title: The impact of immigration on international trade: a meta‐analysis

authors: Genc, Murat

subjects: international trade

abstract: Since the early 1990s many studies have been conducted on the impact of international migration on international trade, predominantly from the host country perspective. Because most studies have adopted broadly the same specification, namely a log‐linear gravity model of export and import flows augmented with the logarithm of the stock of immigrants from specific source countries as an additional explanatory variable, the resulting elasticities are broadly comparable and yield a set of estimates that is well suited to meta‐analysis. We therefore compile and analyze in this paper the distribution of immigration elasticities of imports and exports across 48 studies that yielded 300 estimates. The results confirm that immigration boosts trade, but its impact is lower on trade in homogeneous goods. An increase in the number of immigrants by 10 percent increases the volume of trade by about 1‐2 percent The migrant elasticity of imports is on average similar to that of exports. The estimates are affected by the choice of some covariates, the nature of the data (cross‐section or panel) and the estimation technique.  Elasticities vary between countries in ways that cannot be explained by study characteristics; host country differences in immigration policies do apparently matter for the trade impact. The trade‐enhancing impact of migration appears to be greater for migration between countries of different levels of development than between developed countries.

text: The impact of immigration on international trade: a meta‐analysis Since the early 1990s many studies have been conducted on the impact of international migration on international trade, predominantly from the host country perspective. Because most studies have adopted broadly the same specification, namely a log‐linear gravity model of export and import flows augmented with the logarithm of the stock of immigrants from specific source countries as an additional explanatory variable, the resulting elasticities are broadly comparable and yield a set of estimates that is well suited to meta‐analysis. We therefore compile and analyze in this paper the distribution of immigration elasticities of imports and exports across 48 studies that yielded 300 estimates. The results confirm that immigration boosts trade, but its impact is lower on trade in homogeneous goods. An increase in the number of immigrants by 10 percent increases the volume of trade by about 1‐2 percent The migrant elasticity of imports is on average similar to that of exports. The estimates are affected by the choice of some covariates, the nature of the data (cross‐section or panel) and the estimation technique.  Elasticities vary between countries in ways that cannot be explained by study characteristics; host country differences in immigration policies do apparently matter for the trade impact. The trade‐enhancing impact of migration appears to be greater for migration between countries of different levels of development than between developed countries.

year: 2011

title: Note on the occurrence of Taupo pumice in the Hamilton basin

authors: Tonkin, Philip J.

subjects: Hamilton basin

abstract: The presence of a thin layer of pumice lapilli and ash close to the surface of the Rukuhia and Moanatuatua peat bogs was recorded by Grange and Taylor (1939). Since this time a similar band of pumice has been noted in many of the other peat areas in the Hamilton basin. In the undeveloped fibrous peats of the Woodlands bog a layer of pumice lapilli 2 to 3 inches thick occurs at a depth of 18 to 20 inches from the surface. This is similar to the observations of Grange and Taylor. In the more loamy peats the pumice layer is predominantly fine ash and any lapilli present are extremely weathered and crush easily. In the fibrous peats it is thought that the fine ash that fell on the bog surface soon dispersed in the loose network of dead material, whereas the lapilli were of sufficient size to be trapped. In the loamy peats more active weathering took place in an acid environment as the organic matter was breaking down. This made the lapilli very fragile, so with drainage and compaction of the peat the lapilli were very soon crushed to fine ash size.

text: Note on the occurrence of Taupo pumice in the Hamilton basin The presence of a thin layer of pumice lapilli and ash close to the surface of the Rukuhia and Moanatuatua peat bogs was recorded by Grange and Taylor (1939). Since this time a similar band of pumice has been noted in many of the other peat areas in the Hamilton basin. In the undeveloped fibrous peats of the Woodlands bog a layer of pumice lapilli 2 to 3 inches thick occurs at a depth of 18 to 20 inches from the surface. This is similar to the observations of Grange and Taylor. In the more loamy peats the pumice layer is predominantly fine ash and any lapilli present are extremely weathered and crush easily. In the fibrous peats it is thought that the fine ash that fell on the bog surface soon dispersed in the loose network of dead material, whereas the lapilli were of sufficient size to be trapped. In the loamy peats more active weathering took place in an acid environment as the organic matter was breaking down. This made the lapilli very fragile, so with drainage and compaction of the peat the lapilli were very soon crushed to fine ash size.

year: 1967

title: Sharemilking with the Te Raparahi Lands Trust (Wāotū)

authors: Hutcheson, Gail Yvonne

subjects: Place

abstract: This paper discusses sharemilking  in New Zealand.

text: Sharemilking with the Te Raparahi Lands Trust (Wāotū) This paper discusses sharemilking  in New Zealand.

year: 2017