(Table 1) Isotopic and geochemical parameters of gas phase from underground fluids of the Baikal rift and its framing

Results of studying isotopic composition of helium in underground fluids of the Baikal-Mongolian region during the last quarter of XX century are summarized. Determinations of 3He/4He ratio in 139 samples of gas phase from fluids, collected at 104 points of the Baikal rift zone and adjacent structures are given. 3He/4He values lie within the range from 1x10**-8 (typical for crustal radiogenic helium) to 1.1x10**-5 (close to typical MORB reservoir). Repeated sampling in some points during more than 20 years showed stability of helium isotopic composition in time in each of them at any level of 3He/4He values. There is no systematic differences of 3He/4He in samples from surface water sources and deeper intervals of boreholes in the same areas. Universal relationship between isotopic composition of helium and general composition of gas phase is absent either, but the minimum 3He/4He values occurred in methane gas of hydrocarbon deposits, whereas in nitrogen and carbon dioxide gases of helium composition varied (in the latter maximum 3He/4He values have been measured). According to N2/Ar_atm ratio nitrogen gases are atmospheric. In carbonic gas fN2/fNe ratio indicates presence of excessive (non-atmogenic) nitrogen, but the attitude CO2/3He differs from one in MORB. Comparison of helium isotopic composition with its concentration and composition of the main components of gas phase from fluids shows that it is formed under influence of fractionation of components with different solubility in the gas-water system and generation/consumption of reactive gases in the crust. Structural and tectonic elements of the region differ from the spectrum of 3He/4He values. At the pre-Riphean Siberian Platform the mean 3He/4He = (3.6+/-0.9)x10**- 8 is very close to radiogenic one. In the Paleozoic crust of Khangay 3He/4He = (16.3+/-4.6)x10**-8, and the most probable estimate is (12.3+/-2.9)x10**-8. In structures of the eastern flank of the Baikal rift zone (Khentei, Dauria) affected by the Mz-Kz activization 3He/4He values range from 4.4x10**-8 to 2.14x10**-6 (average 0.94x10**-6). Distribution of 3He/4He values across the strike of the Baikal rift zone indicates advective heat transfer from the mantle not only in the rift zone, but also much further to the east. In fluids of the Baikal rift zone range of 3He/4He values is the widest: from 4x10**-8 to 1.1x10**-5. Their variations along the strike of the rift zone are clearly patterned, namely, decrease of 3He/4He values in both directions from the Tunka depression. Accompanied by decrease in density of conductive heat flow and in size of rift basins, this trend indicates decrease in intensity of advective heat transfer from the mantle to peripheral segments of the rift zone. Comparing this trend with data on other continental rift zones and mid-ocean ridges leads to the conclusion about fundamental differences in mechanisms of interaction between the crust and the mantle in these environments.

The growth of demand will limit output growth for food over the next quarter century

The rate of growth of world food demand will be much slower for 1990–2010 than it was for the prior three decades. The major factor determining the increase in food demand is population growth. Income growth has a much smaller effect. From 1960 to 1990, population growth accounted for approximately three fourths of the growth in demand or use of grain. For 1990–2010, it is anticipated that population growth will account for nearly all of the increase in world demand for grain. The rate of population growth from 1990 to 2020 is projected to be at an annual rate of 1.3% compared with 1.9% for 1960 to 1990—a decline of more than 30%. World per capita use of grain will increase very little—perhaps by 4%. The increase in grain use is projected to be 40% less than in 1960–1990. It is anticipated that real grain prices will decline during the period, although not nearly as much as the 40% decline in the previous three decades. Concern has been expressed concerning the deterioration of the quality and productivity of the world’s farmland. A study for China and Indonesia indicates that there has been no significant change in the productive capacity of the land over the past 50 years. Contrary to numerous claims, the depth of the topsoil has not changed, indicating that erosion has had little or no impact.

Quarter bills, 1796

Two printed quarter bills for Loammi Baldwin dated August 25, 1796 and November 24, 1796.

Quarter bills, 1797

Four printed quarter bills for Loammi Baldwin dated February 23, 1797, May 25, 1797, August 24, 1797, and November 23, 1797.

Quarter bills, 1798

Three printed quarter bills for Loammi Baldwin dated February 22, 1798, May 24, 1798, and November 29, 1798.

Quarter bills, 1799

Two printed quarter bills for Loammi Baldwin dated February 21, 1799 and November 28, 1799.

Quarter bills, 1800

Three printed quarter bills for Loammi Baldwin with one dated February 27, 1800 and two from May 29, 1800.

An account of my quarter bills, charges &c from July 11th 1743 to July 13th 1748 at Harvard College

Handwritten account book kept while Storer was a student at Harvard College. The well-organized volume is arranged by expense type and then date and was updated periodically, usually quarterly. The information offers a glimpse at the expenses of a Harvard student and provides information about the larger community that supported student life. The precise entries indicate the lifelong habits of Storer as a careful and methodical financial manager that would prove so valuable when he served as Harvard's treasurer more than thirty years later. Storer documents accounts with the steward, butler, sweeper, glazier, barber, and lists these individuals by name. The volume also includes notes on expenses for boarding, transportation, wood, and pocket expenses. While most entries do not list specific purchases, Storer provides details on the cost of a Harvard Commencement in 1747 (including the cost of a diploma, money to the President, hiring a house, a boat, a woman, and "2 Negroes"), and a specific accounting of the different food purchased for the event; Storer also lists expenses for an 1748 "supper for the graduates."

Report of committee for the form of quarter bills, 1778 December 12

This one-and-a-half page handwritten draft of a report on a folio-sized leaf outlines a six-point process for drafting and authorizing student quarter bills. The procedures consolidate the billing areas, detail the Treasurer's responsibilities, and expand the oversight of the President and Tutors. The report, dated December 12, 1778, is signed by President Samuel Langdon. The draft includes two differently worded versions of the sixth proposal, one of which is struck through.

Collection of Harvard College quarter bill and butler's bills sent to Charles Davis, 1793-1796

This collection consists of one quarter bill and three butler's bills, all sent to Charles Davis while he was an undergraduate at Harvard College. The quarter bill is from August 1795 and the butler's bills are from February and November 1793 and July 1796. John Pipon and Timothy Alden were the butlers at this time, and Caleb Gannett was the steward (responsible for the quarter bill).