Singer Michael Bliss, Sargeant Christopher I, Piégay Hervé, Riquier Jérémie, Wilson Rob J S, Evans Cristina M
Department of Earth and Environmental Sciences, University of St Andrews St Andrews, UK ; Earth Research Institute, University of California Santa Barbara Santa Barbara, California, USA,.
Department of Earth and Environmental Sciences, University of St Andrews St Andrews, UK.
Water Resour Res. 2014 May;50(5):4490-4513. doi: 10.1002/2014WR015581. Epub 2014 May 29.
Seasonal and annual partitioning of water within river floodplains has important implications for ecohydrologic links between the water cycle and tree growth. Climatic and hydrologic shifts alter water distribution between floodplain storage reservoirs (e.g., vadose, phreatic), affecting water availability to tree roots. Water partitioning is also dependent on the physical conditions that control tree rooting depth (e.g., gravel layers that impede root growth), the sources of contributing water, the rate of water drainage, and water residence times within particular storage reservoirs. We employ instrumental climate records alongside oxygen isotopes within tree rings and regional source waters, as well as topographic data and soil depth measurements, to infer the water sources used over several decades by two co-occurring tree species within a riparian floodplain along the Rhône River in France. We find that water partitioning to riparian trees is influenced by annual (wet versus dry years) and seasonal (spring snowmelt versus spring rainfall) fluctuations in climate. This influence depends strongly on local (tree level) conditions including floodplain surface elevation and subsurface gravel layer elevation. The latter represents the upper limit of the phreatic zone and therefore controls access to shallow groundwater. The difference between them, the thickness of the vadose zone, controls total soil moisture retention capacity. These factors thus modulate the climatic influence on tree ring isotopes. Additionally, we identified growth signatures and tree ring isotope changes associated with recent restoration of minimum streamflows in the Rhône, which made new phreatic water sources available to some trees in otherwise dry years.
Water shifts due to climatic fluctuations between floodplain storage reservoirsAnthropogenic changes to hydrology directly impact water available to treesEcohydrologic approaches to integration of hydrology afford new possibilities.
河漫滩内水的季节性和年度分配对水循环与树木生长之间的生态水文联系具有重要意义。气候和水文变化改变了河漫滩蓄水层(如包气带、潜水层)之间的水分分布,影响树木根系可获取的水量。水分分配还取决于控制树木根系深度的物理条件(如阻碍根系生长的砾石层)、供水水源、排水速率以及特定蓄水层内的水停留时间。我们利用仪器记录的气候数据、树木年轮和区域水源中的氧同位素,以及地形数据和土壤深度测量数据,来推断法国罗纳河沿岸河漫滩中两种共生树种在几十年间所利用的水源。我们发现,河漫滩树木的水分分配受气候的年度(湿润年份与干旱年份)和季节性(春季融雪与春季降雨)波动影响。这种影响很大程度上取决于当地(树木层面)的条件,包括河漫滩地表高程和地下砾石层高程。后者代表潜水层的上限,因此控制着浅层地下水的获取。它们之间的差异,即包气带的厚度,控制着土壤的总持水能力。这些因素因此调节了气候对树木年轮同位素的影响。此外,我们还确定了与罗纳河近期恢复最低流量相关的生长特征和树木年轮同位素变化,这使得一些树木在原本干旱的年份能够获取新的潜水水源。
气候波动导致河漫滩蓄水层之间的水分转移;水文的人为变化直接影响树木可获取的水量;生态水文方法为水文整合提供了新的可能性。