Oxygen isotope enrichment (Δ18O) as a measure of time-averaged transpiration rate

By M. Sheshshayee, H. Bindumadhava, R. Ramesh, T. G. Prasad, M. Lakshminarayana, M. Udayakumar. 2005

97 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Plant Science, Soil Science

View Paper: https://www.semanticscholar.org/paper/8382d557e49a00d65a7ad5b201333ebdb33250c4

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. J. Morison
2. W. Davies
3. Jose Luis Araus
4. Margaret M. Barbour
5. Conxita Royo
6. N. R. Baker
7. P. Mullineaux

In Plant Science

1. Jose Luis Araus
2. G. Slafer
3. Conxita Royo
4. M. D. Serret
5. W. Davies
6. J. Morison
7. Margaret M. Barbour
8. N. R. Baker

In Soil Science

1. G. Slafer

Citations in the corpus

• Improving water use in crop production (2008, background): “B (2008) temperature and air humidity which affects the gradient in vapour pressure (De; Barbour & Farquhar 2000; Sheshshayee et al. 2005).”
• Breeding for Yield Potential and Stress Adaptation in Cereals (2008, background): “A recent study also found a relationship between δ 18 O and plant transpiration for groundnut and rice ( Sheshshayee et al. , 2005 ).”
• Stable oxygen isotope composition of plant tissue: a review. (2007, result): “For example, Sheshshayee et al. (2005) show that � 18Op is actually positively related to gs and transpiration rate in sunflower, cowpea, rice and groundnut, contrary to theoretical predictions.”