Marshall, John
- University of Idaho
Abstract
In many forests of the world, the summer season (temporal element) brings drought conditions causing low soil moisture in the upper soil profile (spatial element)-a potentially large barrier to seedling establishment. We evaluated the relationship between initial seedling root depth, temporal and spatial changes in soil moisture during drought after outplanting, and subsequent seedling performance using seedlings of Pinus ponderosa Laws. var. ponderosa grown in three containers similar in dimension except for depth (i. e. three stocktypes). Soil moisture patterns were quantified and growth, gas exchange, and carbon isotope analysis were used as metrics for stocktype evaluation. Soil moisture reached minimum volumetric soil moisture contents (theta) of 0.078 m(3) m(-3) at a 15 cm depth and 0.15 m(3) m(-3) at 90 cm by late summer, which also translated to estimated soil water potential (Psi(soil)) values of -2.29 and -0.02 MPa, respectively. Seedling photosynthesis (A) and transpiration (E) rates followed soil moisture trends, also reaching seasonal lows in late summer. In early fall, gas exchange rates nearly doubled following a replenishment of upper-profile soil moisture by precipitation. Over the course of the growing season, stocktypes did not differ in gas exchange rates (P >= 0.15), biomass (P >= 0.45), root penetration depth (P = 0.60), or carbon isotope signature (P >= 0.60). For all seedlings, current-year needles showed greater capacity for A than previous-year needles (P
Keywords
Ponderosa pine; Soil water potential; Container seedlings; Stocktype; Volumetric water content
Published in
New Forests
2016, volume: 47, number: 2, pages: 223-241
Publisher: SPRINGER
SLU Authors
UKÄ Subject classification
Forest Science
Publication identifier
- DOI: https://doi.org/10.1007/s11056-015-9511-7
Permanent link to this page (URI)
https://res.slu.se/id/publ/89104