reed, Arundo donax L

Leaf surface traits and water storage retention affect photosynthetic responses to leaf surface wetness among wet tropical forest and semiarid savanna plants

While it is reasonable to predict that photosynthetic rates are inhibited while leaves are wet, leaf gas exchange measurements during wet conditions are challenging to obtain due to equipment limitations and the complexity of canopy-atmosphere interactions in forested environments. Thus, the objective of this study was to evaluate responses of seven tropical and three semiarid savanna plant species to simulated leaf wetness and test the hypotheses that (i) leaf wetness reduces photosynthetic rates (Anet), (ii) leaf traits explain different responses among species and (iii) leaves from wet environments are better adapted for wet leaf conditions than those from drier environments. The two sites were a tropical rainforest in northern Costa Rica with ~4200 mm annual rainfall and a savanna in central Texas with ~1100 mm. Gas exchange measurements were collected under dry and wet conditions on five sun-exposed leaf replicates from each species. Additional measurements included leaf wetness duration and stomatal density. We found that Anet responses varied greatly among species, but all plants maintained a baseline of activity under wet leaf conditions, suggesting that abaxial leaf Anet was a significant percentage of total leaf Anet for amphistomatous species. Among tropical species, Anet responses immediately after wetting ranged from -31% (Senna alata (L.) Roxb.) to +21% (Zamia skinneri Warsz. Ex. A. Dietr.), while all savanna species declined (up to -48%). After 10 min of drying, most species recovered Anet towards the observed status prior to wetting or surpassed it, with the exception of Quercus stellata Wangenh., a savanna species, which remained 13% below Anet dry. The combination of leaf wetness duration and leaf traits, such as stomatal density, trichomes or wax, most likely influenced Anet responses positively or negatively. There was also overlap between leaf traits and Anet responses of savanna and tropical plants. It is possible that these species converge on a relatively conservative response to wetness, each for divergent purposes (cooling, avoiding stomatal occlusion, or by several unique means of rapid drying). A better understanding of leaf wetness inhibiting photosynthesis is vital for accurate modeling of growth in forested environments; however, species adapted for wet environments may possess compensatory traits that mitigate these effects.

Removing Adult Overstory Trees Stimulates Growth and Transpiration of Conspecific Juvenile Trees

Abstract During the last century, the density of Ashe juniper (Juniperus ashei Buchholz) has greatly increased in oak savannahs of central Texas. Recently, juniper removal has been advocated as a regional water conservation tool. In this study, we investigated whether juvenile trees released from an overstory canopy after clearing exhibited accelerated growth and water consumption. We compared leaf-level transpiration (El) and carbon assimilation (Anet) rates among juvenile juniper under three different treatment scenarios: 1) in the open, 2) under an adult juniper canopy or 3) recently released by the removal of an adult juniper canopy. Released plants apparently grew faster and used more water than other juvenile trees; average Anet of released plants was 94%–162% greater (P < 0.05) than those beneath an adult canopy and 22%–44% greater than open-grown plants. Furthermore, average El of released plants was 22%–72% greater than those beneath an adult canopy and 13%–22% greater than open-grown plants. These differences persisted for at least two years after treatment. Rates of Anet were particularly elevated in released plants compared to other plants during periods of low water stress; whereas El tended to be higher in released plants compared to other plants at all levels of water availability. Our evidence suggests released plants have better access to water, because at two out of three study sites, predawn leaf water potential (Ψp) was significantly more favorable for released plants than open-grown or under-canopy plants (P < 0.05). Although adult canopy removal temporarily reduced leaf area of juniper on a community level, and likely total water use, we demonstrated that released juveniles, at a minimum, partially compensated for the reduced overstory by increasing rates of water use and growth.

Tamarix transpiration along a semiarid river has negligible impact on water resources

The proliferation of saltcedar (Tamarix spp.) along regulated rivers in the western United States has transformed riparian plant communities. It is commonly assumed that transpiration by these alien plants has led to large losses of water that would otherwise contribute to streamflow. Control of saltcedar, therefore, has been considered a viable strategy for conserving water and increasing streamflow in these regions. In an effort to better understand the linkage between transpiration by saltcedar and streamflow, we monitored transpiration, stream stage, and groundwater elevations within a saltcedar stand along the Pecos River during June 2004. Transpiration, as determined by sap flow measurements, exhibited a strong diel pattern; stream stage did not. Diel fluctuations in groundwater levels were observed, but only in one well, which was located in the center of the saltcedar stand. In that well, the correlation between maximal transpiration and minimal groundwater elevation was weak (R2 = 0.16). No effects of transpiration were detected in other wells within the saltcedar stand, nor in the stream stage. The primary reason, we believe, is that the saltcedar stand along this reach of the Pecos River has relatively low sapwood area and a limited spatial extent resulting in very low transpiration compared with the stream discharge. Our results are important because they provide a mechanistic explanation for the lack of increase in streamflow following large-scale control of invasive trees along semiarid rivers.

Upscaling transpiration in diverse forests: Insights from a tropical premontane site

Department of Ecosystem Science and Management, Texas A&M University, 2138 TAMU, College Station, TX 77843, USA 2 INVISTA S.à r.l., 5060 FM 1006, Orange, TX 77630, USA Department of Civil Engineering, Texas A&M University, 3136 TAMU, College Station, TX 77843‐3136, USA Correspondence Georgianne W. Moore, Department of Ecosystem Science and Management, Texas A&M University, 2138 TAMU, College Station, TX 77843, USA. Email: gwmoore@tamu.edu Funding information Soltis and Hammer families; U.S. Department of Energy, Office of Science, Biological and Environmental Research, Grant/Award Number: DE‐SC0010654; National Science Foundation, Grant/Award Number: EAR‐1004874

Transpiration in recovering mixed loblolly pine and oak stands following wildfire in the Lost Pines region of Texas: Post-fire transpiration of mixed pine and oak stands

Department of Soil and Crop Sciences, Texas A&M University, College Station, Texas Department of Ecosystem Science and Management, Texas A&M University, College Station, Texas Department of Soil and Crop Sciences, Texas A&M AgriLife Research, Stephenville, Texas Correspondence Caitlyn E. Cooper, Department of Soil and Crop Sciences, Texas A&M University, 2474 TAMU, College Station, TX 77843. Email: caitlyn.cooper@ag.tamu.edu Present Address Department of Ecosystem Science and Management, Texas A&M AgriLife Research, Vernon, Texas