From c6e325985a9f27f8edd3286d716ee4d473f3c696 Mon Sep 17 00:00:00 2001 From: rmshkv Date: Thu, 27 Jun 2024 23:41:06 -0600 Subject: [PATCH] Fixing one more link --- notebooks/ocn-phyto-lims.ipynb | 2 +- 1 file changed, 1 insertion(+), 1 deletion(-) diff --git a/notebooks/ocn-phyto-lims.ipynb b/notebooks/ocn-phyto-lims.ipynb index 358b010..5344797 100644 --- a/notebooks/ocn-phyto-lims.ipynb +++ b/notebooks/ocn-phyto-lims.ipynb @@ -315,7 +315,7 @@ "metadata": {}, "source": [ "## Mapping nutrient limitation at the surface\n", - "Phytoplankton need a specific ratio of nutrients to grow and produce organic matter. In general, this is known as the Redfield ratio, first proposed by [Redfield et al., 1963](https://books.google.com/books?id=LeMvduUHtxQC&pg=PA26&source=gbs_toc_r&cad=1#v=onepage&q&f=false), and is approximately 106 C:16 N:1 P. Micronutrients like silicate and iron are also needed in more variable amounts depending on plankton type. To learn more about nutrient limitation, see [Sarmiento and Gruber Chapter 4: Organic Matter Production](https://doi.org/10.2307/j.ctt3fgxqx.7).\n", + "Phytoplankton need a specific ratio of nutrients to grow and produce organic matter. In general, this is known as the Redfield ratio, first proposed by [Redfield et al., 1963](https://books.google.com/books?id=LeMvduUHtxQC&pg=PA26&source=gbs_toc_r&cad=1), and is approximately 106 C:16 N:1 P. Micronutrients like silicate and iron are also needed in more variable amounts depending on plankton type. To learn more about nutrient limitation, see [Sarmiento and Gruber Chapter 4: Organic Matter Production](https://doi.org/10.2307/j.ctt3fgxqx.7).\n", "Our dataset uses a numerical notation to specify which nutrient is limiting in each area for each phytoplankton functional type, as specified below:\n", "- 0 = PO4\n", "- 1 = Fe\n",