国立情報学研究所 - ディジタル・シルクロード・プロジェクト
『東洋文庫所蔵』貴重書デジタルアーカイブ
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| 0264 |
The Pulse of Asia : vol.1 |
| アジアの鼓動 : vol.1 |
引用情報
OCR読み取り結果
first in the zone of piedmont gravel. At the edge of the zone
of vegetation it reappears, and after watering Niya, sinks
into the ground a second time. Within a few miles it comes
to light again, only to be lost in the course of the next twenty
or thirty miles. Finally, at the shrine of Imam Jafir Sadik,
fifty miles from Niya, it reappears once more, but with such
diminished volume that it persists only five or six miles
before disappearing for the fourth and last time. During
the flood season, an uninterrupted stream flows from the
mountains to the last shepherd hut below the shrine, but
it is very temporary, and does not persist more than two or
three miles beyond the limit of the winter stream.
In an arid region like the Lop basin, water which flows
far underground becomes saline. Even Niya suffers from
salinity. North of the town I crossed fully half a mile of
land formerly reckoned as "first" of the three classes rated
for taxation, but now abandoned as too saline for anything
save pasture. Year by year fields are being given up at a
rate which threatens the extinction of the oasis within a few
generations. As might be expected, the water is even more
saline farther downstream, and permanent cultivation is
impossible. Various attempts, in addition to the one men-
tioned above, have been made to found villages near the
shrine and farther upstream, but all have failed within
three or four years at most. At Imam Jafir Sadik, eleven
families, scattered along the river for four or five miles, raise
a little corn, wheat, alfalfa, and melons, but cannot culti-
vate trees. They choose the sandiest, least saline soil, and
by cultivating a given patch only once in two or three
years, manage to eke out the produce of their flocks. In one
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